Articles | Volume 40, issue 2
https://doi.org/10.5194/jm-40-175-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/jm-40-175-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
29 Oct 2021
Research article |
| 29 Oct 2021
| 29 Oct 2021
Late Eocene–early Miocene evolution of the southern Australian subtropical front: a marine palynological approach
Marine Palynology and Paleoceanography, Department of Earth Sciences,
Utrecht University, Utrecht, the Netherlands
Isabel Sauermilch
Marine Palynology and Paleoceanography, Department of Earth Sciences,
Utrecht University, Utrecht, the Netherlands
Suning Hou
Marine Palynology and Paleoceanography, Department of Earth Sciences,
Utrecht University, Utrecht, the Netherlands
Henk Brinkhuis
Marine Palynology and Paleoceanography, Department of Earth Sciences,
Utrecht University, Utrecht, the Netherlands
Royal Netherlands Institute for Sea Research (NIOZ), Texel, the
Netherlands
Francesca Sangiorgi
Marine Palynology and Paleoceanography, Department of Earth Sciences,
Utrecht University, Utrecht, the Netherlands
Peter K. Bijl
Marine Palynology and Paleoceanography, Department of Earth Sciences,
Utrecht University, Utrecht, the Netherlands
Related authors
Frida S. Hoem, Karlijn van den Broek, Adrián López-Quirós, Suzanna H. A. van de Lagemaat, Steve M. Bohaty, Claus-Dieter Hillenbrand, Robert D. Larter, Tim E. van Peer, Henk Brinkhuis, Francesca Sangiorgi, and Peter K. Bijl
J. Micropalaeontol., 43, 497–517, https://doi.org/10.5194/jm-43-497-2024, https://doi.org/10.5194/jm-43-497-2024, 2024
Short summary
Short summary
The timing and impact of onset of Antarctic Circumpolar Current (ACC) on climate and Antarctic ice are unclear. We reconstruct late Eocene to Miocene southern Atlantic surface ocean environment using microfossil remains of dinoflagellates (dinocysts). Our dinocyst records shows the breakdown of subpolar gyres in the late Oligocene and the transition into a modern-like oceanographic regime with ACC flow, established frontal systems, Antarctic proximal cooling, and sea ice by the late Miocene.
Frida S. Hoem, Adrián López-Quirós, Suzanna van de Lagemaat, Johan Etourneau, Marie-Alexandrine Sicre, Carlota Escutia, Henk Brinkhuis, Francien Peterse, Francesca Sangiorgi, and Peter K. Bijl
Clim. Past, 19, 1931–1949, https://doi.org/10.5194/cp-19-1931-2023, https://doi.org/10.5194/cp-19-1931-2023, 2023
Short summary
Short summary
We present two new sea surface temperature (SST) records in comparison with available SST records to reconstruct South Atlantic paleoceanographic evolution. Our results show a low SST gradient in the Eocene–early Oligocene due to the persistent gyral circulation. A higher SST gradient in the Middle–Late Miocene infers a stronger circumpolar current. The southern South Atlantic was the coldest region in the Southern Ocean and likely the main deep-water formation location in the Middle Miocene.
Suning Hou, Foteini Lamprou, Frida S. Hoem, Mohammad Rizky Nanda Hadju, Francesca Sangiorgi, Francien Peterse, and Peter K. Bijl
Clim. Past, 19, 787–802, https://doi.org/10.5194/cp-19-787-2023, https://doi.org/10.5194/cp-19-787-2023, 2023
Short summary
Short summary
Neogene climate cooling is thought to be accompanied by increased Equator-to-pole temperature gradients, but mid-latitudes are poorly represented. We use biomarkers to reconstruct a 23 Myr continuous sea surface temperature record of the mid-latitude Southern Ocean. We note a profound mid-latitude cooling which narrowed the latitudinal temperature gradient with the northward expansion of subpolar conditions. We surmise that this reflects the strengthening of the ACC and the expansion of sea ice.
Nick Thompson, Ulrich Salzmann, Adrián López-Quirós, Peter K. Bijl, Frida S. Hoem, Johan Etourneau, Marie-Alexandrine Sicre, Sabine Roignant, Emma Hocking, Michael Amoo, and Carlota Escutia
Clim. Past, 18, 209–232, https://doi.org/10.5194/cp-18-209-2022, https://doi.org/10.5194/cp-18-209-2022, 2022
Short summary
Short summary
New pollen and spore data from the Antarctic Peninsula region reveal temperate rainforests that changed and adapted in response to Eocene climatic cooling, roughly 35.5 Myr ago, and glacially related disturbance in the early Oligocene, approximately 33.5 Myr ago. The timing of these events indicates that the opening of ocean gateways alone did not trigger Antarctic glaciation, although ocean gateways may have played a role in climate cooling.
Frida S. Hoem, Luis Valero, Dimitris Evangelinos, Carlota Escutia, Bella Duncan, Robert M. McKay, Henk Brinkhuis, Francesca Sangiorgi, and Peter K. Bijl
Clim. Past, 17, 1423–1442, https://doi.org/10.5194/cp-17-1423-2021, https://doi.org/10.5194/cp-17-1423-2021, 2021
Short summary
Short summary
We present new offshore palaeoceanographic reconstructions for the Oligocene (33.7–24.4 Ma) in the Ross Sea, Antarctica. Our study of dinoflagellate cysts and lipid biomarkers indicates warm-temperate sea surface conditions. We posit that warm surface-ocean conditions near the continental shelf during the Oligocene promoted increased precipitation and heat delivery towards Antarctica that led to dynamic terrestrial ice sheet volumes in the warmer climate state of the Oligocene.
Frida S. Hoem, Karlijn van den Broek, Adrián López-Quirós, Suzanna H. A. van de Lagemaat, Steve M. Bohaty, Claus-Dieter Hillenbrand, Robert D. Larter, Tim E. van Peer, Henk Brinkhuis, Francesca Sangiorgi, and Peter K. Bijl
J. Micropalaeontol., 43, 497–517, https://doi.org/10.5194/jm-43-497-2024, https://doi.org/10.5194/jm-43-497-2024, 2024
Short summary
Short summary
The timing and impact of onset of Antarctic Circumpolar Current (ACC) on climate and Antarctic ice are unclear. We reconstruct late Eocene to Miocene southern Atlantic surface ocean environment using microfossil remains of dinoflagellates (dinocysts). Our dinocyst records shows the breakdown of subpolar gyres in the late Oligocene and the transition into a modern-like oceanographic regime with ACC flow, established frontal systems, Antarctic proximal cooling, and sea ice by the late Miocene.
Appy Sluijs and Henk Brinkhuis
J. Micropalaeontol., 43, 441–474, https://doi.org/10.5194/jm-43-441-2024, https://doi.org/10.5194/jm-43-441-2024, 2024
Short summary
Short summary
We present intrinsic details of dinocyst taxa and assemblages from the sole available central Arctic late Paleocene–early Eocene sedimentary succession recovered at the central Lomonosov Ridge by the Integrated Ocean Drilling Program (IODP) Expedition 302. We develop a pragmatic taxonomic framework, document critical biostratigraphic events, and propose two new genera and seven new species.
Dominique K. L. L. Jenny, Tammo Reichgelt, Charlotte L. O'Brien, Xiaoqing Liu, Peter K. Bijl, Matthew Huber, and Appy Sluijs
Clim. Past, 20, 1627–1657, https://doi.org/10.5194/cp-20-1627-2024, https://doi.org/10.5194/cp-20-1627-2024, 2024
Short summary
Short summary
This study reviews the current state of knowledge regarding the Oligocene
icehouseclimate. We extend an existing marine climate proxy data compilation and present a new compilation and analysis of terrestrial plant assemblages to assess long-term climate trends and variability. Our data–climate model comparison reinforces the notion that models underestimate polar amplification of Oligocene climates, and we identify potential future research directions.
Mark Vinz Elbertsen, Erik van Sebille, and Peter Kristian Bijl
EGUsphere, https://doi.org/10.5194/egusphere-2024-1596, https://doi.org/10.5194/egusphere-2024-1596, 2024
Short summary
Short summary
This work verifies the remarkable finds of late Eocene Antarctic-sourced iceberg-rafted debris found on South Orkney. We find that these icebergs must have been on the larger end of the size scale compared to today’s icebergs due to faster melting in the warmer Eocene climate. The study was performed using a high-resolution model in which individual icebergs were followed through time.
Chris D. Fokkema, Tobias Agterhuis, Danielle Gerritsma, Myrthe de Goeij, Xiaoqing Liu, Pauline de Regt, Addison Rice, Laurens Vennema, Claudia Agnini, Peter K. Bijl, Joost Frieling, Matthew Huber, Francien Peterse, and Appy Sluijs
Clim. Past, 20, 1303–1325, https://doi.org/10.5194/cp-20-1303-2024, https://doi.org/10.5194/cp-20-1303-2024, 2024
Short summary
Short summary
Polar amplification (PA) is a key uncertainty in climate projections. The factors that dominantly control PA are difficult to separate. Here we provide an estimate for the non-ice-related PA by reconstructing tropical ocean temperature variability from the ice-free early Eocene, which we compare to deep-ocean-derived high-latitude temperature variability across short-lived warming periods. We find a PA factor of 1.7–2.3 on 20 kyr timescales, which is somewhat larger than model estimates.
Suning Hou, Leonie Toebrock, Mart van der Linden, Fleur Rothstegge, Martin Ziegler, Lucas J. Lourens, and Peter K. Bijl
Clim. Past Discuss., https://doi.org/10.5194/cp-2024-33, https://doi.org/10.5194/cp-2024-33, 2024
Revised manuscript accepted for CP
Short summary
Short summary
Based on dinoflagellate cyst assemblage and sea surface temperature record west offshore Tasmania, we find a northward migration and freshening of the subtropical front, not at the M2 glacial maximum but at its deglaciation phase. This oceanographic change aligns well with the trends in pCO2. We propose that iceberg discharge from the M2 deglaciation freshened the subtropical front, which together with the other oceanographic changes, affected atmosphere-ocean CO2 exchange in the Southern Ocean.
Peter K. Bijl
Earth Syst. Sci. Data, 16, 1447–1452, https://doi.org/10.5194/essd-16-1447-2024, https://doi.org/10.5194/essd-16-1447-2024, 2024
Short summary
Short summary
This new version release of DINOSTRAT, version 2.1, aligns stratigraphic ranges of dinoflagellate cysts (dinocysts), a microfossil group, to the latest Geologic Time Scale. In this release I present the evolution of dinocyst subfamilies from the Middle Triassic to the modern period.
Michiel Baatsen, Peter Bijl, Anna von der Heydt, Appy Sluijs, and Henk Dijkstra
Clim. Past, 20, 77–90, https://doi.org/10.5194/cp-20-77-2024, https://doi.org/10.5194/cp-20-77-2024, 2024
Short summary
Short summary
This work introduces the possibility and consequences of monsoons on Antarctica in the warm Eocene climate. We suggest that such a monsoonal climate can be important to understand conditions in Antarctica prior to large-scale glaciation. We can explain seemingly contradictory indications of ice and vegetation on the continent through regional variability. In addition, we provide a new mechanism through which most of Antarctica remained ice-free through a wide range of global climatic changes.
Peter K. Bijl and Henk Brinkhuis
J. Micropalaeontol., 42, 309–314, https://doi.org/10.5194/jm-42-309-2023, https://doi.org/10.5194/jm-42-309-2023, 2023
Short summary
Short summary
We developed an online, open-access database for taxonomic descriptions, stratigraphic information and images of organic-walled dinoflagellate cyst species. With this new resource for applied and academic research, teaching and training, we open up organic-walled dinoflagellate cysts for the academic era of open science. We expect that palsys.org represents a starting point to improve taxonomic concepts, and we invite the community to contribute.
Yord W. Yedema, Timme Donders, Francien Peterse, and Francesca Sangiorgi
J. Micropalaeontol., 42, 257–276, https://doi.org/10.5194/jm-42-257-2023, https://doi.org/10.5194/jm-42-257-2023, 2023
Short summary
Short summary
The pollen and dinoflagellate cyst content of 21 surface sediments from the northern Gulf of Mexico is used to test the applicability of three palynological ratios (heterotroph/autotroph, pollen/dinocyst, and pollen/bisaccate ratio) as proxies for marine productivity and distance to the coast/river. Redundancy analysis confirms the suitability of these three ratios, where the H/A ratio can be used as an indicator of primary production, and the P/B ratio best tracks the distance to the coast.
Frida S. Hoem, Adrián López-Quirós, Suzanna van de Lagemaat, Johan Etourneau, Marie-Alexandrine Sicre, Carlota Escutia, Henk Brinkhuis, Francien Peterse, Francesca Sangiorgi, and Peter K. Bijl
Clim. Past, 19, 1931–1949, https://doi.org/10.5194/cp-19-1931-2023, https://doi.org/10.5194/cp-19-1931-2023, 2023
Short summary
Short summary
We present two new sea surface temperature (SST) records in comparison with available SST records to reconstruct South Atlantic paleoceanographic evolution. Our results show a low SST gradient in the Eocene–early Oligocene due to the persistent gyral circulation. A higher SST gradient in the Middle–Late Miocene infers a stronger circumpolar current. The southern South Atlantic was the coldest region in the Southern Ocean and likely the main deep-water formation location in the Middle Miocene.
William Rush, Jean Self-Trail, Yang Zhang, Appy Sluijs, Henk Brinkhuis, James Zachos, James G. Ogg, and Marci Robinson
Clim. Past, 19, 1677–1698, https://doi.org/10.5194/cp-19-1677-2023, https://doi.org/10.5194/cp-19-1677-2023, 2023
Short summary
Short summary
The Eocene contains several brief warming periods referred to as hyperthermals. Studying these events and how they varied between locations can help provide insight into our future warmer world. This study provides a characterization of two of these events in the mid-Atlantic region of the USA. The records of climate that we measured demonstrate significant changes during this time period, but the type and timing of these changes highlight the complexity of climatic changes.
Peter K. Bijl
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2023-169, https://doi.org/10.5194/essd-2023-169, 2023
Publication in ESSD not foreseen
Short summary
Short summary
This new version release of DINOSTRAT, version 2.0, aligns stratigraphic ranges of dinoflagellate cysts, a microfossil group, to the Geologic Time Scale. In this release we present the evolution of dinocyst subfamilies from the mid-Triassic to the modern.
Lena Mareike Thöle, Peter Dirk Nooteboom, Suning Hou, Rujian Wang, Senyan Nie, Elisabeth Michel, Isabel Sauermilch, Fabienne Marret, Francesca Sangiorgi, and Peter Kristian Bijl
J. Micropalaeontol., 42, 35–56, https://doi.org/10.5194/jm-42-35-2023, https://doi.org/10.5194/jm-42-35-2023, 2023
Short summary
Short summary
Dinoflagellate cysts can be used to infer past oceanographic conditions in the Southern Ocean. This requires knowledge of their present-day ecologic affinities. We add 66 Antarctic-proximal surface sediment samples to the Southern Ocean data and derive oceanographic conditions at those stations. Dinoflagellate cysts are clearly biogeographically separated along latitudinal gradients of temperature, sea ice, nutrients, and salinity, which allows us to reconstruct these parameters for the past.
Suning Hou, Foteini Lamprou, Frida S. Hoem, Mohammad Rizky Nanda Hadju, Francesca Sangiorgi, Francien Peterse, and Peter K. Bijl
Clim. Past, 19, 787–802, https://doi.org/10.5194/cp-19-787-2023, https://doi.org/10.5194/cp-19-787-2023, 2023
Short summary
Short summary
Neogene climate cooling is thought to be accompanied by increased Equator-to-pole temperature gradients, but mid-latitudes are poorly represented. We use biomarkers to reconstruct a 23 Myr continuous sea surface temperature record of the mid-latitude Southern Ocean. We note a profound mid-latitude cooling which narrowed the latitudinal temperature gradient with the northward expansion of subpolar conditions. We surmise that this reflects the strengthening of the ACC and the expansion of sea ice.
Yord W. Yedema, Francesca Sangiorgi, Appy Sluijs, Jaap S. Sinninghe Damsté, and Francien Peterse
Biogeosciences, 20, 663–686, https://doi.org/10.5194/bg-20-663-2023, https://doi.org/10.5194/bg-20-663-2023, 2023
Short summary
Short summary
Terrestrial organic matter (TerrOM) is transported to the ocean by rivers, where its burial can potentially form a long-term carbon sink. This burial is dependent on the type and characteristics of the TerrOM. We used bulk sediment properties, biomarkers, and palynology to identify the dispersal patterns of plant-derived, soil–microbial, and marine OM in the northern Gulf of Mexico and show that plant-derived OM is transported further into the coastal zone than soil and marine-produced TerrOM.
Qianjiang Xing, David Munday, Andreas Klocker, Isabel Sauermilch, and Joanne Whittaker
Clim. Past, 18, 2669–2693, https://doi.org/10.5194/cp-18-2669-2022, https://doi.org/10.5194/cp-18-2669-2022, 2022
Short summary
Short summary
A high-resolution ocean model and realistic paleo-bathymetry are applied to obtain accurate simulation results. We firstly propose that the alignment of the maximum wind stress with a deep Tasmanian Gateway and Drake Passage is a trigger for the proto-Antarctic Circumpolar Current (proto-ACC) and the cooling of the Eocene Southern Ocean. We use zonal momentum budget analysis to explore the nature of the proto-ACC and the sensitivity of its transport through gateways to doubled wind stress.
Frédérique M. S. A. Kirkels, Huub M. Zwart, Muhammed O. Usman, Suning Hou, Camilo Ponton, Liviu Giosan, Timothy I. Eglinton, and Francien Peterse
Biogeosciences, 19, 3979–4010, https://doi.org/10.5194/bg-19-3979-2022, https://doi.org/10.5194/bg-19-3979-2022, 2022
Short summary
Short summary
Soil organic carbon (SOC) that is transferred to the ocean by rivers forms a long-term sink of atmospheric CO2 upon burial on the ocean floor. We here test if certain bacterial membrane lipids can be used to trace SOC through the monsoon-fed Godavari River basin in India. We find that these lipids trace the mobilisation and transport of SOC in the wet season but that these lipids are not transferred far into the sea. This suggests that the burial of SOC on the sea floor is limited here.
Carolien M. H. van der Weijst, Koen J. van der Laan, Francien Peterse, Gert-Jan Reichart, Francesca Sangiorgi, Stefan Schouten, Tjerk J. T. Veenstra, and Appy Sluijs
Clim. Past, 18, 1947–1962, https://doi.org/10.5194/cp-18-1947-2022, https://doi.org/10.5194/cp-18-1947-2022, 2022
Short summary
Short summary
The TEX86 proxy is often used by paleoceanographers to reconstruct past sea-surface temperatures. However, the origin of the TEX86 signal in marine sediments has been debated since the proxy was first proposed. In our paper, we show that TEX86 carries a mixed sea-surface and subsurface temperature signal and should be calibrated accordingly. Using our 15-million-year record, we subsequently show how a TEX86 subsurface temperature record can be used to inform us on past sea-surface temperatures.
Carolien M. H. van der Weijst, Josse Winkelhorst, Wesley de Nooijer, Anna von der Heydt, Gert-Jan Reichart, Francesca Sangiorgi, and Appy Sluijs
Clim. Past, 18, 961–973, https://doi.org/10.5194/cp-18-961-2022, https://doi.org/10.5194/cp-18-961-2022, 2022
Short summary
Short summary
A hypothesized link between Pliocene (5.3–2.5 million years ago) global climate and tropical thermocline depth is currently only backed up by data from the Pacific Ocean. In our paper, we present temperature, salinity, and thermocline records from the tropical Atlantic Ocean. Surprisingly, the Pliocene thermocline evolution was remarkably different in the Atlantic and Pacific. We need to reevaluate the mechanisms that drive thermocline depth, and how these are tied to global climate change.
Michael Amoo, Ulrich Salzmann, Matthew J. Pound, Nick Thompson, and Peter K. Bijl
Clim. Past, 18, 525–546, https://doi.org/10.5194/cp-18-525-2022, https://doi.org/10.5194/cp-18-525-2022, 2022
Short summary
Short summary
Late Eocene to earliest Oligocene (37.97–33.06 Ma) climate and vegetation dynamics around the Tasmanian Gateway region reveal that changes in ocean circulation due to accelerated deepening of the Tasmanian Gateway may not have been solely responsible for the changes in terrestrial climate and vegetation; a series of regional and global events, including a change in stratification of water masses and changes in pCO2, may have played significant roles.
Peter D. Nooteboom, Peter K. Bijl, Christian Kehl, Erik van Sebille, Martin Ziegler, Anna S. von der Heydt, and Henk A. Dijkstra
Earth Syst. Dynam., 13, 357–371, https://doi.org/10.5194/esd-13-357-2022, https://doi.org/10.5194/esd-13-357-2022, 2022
Short summary
Short summary
Having descended through the water column, microplankton in ocean sediments represents the ocean surface environment and is used as an archive of past and present surface oceanographic conditions. However, this microplankton is advected by turbulent ocean currents during its sinking journey. We use simulations of sinking particles to define ocean bottom provinces and detect these provinces in datasets of sedimentary microplankton, which has implications for palaeoclimate reconstructions.
Peter K. Bijl
Earth Syst. Sci. Data, 14, 579–617, https://doi.org/10.5194/essd-14-579-2022, https://doi.org/10.5194/essd-14-579-2022, 2022
Short summary
Short summary
Using microfossils to gauge the age of rocks and sediments requires an accurate age of their first (origination) and last (extinction) appearances. But how do you know such ages can then be applied worldwide? And what causes regional differences? This paper investigates the regional consistency of ranges of species of a specific microfossil group, organic-walled dinoflagellate cysts. This overview helps in identifying regional differences in the stratigraphic ranges of species and their causes.
Nick Thompson, Ulrich Salzmann, Adrián López-Quirós, Peter K. Bijl, Frida S. Hoem, Johan Etourneau, Marie-Alexandrine Sicre, Sabine Roignant, Emma Hocking, Michael Amoo, and Carlota Escutia
Clim. Past, 18, 209–232, https://doi.org/10.5194/cp-18-209-2022, https://doi.org/10.5194/cp-18-209-2022, 2022
Short summary
Short summary
New pollen and spore data from the Antarctic Peninsula region reveal temperate rainforests that changed and adapted in response to Eocene climatic cooling, roughly 35.5 Myr ago, and glacially related disturbance in the early Oligocene, approximately 33.5 Myr ago. The timing of these events indicates that the opening of ocean gateways alone did not trigger Antarctic glaciation, although ocean gateways may have played a role in climate cooling.
Peter K. Bijl, Joost Frieling, Marlow Julius Cramwinckel, Christine Boschman, Appy Sluijs, and Francien Peterse
Clim. Past, 17, 2393–2425, https://doi.org/10.5194/cp-17-2393-2021, https://doi.org/10.5194/cp-17-2393-2021, 2021
Short summary
Short summary
Here, we use the latest insights for GDGT and dinocyst-based paleotemperature and paleoenvironmental reconstructions in late Cretaceous–early Oligocene sediments from ODP Site 1172 (East Tasman Plateau, Australia). We reconstruct strong river runoff during the Paleocene–early Eocene, a progressive decline thereafter with increased wet/dry seasonality in the northward-drifting hinterland. Our critical review leaves the anomalous warmth of the Eocene SW Pacific Ocean unexplained.
Frida S. Hoem, Luis Valero, Dimitris Evangelinos, Carlota Escutia, Bella Duncan, Robert M. McKay, Henk Brinkhuis, Francesca Sangiorgi, and Peter K. Bijl
Clim. Past, 17, 1423–1442, https://doi.org/10.5194/cp-17-1423-2021, https://doi.org/10.5194/cp-17-1423-2021, 2021
Short summary
Short summary
We present new offshore palaeoceanographic reconstructions for the Oligocene (33.7–24.4 Ma) in the Ross Sea, Antarctica. Our study of dinoflagellate cysts and lipid biomarkers indicates warm-temperate sea surface conditions. We posit that warm surface-ocean conditions near the continental shelf during the Oligocene promoted increased precipitation and heat delivery towards Antarctica that led to dynamic terrestrial ice sheet volumes in the warmer climate state of the Oligocene.
Michiel Baatsen, Anna S. von der Heydt, Matthew Huber, Michael A. Kliphuis, Peter K. Bijl, Appy Sluijs, and Henk A. Dijkstra
Clim. Past, 16, 2573–2597, https://doi.org/10.5194/cp-16-2573-2020, https://doi.org/10.5194/cp-16-2573-2020, 2020
Short summary
Short summary
Warm climates of the deep past have proven to be challenging to reconstruct with the same numerical models used for future predictions. We present results of CESM simulations for the middle to late Eocene (∼ 38 Ma), in which we managed to match the available indications of temperature well. With these results we can now look into regional features and the response to external changes to ultimately better understand the climate when it is in such a warm state.
Appy Sluijs, Joost Frieling, Gordon N. Inglis, Klaas G. J. Nierop, Francien Peterse, Francesca Sangiorgi, and Stefan Schouten
Clim. Past, 16, 2381–2400, https://doi.org/10.5194/cp-16-2381-2020, https://doi.org/10.5194/cp-16-2381-2020, 2020
Short summary
Short summary
We revisit 15-year-old reconstructions of sea surface temperatures in the Arctic Ocean for the late Paleocene and early Eocene epochs (∼ 57–53 million years ago) based on the distribution of fossil membrane lipids of archaea preserved in Arctic Ocean sediments. We find that improvements in the methods over the past 15 years do not lead to different results. However, data quality is now higher and potential biases better characterized. Results confirm remarkable Arctic warmth during this time.
Marlow Julius Cramwinckel, Lineke Woelders, Emiel P. Huurdeman, Francien Peterse, Stephen J. Gallagher, Jörg Pross, Catherine E. Burgess, Gert-Jan Reichart, Appy Sluijs, and Peter K. Bijl
Clim. Past, 16, 1667–1689, https://doi.org/10.5194/cp-16-1667-2020, https://doi.org/10.5194/cp-16-1667-2020, 2020
Short summary
Short summary
Phases of past transient warming can be used as a test bed to study the environmental response to climate change independent of tectonic change. Using fossil plankton and organic molecules, here we reconstruct surface ocean temperature and circulation in and around the Tasman Gateway during a warming phase 40 million years ago termed the Middle Eocene Climatic Optimum. We find that plankton assemblages track ocean circulation patterns, with superimposed variability being related to temperature.
Carolien Maria Hendrina van der Weijst, Josse Winkelhorst, Anna von der Heydt, Gert-Jan Reichart, Francesca Sangiorgi, and Appy Sluijs
Clim. Past Discuss., https://doi.org/10.5194/cp-2020-105, https://doi.org/10.5194/cp-2020-105, 2020
Manuscript not accepted for further review
Christopher J. Hollis, Tom Dunkley Jones, Eleni Anagnostou, Peter K. Bijl, Marlow Julius Cramwinckel, Ying Cui, Gerald R. Dickens, Kirsty M. Edgar, Yvette Eley, David Evans, Gavin L. Foster, Joost Frieling, Gordon N. Inglis, Elizabeth M. Kennedy, Reinhard Kozdon, Vittoria Lauretano, Caroline H. Lear, Kate Littler, Lucas Lourens, A. Nele Meckler, B. David A. Naafs, Heiko Pälike, Richard D. Pancost, Paul N. Pearson, Ursula Röhl, Dana L. Royer, Ulrich Salzmann, Brian A. Schubert, Hannu Seebeck, Appy Sluijs, Robert P. Speijer, Peter Stassen, Jessica Tierney, Aradhna Tripati, Bridget Wade, Thomas Westerhold, Caitlyn Witkowski, James C. Zachos, Yi Ge Zhang, Matthew Huber, and Daniel J. Lunt
Geosci. Model Dev., 12, 3149–3206, https://doi.org/10.5194/gmd-12-3149-2019, https://doi.org/10.5194/gmd-12-3149-2019, 2019
Short summary
Short summary
The Deep-Time Model Intercomparison Project (DeepMIP) is a model–data intercomparison of the early Eocene (around 55 million years ago), the last time that Earth's atmospheric CO2 concentrations exceeded 1000 ppm. Previously, we outlined the experimental design for climate model simulations. Here, we outline the methods used for compilation and analysis of climate proxy data. The resulting climate
atlaswill provide insights into the mechanisms that control past warm climate states.
Thomas M. Hoyle, Manuel Sala-Pérez, and Francesca Sangiorgi
J. Micropalaeontol., 38, 55–65, https://doi.org/10.5194/jm-38-55-2019, https://doi.org/10.5194/jm-38-55-2019, 2019
Short summary
Short summary
Morphology of dinoflagellate cysts (which are valuable tools in deciphering past environmental and climate changes) depends not only on genetics, but also on a range of environmental factors. We review frequently occurring (Black Sea) morphotypes and propose use of matrices to record gradual variation between endmember forms as a pragmatic approach until cyst–theca studies and genetic sequencing can demonstrate relationships between genetically and environmentally controlled morphotypes.
Robert McKay, Neville Exon, Dietmar Müller, Karsten Gohl, Michael Gurnis, Amelia Shevenell, Stuart Henrys, Fumio Inagaki, Dhananjai Pandey, Jessica Whiteside, Tina van de Flierdt, Tim Naish, Verena Heuer, Yuki Morono, Millard Coffin, Marguerite Godard, Laura Wallace, Shuichi Kodaira, Peter Bijl, Julien Collot, Gerald Dickens, Brandon Dugan, Ann G. Dunlea, Ron Hackney, Minoru Ikehara, Martin Jutzeler, Lisa McNeill, Sushant Naik, Taryn Noble, Bradley Opdyke, Ingo Pecher, Lowell Stott, Gabriele Uenzelmann-Neben, Yatheesh Vadakkeykath, and Ulrich G. Wortmann
Sci. Dril., 24, 61–70, https://doi.org/10.5194/sd-24-61-2018, https://doi.org/10.5194/sd-24-61-2018, 2018
Julian D. Hartman, Peter K. Bijl, and Francesca Sangiorgi
J. Micropalaeontol., 37, 445–497, https://doi.org/10.5194/jm-37-445-2018, https://doi.org/10.5194/jm-37-445-2018, 2018
Short summary
Short summary
We present an extensive overview of the organic microfossil remains found at Site U1357, Adélie Basin, East Antarctica. The organic microfossil remains are exceptionally well preserved and are derived from unicellular as well as higher organisms. We provide a morphological description, photographic images, and a discussion of the ecological preferences of the biological species from which the organic remains were derived.
Julian D. Hartman, Francesca Sangiorgi, Ariadna Salabarnada, Francien Peterse, Alexander J. P. Houben, Stefan Schouten, Henk Brinkhuis, Carlota Escutia, and Peter K. Bijl
Clim. Past, 14, 1275–1297, https://doi.org/10.5194/cp-14-1275-2018, https://doi.org/10.5194/cp-14-1275-2018, 2018
Short summary
Short summary
We reconstructed sea surface temperatures for the Oligocene and Miocene periods (34–11 Ma) based on archaeal lipids from a site close to the Wilkes Land coast, Antarctica. Our record suggests generally warm to temperate surface waters: on average 17 °C. Based on the lithology, glacial and interglacial temperatures could be distinguished, showing an average 3 °C offset. The long-term temperature trend resembles the benthic δ18O stack, which may have implications for ice volume reconstructions.
Peter K. Bijl, Alexander J. P. Houben, Julian D. Hartman, Jörg Pross, Ariadna Salabarnada, Carlota Escutia, and Francesca Sangiorgi
Clim. Past, 14, 1015–1033, https://doi.org/10.5194/cp-14-1015-2018, https://doi.org/10.5194/cp-14-1015-2018, 2018
Short summary
Short summary
We document Southern Ocean surface ocean conditions and changes therein during the Oligocene and Miocene (34–10 Myr ago). We infer profound long-term and short-term changes in ice-proximal oceanographic conditions: sea surface temperature, nutrient conditions and sea ice. Our results point to warm-temperate, oligotrophic, ice-proximal oceanographic conditions. These distinct oceanographic conditions may explain the high amplitude in inferred Oligocene–Miocene Antarctic ice volume changes.
Ariadna Salabarnada, Carlota Escutia, Ursula Röhl, C. Hans Nelson, Robert McKay, Francisco J. Jiménez-Espejo, Peter K. Bijl, Julian D. Hartman, Stephanie L. Strother, Ulrich Salzmann, Dimitris Evangelinos, Adrián López-Quirós, José Abel Flores, Francesca Sangiorgi, Minoru Ikehara, and Henk Brinkhuis
Clim. Past, 14, 991–1014, https://doi.org/10.5194/cp-14-991-2018, https://doi.org/10.5194/cp-14-991-2018, 2018
Short summary
Short summary
Here we reconstruct ice sheet and paleoceanographic configurations in the East Antarctic Wilkes Land margin based on a multi-proxy study conducted in late Oligocene (26–25 Ma) sediments from IODP Site U1356. The new obliquity-forced glacial–interglacial sedimentary model shows that, under the high CO2 values of the late Oligocene, ice sheets had mostly retreated to their terrestrial margins and the ocean was very dynamic with shifting positions of the polar fronts and associated water masses.
Michiel Baatsen, Anna S. von der Heydt, Matthew Huber, Michael A. Kliphuis, Peter K. Bijl, Appy Sluijs, and Henk A. Dijkstra
Clim. Past Discuss., https://doi.org/10.5194/cp-2018-43, https://doi.org/10.5194/cp-2018-43, 2018
Revised manuscript not accepted
Short summary
Short summary
The Eocene marks a period where the climate was in a hothouse state, without any continental-scale ice sheets. Such climates have proven difficult to reproduce in models, especially their low temperature difference between equator and poles. Here, we present high resolution CESM simulations using a new geographic reconstruction of the middle-to-late Eocene. The results provide new insights into a period for which knowledge is limited, leading up to a transition into the present icehouse state.
Timme H. Donders, Niels A. G. M. van Helmond, Roel Verreussel, Dirk Munsterman, Johan ten Veen, Robert P. Speijer, Johan W. H. Weijers, Francesca Sangiorgi, Francien Peterse, Gert-Jan Reichart, Jaap S. Sinninghe Damsté, Lucas Lourens, Gesa Kuhlmann, and Henk Brinkhuis
Clim. Past, 14, 397–411, https://doi.org/10.5194/cp-14-397-2018, https://doi.org/10.5194/cp-14-397-2018, 2018
Short summary
Short summary
The buildup and melting of ice during the early glaciations in the Northern Hemisphere, around 2.5 million years ago, were far shorter in duration than during the last million years. Based on molecular compounds and microfossils from sediments dating back to the early glaciations we show that the temperature on land and in the sea changed simultaneously and was a major factor in the ice buildup in the Northern Hemisphere. These data provide key insights into the dynamics of early glaciations.
Joost Frieling, Emiel P. Huurdeman, Charlotte C. M. Rem, Timme H. Donders, Jörg Pross, Steven M. Bohaty, Guy R. Holdgate, Stephen J. Gallagher, Brian McGowran, and Peter K. Bijl
J. Micropalaeontol., 37, 317–339, https://doi.org/10.5194/jm-37-317-2018, https://doi.org/10.5194/jm-37-317-2018, 2018
Short summary
Short summary
The hothouse climate of the early Paleogene and the associated violent carbon cycle perturbations are of particular interest to understanding current and future global climate change. Using dinoflagellate cysts and stable carbon isotope analyses, we identify several significant events, e.g., the Paleocene–Eocene Thermal Maximum in sedimentary deposits from the Otway Basin, SE Australia. We anticipate that this study will facilitate detailed climate reconstructions west of the Tasmanian Gateway.
Peter K. Bijl, Alexander J. P. Houben, Anja Bruls, Jörg Pross, and Francesca Sangiorgi
J. Micropalaeontol., 37, 105–138, https://doi.org/10.5194/jm-37-105-2018, https://doi.org/10.5194/jm-37-105-2018, 2018
Short summary
Short summary
In order to use ocean sediments as a recorder of past oceanographic changes, a critical first step is to stratigraphically date the sediments. The absence of microfossils with known stratigraphic ranges has always hindered dating of Southern Ocean sediments. Here we tie dinocyst ranges to the international timescale in a well-dated sediment core from offshore Antarctica. With this, we can now use dinocysts as a biostratigraphic tool in otherwise stratigraphically poorly dated sediments.
Stephanie L. Strother, Ulrich Salzmann, Francesca Sangiorgi, Peter K. Bijl, Jörg Pross, Carlota Escutia, Ariadna Salabarnada, Matthew J. Pound, Jochen Voss, and John Woodward
Biogeosciences, 14, 2089–2100, https://doi.org/10.5194/bg-14-2089-2017, https://doi.org/10.5194/bg-14-2089-2017, 2017
Short summary
Short summary
One of the main challenges in Antarctic vegetation reconstructions is the uncertainty in unambiguously identifying reworked pollen and spore assemblages in marine sedimentary records influenced by waxing and waning ice sheets. This study uses red fluorescence and digital imaging as a new tool to identify reworking in a marine sediment core from circum-Antarctic waters to reconstruct Cenozoic climate change and vegetation with high confidence.
Johan Vellekoop, Lineke Woelders, Sanem Açikalin, Jan Smit, Bas van de Schootbrugge, Ismail Ö. Yilmaz, Henk Brinkhuis, and Robert P. Speijer
Biogeosciences, 14, 885–900, https://doi.org/10.5194/bg-14-885-2017, https://doi.org/10.5194/bg-14-885-2017, 2017
Short summary
Short summary
The Cretaceous–Paleogene boundary, ~ 66 Ma, is characterized by a mass extinction. We studied groups of both surface-dwelling and bottom-dwelling organisms to unravel the oceanographic consequences of these extinctions. Our integrated records indicate that a reduction of the transport of organic matter to the sea floor resulted in enhanced recycling of nutrients in the upper water column and decreased food supply at the sea floor in the first tens of thousands of years after the extinctions.
Michiel Baatsen, Douwe J. J. van Hinsbergen, Anna S. von der Heydt, Henk A. Dijkstra, Appy Sluijs, Hemmo A. Abels, and Peter K. Bijl
Clim. Past, 12, 1635–1644, https://doi.org/10.5194/cp-12-1635-2016, https://doi.org/10.5194/cp-12-1635-2016, 2016
Short summary
Short summary
One of the major difficulties in modelling palaeoclimate is constricting the boundary conditions, causing significant discrepancies between different studies. Here, a new method is presented to automate much of the process of generating the necessary geographical reconstructions. The latter can be made using various rotational frameworks and topography/bathymetry input, allowing for easy inter-comparisons and the incorporation of the latest insights from geoscientific research.
Niels A. G. M. van Helmond, Appy Sluijs, Nina M. Papadomanolaki, A. Guy Plint, Darren R. Gröcke, Martin A. Pearce, James S. Eldrett, João Trabucho-Alexandre, Ireneusz Walaszczyk, Bas van de Schootbrugge, and Henk Brinkhuis
Biogeosciences, 13, 2859–2872, https://doi.org/10.5194/bg-13-2859-2016, https://doi.org/10.5194/bg-13-2859-2016, 2016
Short summary
Short summary
Over the past decades large changes have been observed in the biogeographical dispersion of marine life resulting from climate change. To better understand present and future trends it is important to document and fully understand the biogeographical response of marine life during episodes of environmental change in the geological past.
Here we investigate the response of phytoplankton, the base of the marine food web, to a rapid cold spell, interrupting greenhouse conditions during the Cretaceous.
Willem P. Sijp, Anna S. von der Heydt, and Peter K. Bijl
Clim. Past, 12, 807–817, https://doi.org/10.5194/cp-12-807-2016, https://doi.org/10.5194/cp-12-807-2016, 2016
Short summary
Short summary
The timing and role in ocean circulation and climate of the opening of Southern Ocean gateways is as yet elusive. Here, we present the first model results specific to the early-to-middle Eocene where, in agreement with the field evidence, a southerly shallow opening of the Tasman Gateway does indeed cause a westward flow across the Tasman Gateway, in agreement with recent micropalaeontological studies.
N. A. G. M. van Helmond, A. Sluijs, J. S. Sinninghe Damsté, G.-J. Reichart, S. Voigt, J. Erbacher, J. Pross, and H. Brinkhuis
Clim. Past, 11, 495–508, https://doi.org/10.5194/cp-11-495-2015, https://doi.org/10.5194/cp-11-495-2015, 2015
Short summary
Short summary
Based on the chemistry and microfossils preserved in sediments deposited in a shallow sea, in the current Lower Saxony region (NW Germany), we conclude that changes in Earth’s orbit around the Sun led to enhanced rainfall and organic matter production. The additional supply of organic matter, depleting oxygen upon degradation, and freshwater, inhibiting the mixing of oxygen-rich surface waters with deeper waters, caused the development of oxygen-poor waters about 94 million years ago.
L. Contreras, J. Pross, P. K. Bijl, R. B. O'Hara, J. I. Raine, A. Sluijs, and H. Brinkhuis
Clim. Past, 10, 1401–1420, https://doi.org/10.5194/cp-10-1401-2014, https://doi.org/10.5194/cp-10-1401-2014, 2014
I. Ruvalcaba Baroni, R. P. M. Topper, N. A. G. M. van Helmond, H. Brinkhuis, and C. P. Slomp
Biogeosciences, 11, 977–993, https://doi.org/10.5194/bg-11-977-2014, https://doi.org/10.5194/bg-11-977-2014, 2014
Related subject area
Palynology
Stepwise Oligocene–Miocene breakdown of subpolar gyres and strengthening of the Antarctic Circumpolar Current
Chitinozoan biostratigraphy through the Aeronian–Telychian boundary interval on Anticosti Island, Canada
High Arctic late Paleocene and early Eocene dinoflagellate cysts
Palsys.org: an open-access taxonomic and stratigraphic database of organic-walled dinoflagellate cysts
Miocene Climatic Optimum fungal record and plant-based CREST climatic reconstruction from southern McMurdo Sound, Antarctica
Dinoflagellate cyst and pollen assemblages as tracers for marine productivity and river input in the northern Gulf of Mexico
An expanded database of Southern Hemisphere surface sediment dinoflagellate cyst assemblages and their oceanographic affinities
Desmocysta hadra, a new Late Cretaceous dinoflagellate cyst species: stratigraphic range, palaeogeographic distribution and palaeoecology
New species of the dinoflagellate cyst genus Svalbardella Manum, 1960, emend. from the Paleogene and Neogene of the northern high to middle latitudes
Organic-walled dinoflagellate cyst biostratigraphy of the upper Eocene to lower Oligocene Yazoo Formation, US Gulf Coast
Early Oligocene dinocysts as a tool for palaeoenvironment reconstruction and stratigraphical framework – a case study from a North Sea well
Chemotaxonomy of domesticated grasses: a pathway to understanding the origins of agriculture
Where should we draw the lines between dinocyst “species”? Morphological continua in Black Sea dinocysts
Record of Early to Middle Eocene paleoenvironmental changes from lignite mines, western India
A review of the ecological affinities of marine organic microfossils from a Holocene record offshore of Adélie Land (East Antarctica)
Stratigraphic calibration of Oligocene–Miocene organic-walled dinoflagellate cysts from offshore Wilkes Land, East Antarctica, and a zonation proposal
Frida S. Hoem, Karlijn van den Broek, Adrián López-Quirós, Suzanna H. A. van de Lagemaat, Steve M. Bohaty, Claus-Dieter Hillenbrand, Robert D. Larter, Tim E. van Peer, Henk Brinkhuis, Francesca Sangiorgi, and Peter K. Bijl
J. Micropalaeontol., 43, 497–517, https://doi.org/10.5194/jm-43-497-2024, https://doi.org/10.5194/jm-43-497-2024, 2024
Short summary
Short summary
The timing and impact of onset of Antarctic Circumpolar Current (ACC) on climate and Antarctic ice are unclear. We reconstruct late Eocene to Miocene southern Atlantic surface ocean environment using microfossil remains of dinoflagellates (dinocysts). Our dinocyst records shows the breakdown of subpolar gyres in the late Oligocene and the transition into a modern-like oceanographic regime with ACC flow, established frontal systems, Antarctic proximal cooling, and sea ice by the late Miocene.
Carolina Klock, André Desrochers, Patrick I. McLaughlin, Poul Emsbo, Tim De Backer, Fien M. Jonckheere, Cristiana J. P. Esteves, and Thijs R. A. Vandenbroucke
J. Micropalaeontol., 43, 475–495, https://doi.org/10.5194/jm-43-475-2024, https://doi.org/10.5194/jm-43-475-2024, 2024
Short summary
Short summary
Anticosti Island has a well-preserved rock succession throughout the Aeronian–Telychian boundary in the Llandovery Epoch, Silurian period, which includes two important biogeochemical events, the late Aeronian and the Valgu. This study suggests the position of this boundary in Anticosti based on the correlation of the island’s chitinozoan assemblages with the global occurrences, confirming both a remarkable preservation of upper Aeronian rocks and the record of the Valgu event.
Appy Sluijs and Henk Brinkhuis
J. Micropalaeontol., 43, 441–474, https://doi.org/10.5194/jm-43-441-2024, https://doi.org/10.5194/jm-43-441-2024, 2024
Short summary
Short summary
We present intrinsic details of dinocyst taxa and assemblages from the sole available central Arctic late Paleocene–early Eocene sedimentary succession recovered at the central Lomonosov Ridge by the Integrated Ocean Drilling Program (IODP) Expedition 302. We develop a pragmatic taxonomic framework, document critical biostratigraphic events, and propose two new genera and seven new species.
Peter K. Bijl and Henk Brinkhuis
J. Micropalaeontol., 42, 309–314, https://doi.org/10.5194/jm-42-309-2023, https://doi.org/10.5194/jm-42-309-2023, 2023
Short summary
Short summary
We developed an online, open-access database for taxonomic descriptions, stratigraphic information and images of organic-walled dinoflagellate cyst species. With this new resource for applied and academic research, teaching and training, we open up organic-walled dinoflagellate cysts for the academic era of open science. We expect that palsys.org represents a starting point to improve taxonomic concepts, and we invite the community to contribute.
Mallory Pilie, Martha E. Gibson, Ingrid C. Romero, Noelia B. Nuñez Otaño, Matthew J. Pound, Jennifer M. K. O'Keefe, and Sophie Warny
J. Micropalaeontol., 42, 291–307, https://doi.org/10.5194/jm-42-291-2023, https://doi.org/10.5194/jm-42-291-2023, 2023
Short summary
Short summary
The ANDRILL SMS site provides the first Middle Miocene Antarctic fungal record. The CREST plant-based paleoclimate reconstructions confirm an intensification of the hydrological cycle during the MCO, with the Ross Sea region reconstructed 279 % wetter than modern conditions and a maximum mean annual temperature of 10.3 °C for the warmest intervals of the MCO. The plant-based reconstructions indicate a temperate, no dry season with a warm summer (Cfb) Köppen–Geiger climate classification.
Yord W. Yedema, Timme Donders, Francien Peterse, and Francesca Sangiorgi
J. Micropalaeontol., 42, 257–276, https://doi.org/10.5194/jm-42-257-2023, https://doi.org/10.5194/jm-42-257-2023, 2023
Short summary
Short summary
The pollen and dinoflagellate cyst content of 21 surface sediments from the northern Gulf of Mexico is used to test the applicability of three palynological ratios (heterotroph/autotroph, pollen/dinocyst, and pollen/bisaccate ratio) as proxies for marine productivity and distance to the coast/river. Redundancy analysis confirms the suitability of these three ratios, where the H/A ratio can be used as an indicator of primary production, and the P/B ratio best tracks the distance to the coast.
Lena Mareike Thöle, Peter Dirk Nooteboom, Suning Hou, Rujian Wang, Senyan Nie, Elisabeth Michel, Isabel Sauermilch, Fabienne Marret, Francesca Sangiorgi, and Peter Kristian Bijl
J. Micropalaeontol., 42, 35–56, https://doi.org/10.5194/jm-42-35-2023, https://doi.org/10.5194/jm-42-35-2023, 2023
Short summary
Short summary
Dinoflagellate cysts can be used to infer past oceanographic conditions in the Southern Ocean. This requires knowledge of their present-day ecologic affinities. We add 66 Antarctic-proximal surface sediment samples to the Southern Ocean data and derive oceanographic conditions at those stations. Dinoflagellate cysts are clearly biogeographically separated along latitudinal gradients of temperature, sea ice, nutrients, and salinity, which allows us to reconstruct these parameters for the past.
Manuel Vieira and Salih Mahdi
J. Micropalaeontol., 39, 155–167, https://doi.org/10.5194/jm-39-155-2020, https://doi.org/10.5194/jm-39-155-2020, 2020
Short summary
Short summary
This paper describes a new species of the genus Desmocysta from the Late Cretaceous in the Norwegian Sea. The short stratigraphic range for this new species makes it a good biostratigraphic marker. The available published data also indicate that this genus is restricted to higher latitudes in the Northern Hemisphere and is suggested to have preferred turbid waters and stressed marine environments.
Kasia K. Śliwińska and Martin J. Head
J. Micropalaeontol., 39, 139–154, https://doi.org/10.5194/jm-39-139-2020, https://doi.org/10.5194/jm-39-139-2020, 2020
Short summary
Short summary
We described two new species of the fossil dinoflagellate cyst genus Svalbardella. S. clausii sp. nov. has a narrow range in the lowermost Chattian and may be related to cooler surface waters. S. kareniae sp. nov. ranges from Lower Oligocene to Lower Miocene and favours more open marine conditions.
Our study illustrates the close phylogenetic relationship between Svalbardella and Palaeocystodinium and shows that surface ornamentation and the tabulation are variable features within both genera.
Marcelo Augusto De Lira Mota, Guy Harrington, and Tom Dunkley Jones
J. Micropalaeontol., 39, 1–26, https://doi.org/10.5194/jm-39-1-2020, https://doi.org/10.5194/jm-39-1-2020, 2020
Short summary
Short summary
New high-resolution microfossil record from a clay succession in the US Gulf Coastal Plain reveal more accurate age estimates for the critical Eocene–Oligocene transition (EOT), a global climate event marked by the rapid expansion of the first permanent Antarctic ice sheet 34 million years ago. These data suggest a coeval major increase in sedimentation rate. Future isotopic and palaeoecological work on this core can be more precisely integrated with other global records of the EOT.
Kasia K. Śliwińska
J. Micropalaeontol., 38, 143–176, https://doi.org/10.5194/jm-38-143-2019, https://doi.org/10.5194/jm-38-143-2019, 2019
Short summary
Short summary
This study provides an age model based on dinocysts for the early Oligocene succession from the North Sea. The changes in the dinocysts assemblage show that the succession was deposited in a proximal and dynamic environment. Furthermore, the results suggests that the early icehouse climate played an important role in the depositional development of the Oligocene succession in the North Sea basin.
Phillip E. Jardine, William D. Gosling, Barry H. Lomax, Adele C. M. Julier, and Wesley T. Fraser
J. Micropalaeontol., 38, 83–95, https://doi.org/10.5194/jm-38-83-2019, https://doi.org/10.5194/jm-38-83-2019, 2019
Short summary
Short summary
Many major food crops, including rice, wheat, maize, rye, barley, oats and millet, are domesticated species of grass. However, because grass pollen all looks highly similar, it has been challenging to track grass domestication using pollen in archaeological samples. Here, we show that we can use the chemical signature of pollen grains to classify different grass species. This approach has the potential to help unravel the spread of domestication and agriculture over the last 10 000 years.
Thomas M. Hoyle, Manuel Sala-Pérez, and Francesca Sangiorgi
J. Micropalaeontol., 38, 55–65, https://doi.org/10.5194/jm-38-55-2019, https://doi.org/10.5194/jm-38-55-2019, 2019
Short summary
Short summary
Morphology of dinoflagellate cysts (which are valuable tools in deciphering past environmental and climate changes) depends not only on genetics, but also on a range of environmental factors. We review frequently occurring (Black Sea) morphotypes and propose use of matrices to record gradual variation between endmember forms as a pragmatic approach until cyst–theca studies and genetic sequencing can demonstrate relationships between genetically and environmentally controlled morphotypes.
Sonal Khanolkar and Jyoti Sharma
J. Micropalaeontol., 38, 1–24, https://doi.org/10.5194/jm-38-1-2019, https://doi.org/10.5194/jm-38-1-2019, 2019
Short summary
Short summary
We carried out comparative analyses of multiple microfossil groups like foraminifera, dinoflagellates, pollen and spores from Early and Middle Eocene lignite mine sections from paleotropical sites of the Cambay, Kutch and Barmer basins of western India in order to record the changes in paleovegetation and paleodepositional conditions during the hot and humid climate.
Julian D. Hartman, Peter K. Bijl, and Francesca Sangiorgi
J. Micropalaeontol., 37, 445–497, https://doi.org/10.5194/jm-37-445-2018, https://doi.org/10.5194/jm-37-445-2018, 2018
Short summary
Short summary
We present an extensive overview of the organic microfossil remains found at Site U1357, Adélie Basin, East Antarctica. The organic microfossil remains are exceptionally well preserved and are derived from unicellular as well as higher organisms. We provide a morphological description, photographic images, and a discussion of the ecological preferences of the biological species from which the organic remains were derived.
Peter K. Bijl, Alexander J. P. Houben, Anja Bruls, Jörg Pross, and Francesca Sangiorgi
J. Micropalaeontol., 37, 105–138, https://doi.org/10.5194/jm-37-105-2018, https://doi.org/10.5194/jm-37-105-2018, 2018
Short summary
Short summary
In order to use ocean sediments as a recorder of past oceanographic changes, a critical first step is to stratigraphically date the sediments. The absence of microfossils with known stratigraphic ranges has always hindered dating of Southern Ocean sediments. Here we tie dinocyst ranges to the international timescale in a well-dated sediment core from offshore Antarctica. With this, we can now use dinocysts as a biostratigraphic tool in otherwise stratigraphically poorly dated sediments.
Cited articles
Amoo, M., Salzmann, U., Pound, M. J., Thompson, N., and Bijl, P. K.: Eocene to Oligocene vegetation and climate in the Tasmanian Gateway region controlled by changes in ocean currents and pCO2, Clim. Past Discuss. [preprint], https://doi.org/10.5194/cp-2021-131, in review, 2021.
Bijl, P. K., Pross, J., Warnaar, J., Stickley, C. E., Huber, M., Guerstein,
R., Houben, A. J., Sluijs, A., Visscher, H., and Brinkhuis, H.:
Environmental forcings of Paleogene Southern Ocean dinoflagellate
biogeography, Paleoceanography, 26, PA1202,
https://doi.org/10.1029/2009PA001905, 2011.
Bijl, P. K., Bendle, J. A., Bohaty, S. M., Pross, J., Schouten, S., Tauxe,
L., Stickley, C. E., McKay, R. M., Rohl, U., Olney, M., Sluijs, A., Escutia,
C., Brinkhuis, H., and Expedition 318 scientists: Eocene cooling linked to early flow
across the Tasmanian Gateway, P. Natl. Acad. Sci. USA, 110, 9645–9650,
https://doi.org/10.1073/pnas.1220872110, 2013.
Bijl, P. K., Houben, A. J., Hartman, J. D., Pross, J., Salabarnada, A.,
Escutia, C., and Sangiorgi, F.: Paleoceanography and ice sheet variability
offshore Wilkes Land, Antarctica-Part 2: Insights from Oligocene-Miocene
dinoflagellate cyst assemblages, Clim. Past, 14, 1015–1033,
https://doi.org/10.5194/cp-14-1015-2018, 2018.
Boreham, C., Blevin, J., Duddy, I., Newman, J., Liu, K., Middleton, H.,
Macphail, M., and Cook, A.: Exploring the potential for oil generation,
migration and accumulation in Cape Sorell–1, Sorell Basin, offshore West
Tasmania, APPEA J., 42, 405–435, https://doi.org/10.1071/AJ01022,
2002.
Brinkhuis, H.: Late Eocene to Early Oligocene dinoflagellate cysts from the
Priabonian type-area (Northeast Italy): biostratigraphy and
paleoenvironmental interpretation, Palaeogeogr. Palaeocl., 107, 121–163, https://doi.org/10.1016/0031-0182(94)90168-6,
1994.
Brinkhuis, H. and Biffi, U.: Dinoflagellate cyst stratigraphy of the
Eocene/Oligocene transition in central Italy, Mar. Micropaleontol., 22,
131–183, https://doi.org/10.1016/0377-8398(93)90007-K, 1993.
Brinkhuis, H., Munsterman, D., Sengers, S., Sluijs, A., Warnaar, J., and
Williams, G.: Late Eocene to Quaternary dinoflagellate cysts from ODP Site 1168, Off western Tasmania, Proceedings of the Ocean Drilling Program,
Scientific Results, 189, 1–36,
https://doi.org/10.2973/odp.proc.sr.189.105.2003, 2003.
Cande, S. C. and Stock, J. M.: Pacific–Antarctic–Australia motion and
the formation of the Macquarie Plate, Geophys. J. Int.,
157, 399–414, https://doi.org/10.1111/j.1365-246X.2004.02224.x, 2004.
Carter, R.: The mid-Oligocene Marshall Paraconformity, New Zealand:
coincidence with global eustatic sea-level fall or rise?, J.
Geol., 93, 359–371, https://doi.org/10.1086/628957, 1985.
Clowes, C. D., Hannah, M. J., Wilson, G. J., and Wrenn, J. H.: Marine
palynostratigraphy and new species from the Cape Roberts drill-holes,
Victoria land basin, Antarctica, Mar. Micropaleontol., 126, 65–84,
https://doi.org/10.1016/j.marmicro.2016.06.003, 2016.
Crouch, E., Mildenhall, D., and Neil, H.: Distribution of organic-walled
marine and terrestrial palynomorphs in surface sediments, offshore eastern
New Zealand, Mar. Geol., 270, 235–256,
https://doi.org/10.1016/j.earscirev.2019.102961, 2010.
Dale, B.: Dinoflagellate cyst ecology: modeling and geological applications,
Palynology: principles and applications, AASP Found., College Station,
Texas, USA, 1249–1275, 1996.
De Schepper, S. and Head, M. J.: New late Cenozoic acritarchs: evolution,
palaeoecology and correlation potential in high latitude oceans, J.
System. Palaeontol., 12, 493–519,
https://doi.org/10.1080/14772019.2013.783883, 2014.
De Schepper, S., Fischer, E. I., Groeneveld, J., Head, M. J., and
Matthiessen, J.: Deciphering the palaeoecology of Late Pliocene and Early
Pleistocene dinoflagellate cysts, Palaeogeogr. Palaeocl., 309, 17–32, https://doi.org/10.1016/j.palaeo.2011.04.020,
2011.
Egger, L. M., Bahr, A., Friedrich, O., Wilson, P. A., Norris, R. D., Van
Peer, T. E., Lippert, P. C., Liebrand, D., and Pross, J.: Sea-level and
surface-water change in the western North Atlantic across the
Oligocene–Miocene Transition: a palynological perspective from IODP Site
U1406 (Newfoundland margin), Mar. Micropaleontol., 139, 57–71,
https://doi.org/10.1016/j.marmicro.2017.11.003, 2018.
Evangelinos, D., Escutia, C., Etourneau, J., Hoem, F., Bijl, P., Boterblom,
W., van de Flierdt, T., Valero, L., Flores, J.-A., Rodriguez-Tovar, F. J.,
Jimenez-Espejo, F. J., Salabarnada, A., and López-Quirós, A.: Late
Oligocene-Miocene proto-Antarctic Circumpolar Current dynamics off the
Wilkes Land margin, East Antarctica, Glob. Planet. Change, 191,
103221, https://doi.org/10.1016/j.gloplacha.2020.103221, 2020.
Evitt, W. R.: A discussion and proposals concerning fossil dinoflagellates,
hystrichospheres, and acritarchs, I, P. Natl. Acad.
Sci. USA, 49, 158–164, 1963.
Exon, N. F., Kennett, J. P., Malone, M. J., and the Leg189 Shipboard Scientific Party: Leg 189 summary,
Proceedings of the Ocean Drilling Program Initial Reports, Ocean Drilling
Program, College Station, TX, USA, 2001a.
Exon, N. F., Kennett, J. P., Malone, M. J., and the Leg189 Shipboard Scientific Party: Site 1168. ,
Proceedings of the Ocean Drilling Program Initial Reports, Ocean Drilling
Program, College Station, TX, USA,, 2001b.
Exon, N. F., Kennett, J. P., and Malone, M. J.: Leg 189 synthesis:
Cretaceous–Holocene history of the Tasmanian gateway, Proceedings of the
ocean drilling program, Scientific Results, 189, 1–37,
https://doi.org/10.2973/odp.proc.sr.189.101.2004, 2004.
Fensome, R. A.: A classification of living and fossil dinoflagellates,
Micropaleontology, Special Publication, 7, 1–351, 1993.
Frieling, J. and Sluijs, A.: Towards quantitative environmental
reconstructions from ancient non-analogue microfossil assemblages:
Ecological preferences of Paleocene – Eocene dinoflagellates, Earth-Sci.
Rev., 185, 956–973, https://doi.org/10.1016/j.earscirev.2018.08.014,
2018.
Fulthorpe, C. S., Carter, R. M., Miller, K. G., and Wilson, J.: Marshall
Paraconformity: a mid-Oligocene record of inception of the Antarctic
circumpolar current and coeval glacio-eustatic lowstand?, Mar.
Petrol. Geol., 13, 61–77, https://doi.org/10.1016/0264-8172(95)00033-X,
1996.
Galeotti, S., DeConto, R., Naish, T., Stocchi, P., Florindo, F., Pagani, M.,
Barrett, P., Bohaty, S. M., Lanci, L., Pollard, D., Sandroni, S., Talarico,
F. M., and Zachos, J. C.: Antarctic Ice Sheet variability across the
Eocene-Oligocene boundary climate transition, Science, 352, 76–80,
https://doi.org/10.1126/science.aab0669, 2016.
Gallagher, S. J., Villa, G., Drysdale, R. N., Wade, B. S., Scher, H., Li,
Q., Wallace, M. W., and Holdgate, G. R.: A near-field sea level record of
East Antarctic Ice Sheet instability from 32 to 27 Myr, Paleoceanography,
28, 1–13, https://doi.org/10.1029/2012PA002326, 2013.
Gallagher, S. J., Wade, B., Qianyu, L., Holdgate, G. R., Bown, P.,
Korasidis, V. A., Scher, H., Houben, A. J., McGowran, B., and Allan, T.:
Eocene to Oligocene high paleolatitude neritic record of Oi-1 glaciation in
the Otway Basin southeast Australia, Glob. Planet. Change, 191,
103218, https://doi.org/10.1016/j.gloplacha.2020.103218, 2020.
Gillard, M., Autin, J., Manatschal, G., Sauter, D., Munschy, M., and
Schaming, M.: Tectonomagmatic evolution of the final stages of rifting along
the deep conjugate Australian-Antarctic magma-poor rifted margins:
Constraints from seismic observations, Tectonics, 34, 753–783,
https://doi.org/10.1002/2015TC003850, 2015.
Gradstein, F. M., Ogg, J. G., Schmitz, M. D., and Ogg, G. M.: The Geologic Time Scale 2012, The Geologic Time Scale, 2, 437–1144, 2012.
Greenwood, D. R. and Wing, S. L.: Eocene continental climates and
latitudinal temperature gradients, Geology, 23, 1044–1048, 1995.
Guerstein, G. R., Guler, M. V., Williams, G. L., Fensome, R. A., and Chiesa, J. O.: Middle Palaeogene dinoflagellate cysts from Tierra del Fuego, Argentina: biostratigraphy and palaeoenvironments, J. Micropalaeontol., 27, 75–94, https://doi.org/10.1144/jm.27.1.75, 2008.
Hannah, M., Wrenn, J., and Wilson, G.: Early Miocene and Quaternary marine
palynomorphs from Cape Roberts Project CRP-1, McMurdo Sound, Antarctica,
Terra Antartica, 5, 527–538, 1998.
Hannah, M., Wilson, G., and Wrenn, J.: Oligocene and miocene marine
palynomorphs from CRP-2/2A, Victoria Land Basin, Antarctica, Terra
Antartica, 7, 503–511, 2000.
Hannah, M. J.: The palynology of ODP site 1165, Prydz Bay, East Antarctica:
a record of Miocene glacial advance and retreat, Palaeogeogr.
Palaeocl., 231, 120–133,
https://doi.org/10.1016/j.palaeo.2005.07.029, 2006.
Harland, R. and Pudsey, C. J.: Dinoflagellate cysts from sediment traps
deployed in the Bellingshausen, Weddell and Scotia seas, Antarctica, Mar.
Micropaleontol., 37, 77–99, 1999.
Hartman, J. D., Bijl, P. K., and Sangiorgi, F.: A review of the ecological
affinities of marine organic microfossils from a Holocene record offshore of
Adélie Land (East Antarctica), J. Micropalaeontol., 37,
445–497, https://doi.org/10.5194/jm-37-445-2018, 2018a.
Hartman, J. D., Sangiorgi, F., Salabarnada, A., Peterse, F., Houben, A. J. P., Schouten, S., Brinkhuis, H., Escutia, C., and Bijl, P. K.: Paleoceanography and ice sheet variability offshore Wilkes Land, Antarctica – Part 3: Insights from Oligocene–Miocene TEX86-based sea surface temperature reconstructions, Clim. Past, 14, 1275–1297, https://doi.org/10.5194/cp-14-1275-2018, 2018b.
Head, M.: Modern dinoflagellate cysts and their biological affinities,
Palynology, 3, 1197–1248, 1996.
Hill, D. J., Haywood, A. M., Valdes, P. J., Francis, J. E., Lunt, D. J.,
Wade, B. S., and Bowman, V. C.: Paleogeographic controls on the onset of the
Antarctic circumpolar current, Geophys. Res. Lett., 40, 5199–5204,
https://doi.org/10.1002/grl.50941, 2013.
Hill, P., Meixner, A., Moore, A., and Exon, N.: Structure and development of
the west Tasmanian offshore sedimentary basins: results of recent marine and
aeromagnetic surveys, Austr. J. Earth Sci., 44, 579–596,
https://doi.org/10.1080/08120099708728338, 1997.
Hill, P. J. and Exon, N. F.: Tectonics and basin development of the offshore
Tasmanian area incorporating results from deep ocean drilling, Washington DC
American Geophysical Union, Geophysical Monograph Series, 151, 19–42,
https://doi.org/10.1029/151GM03, 2004.
Hochmuth, K., Gohl, K., Leitchenkov, G., Sauermilch, I., Whittaker, J. M.,
Uenzelmann-Neben, G., Davy, B., and De Santis, L.: The evolving
paleobathymetry of the circum-Antarctic Southern Ocean since 34 Ma – a key to
understanding past cryosphere-ocean developments, Geochem. Geophy.
Geosy., 11, e2020GC009122, https://doi.org/10.1029/2020GC009122, 2020.
Hoem, F. S., Valero, L., Evangelinos, D., Escutia, C., Duncan, B., McKay, R.
M., Brinkhuis, H., Sangiorgi, F., and Bijl, P. K.: Temperate Oligocene
surface ocean conditions offshore of Cape Adare, Ross Sea, Antarctica,
Clim. Past, 17, 1423–1442,
https://doi.org/10.5194/cp-17-1423-2021, 2021a.
Hoem, F. S., Sauermilch, I., Hou, S., Brinkhuis, H., Sangiorgi, F., and Bijl, P. K.: Late Eocene–early Miocene evolution of the southern Australian Subtropical Front: a marine palynological approach, Zenodo [data set], https://doi.org/10.5281/zenodo.5529715, 2021b.
Holdgate, G., Sluiter, I., and Taglieri, J.: Eocene-Oligocene coals of the
Gippsland and Australo-Antarctic basins–Paleoclimatic and paleogeographic
context and implications for the earliest Cenozoic glaciations,
Palaeogeogr. Palaeocl., 472, 236–255,
https://doi.org/10.1016/j.palaeo.2017.01.035, 2017.
Houben, A. J., Bijl, P. K., Pross, J., Bohaty, S. M., Passchier, S.,
Stickley, C. E., Rohl, U., Sugisaki, S., Tauxe, L., van de Flierdt, T.,
Olney, M., Sangiorgi, F., Sluijs, A., Escutia, C., Brinkhuis, H., and Expedition 318 scientists: Reorganization of
Southern Ocean plankton ecosystem at the onset of Antarctic glaciation,
Science, 340, 341–344, https://doi.org/10.1126/science.1223646, 2013.
Houben, A. J. P., Bijl, P. K., Sluijs, A., Schouten, S., and Brinkhuis, H.:
Late Eocene Southern Ocean Cooling and Invigoration of Circulation
Preconditioned Antarctica for Full-Scale Glaciation, Geochem.
Geophy. Geosy., 20, 2214–2234, https://doi.org/10.1029/2019gc008182,
2019.
Huber, M., Brinkhuis, H., Stickley, C. E., Döös, K., Sluijs, A.,
Warnaar, J., Schellenberg, S. A., and Williams, G. L.: Eocene circulation of
the Southern Ocean: Was Antarctica kept warm by subtropical waters?,
Paleoceanography, 19, 4, https://doi.org/10.1029/2004PA001014, 2004.
Hutchinson, D. K., Coxall, H. K., Lunt, D. J., Steinthorsdottir, M., de
Boer, A. M., Baatsen, M., von der Heydt, A., Huber, M., Kennedy-Asser, A.
T., and Kunzmann, L.: The Eocene–Oligocene transition: a review of marine
and terrestrial proxy data, models and model–data comparisons, Clim. Past, 17, 269–315, https://doi.org/10.5194/cp-17-269-2021, 2021.
Lawver, L. A., Gahagan, L. M., and Coffin, M. F.: The development of
paleoseaways around Antarctica, Ant. Res. Ser., 56, 7–30, 1992.
Louwye, S., Foubert, A., Mertens, K., and Van Rooij, D.: Integrated
stratigraphy and palaeoecology of the Lower and Middle Miocene of the
Porcupine Basin, Geol. Mag., 145, 321–344,
https://doi.org/110.1017/S0016756807004244, 2008.
Marret, F., Bradley, L., de Vernal, A., Hardy, W., Kim, S.-Y., Mudie, P.,
Penaud, A., Pospelova, V., Price, A. M., Radi, T., and Rochon, A.: From
bi-polar to regional distribution of modern dinoflagellate cysts, an
overview of their biogeography, Mar. Micropaleontol., 159, 101753,
https://doi.org/10.1016/j.marmicro.2019.101753, 2020.
Matthews, K. J., Maloney, K. T., Zahirovic, S., Williams, S. E., Seton, M.,
and Mueller, R. D.: Global plate boundary evolution and kinematics since the
late Paleozoic, Glob. Planet. Change, 146, 226–250,
https://doi.org/10.1016/j.gloplacha.2016.10.002, 2016.
McCarthy, A., Falloon, T., Sauermilch, I., Whittaker, J., Niida, K., and
Green, D.: Revisiting the Australian-Antarctic ocean-continent transition
zone using petrological and geophysical characterization of exhumed
subcontinental mantle, Geochem. Geophy. Geosy., 21,
e2020GC009040, https://doi.org/10.1029/2020GC009040, 2020.
McGowran, B., Holdgate, G., Li, Q., and Gallagher, S.: Cenozoic
stratigraphic succession in southeastern Australia, Austr. J.
Earth Sci., 51, 459–496,
https://doi.org/10.1111/j.1400-0952.2004.01078.x, 2004.
Mertens, K. N., Verhoeven, K., Verleye, T., Louwye, S., Amorim, A., Ribeiro,
S., Deaf, A. S., Harding, I. C., De Schepper, S., and González, C.:
Determining the absolute abundance of dinoflagellate cysts in recent marine
sediments: the Lycopodium marker-grain method put to the test, Rev. Palaeobot.
Palyno., 157, 238–252, https://doi.org/10.1016/j.revpalbo.2009.05.004, 2009.
Miller, J. M., Norvick, M. S., and Wilson, C. J.: Basement controls on
rifting and the associated formation of ocean transform faults – Cretaceous
continental extension of the southern margin of Australia, Tectonophysics,
359, 131–155, https://doi.org/10.1016/S0040-1951(02)00508-5, 2002.
Miller, K. G., Wright, J. D., and Fairbanks, R. G.: Unlocking the ice house:
Oligocene-Miocene oxygen isotopes, eustasy, and margin erosion, J.
Geophys. Res.-Sol. Ea., 96, 6829–6848,
https://doi.org/10.1029/90JB02015, 1991.
Mudie, P.: Neogene and quaternary dinoflagellate cysts and acritarchs,
Second Symposium on Neogene Dinoflagellates, American Association of
Stratigraphic Palynologists, Dallas, USA, 347–390, 1992.
Mudie, P. J., Marret, F., Gurdebeke, P. R., Hartman, J. D., and Reid, P. C.:
Marine dinocysts, acritarchs and less well-known NPP: tintinnids, ostracod
and foraminiferal linings, copepod and worm remains, Geol. Soc.
Lond. Sp. Publ., 511, 159–232, https://doi.org/10.1144/SP511-2020-55,
2021.
Müller, R. D., Cannon, J., Qin, X., Watson, R. J., Gurnis, M., Williams,
S., Pfaffelmoser, T., Seton, M., Russell, S. H., and Zahirovic, S.: GPlates:
building a virtual Earth through deep time, Geochem. Geophy.
Geosy., 19, 2243–2261, https://doi.org/10.1029/2018GC007584, 2018.
Müntener, O., Manatschal, G., Desmurs, L., and Pettke, T.: Plagioclase
peridotites in ocean–continent transitions: refertilized mantle domains
generated by melt stagnation in the shallow mantle lithosphere, J.
Petrol., 51, 255–294, https://doi.org/10.1093/petrology/egp087, 2010.
Nelson, C. S. and Cooke, P. J.: History of oceanic front development in the New Zealand sector of the Southern Ocean during the Cenozoic – a synthesis, New Zealand J. Geol. Geophys., 44, 535–553, https://doi.org/10.1080/00288306.2001.9514954, 2001.
Orsi, A. H., Whitworth, T., and Nowlin, W. D.: On the meridional extent and
fronts of the Antarctic Circumpolar Current, Deep-Sea Res. Pt. I, 42, 641–673,
https://doi.org/10.1016/0967-0637(95)00021-w, 1995.
Palike, H., Norris, R. D., Herrle, J. O., Wilson, P. A., Coxall, H. K.,
Lear, C. H., Shackleton, N. J., Tripati, A. K., and Wade, B. S.: The
heartbeat of the Oligocene climate system, Science, 314, 1894–1898,
https://doi.org/10.1126/science.1133822, 2006.
Parke, M., Boalch, G., Jowett, R., and Harbour, D.: The genus Pterosperma
(Prasinophyceae): species with a single equatorial ala, J.
Mar. Biol. Assoc. UK, 58, 239–276,
https://doi.org/10.1017/S0025315400024528, 1978.
Pascher, K. M., Hollis, C. J., Bohaty, S. M., Cortese, G., McKay, R. M.,
Seebeck, H., Suzuki, N., and Chiba, K.: Expansion and diversification of
high-latitude radiolarian assemblages in the late Eocene linked to a cooling
event in the southwest Pacific, Clim. Past, 11, 1599–1620,
https://doi.org/10.5194/cp-11-1599-2015, 2015.
Pekar, S. F., Christie-Blick, N., Kominz, M. A., and Miller, K. G.:
Calibration between eustatic estimates from backstripping and oxygen
isotopic records for the Oligocene, Geology, 30, 903–906,
https://doi.org/10.1130/0091-7613(2002)030<0903:CBEEFB>2.0.CO;2, 2002.
Pfuhl, H. A. and McCave, I. N.: Integrated age models for the early
Oligocene-early Miocene, sites 1168 and 1170–1172, Proc. ODP, Sci. Results,
189, 1–21, https://doi.org/10.2973/odp.proc.sr.189.108.2003, 2003.
Prebble, J., Raine, J., Barrett, P., and Hannah, M.: Vegetation and climate
from two Oligocene glacioeustatic sedimentary cycles (31 and 24 Ma) cored by
the Cape Roberts Project, Victoria Land Basin, Antarctica, Palaeogeogr.
Palaeocl., 231, 41–57,
https://doi.org/10.1016/j.palaeo.2005.07.025, 2006.
Prebble, J. G., Crouch, E. M., Carter, L., Cortese, G., Bostock, H., and
Neil, H.: An expanded modern dinoflagellate cyst dataset for the Southwest
Pacific and Southern Hemisphere with environmental associations, Mar.
Micropaleontol., 101, 33–48,
https://doi.org/10.1016/j.marmicro.2013.04.004, 2013.
Pross, J. and Brinkhuis, H.: Organic-walled dinoflagellate cysts as
paleoenvironmental indicators in the Paleogene; a synopsis of concepts,
Palaont. Z., 79, 53–59,
https://doi.org/10.1007/BF03021753, 2005.
Pross, J., Contreras, L., Bijl, P. K., Greenwood, D. R., Bohaty, S. M.,
Schouten, S., Bendle, J. A., Röhl, U., Tauxe, L., and Raine, J. I.:
Persistent near-tropical warmth on the Antarctic continent during the early
Eocene epoch, Nature, 488, 73–77, https://doi.org/10.1038/nature11300, 2012.
Ridgway, K. and Condie, S.: The 5500-km-long boundary flow off western and
southern Australia, J. Geophys. Res.-Ocean., 109, C04017,
https://doi.org/10.1029/2003JC001921, 2004.
Röhl, U., Brinkhuis, H., Sluijs, A., and Fuller, M.: On the search for
the Paleocene/Eocene boundary in the Southern Ocean: exploring ODP Leg 189
Holes 1171D and 1172D, Tasman Sea, The Cenozoic Southern Ocean: Tectonics,
Sesimentation, and Climate Change Between Australia and Antarctica,
Geophys. Monogr. Ser., 151, 113–125, https://doi.org/10.1029/151GM08,
2004.
Salabarnada, A., Escutia, C., Röhl, U., Nelson, C. H., McKay, R.,
Jiménez-Espejo, F. J., Bijl, P. K., Hartman, J. D., Strother, S. L., and
Salzmann, U.: Paleoceanography and ice sheet variability offshore Wilkes
Land, Antarctica – Part 1: Insights from late Oligocene astronomically paced
contourite sedimentation, Clim. Past, 14, 991–1014,
https://doi.org/10.5194/cp-14-991-2018, 2018.
Sangiorgi, F., Bijl, P. K., Passchier, S., Salzmann, U., Schouten, S.,
McKay, R., Cody, R. D., Pross, J., van de Flierdt, T., Bohaty, S. M., Levy,
R., Williams, T., Escutia, C., and Brinkhuis, H.: Southern Ocean warming and
Wilkes Land ice sheet retreat during the mid-Miocene, Nat. Commun., 9, 317–328,
https://doi.org/10.1038/s41467-017-02609-7, 2018.
Sauermilch, I., Whittaker, J. M., Bijl, P. K., Totterdell, J., and Jokat,
W.: Tectonic, oceanographic, and climatic controls on the
Cretaceous-Cenozoic sedimentary record of the Australian-Antarctic Basin,
J. Geophys. Res.-Sol. Ea., 124, 7699–7724,
https://doi.org/10.1029/2018JB016683, 2019a.
Sauermilch, I., Mateo, Z. R. P., and Boaga, J.: A comparative analysis of
time–depth relationships derived from scientific ocean drilling
expeditions, Mar. Geophys. Res., 40, 635–641,
https://doi.org/10.1007/s11001-019-09393-7, 2019b.
Sauermilch, I., Whittaker, J. M., Klocker, A., Munday, D. R., Hochmuth, K.,
LaCasce, J. H., and Bijl, P.: Gateway-driven Southern Ocean cooling – The
crucial role of ocean gyres, Nat. Commun., https://doi.org/10.1038/s41467-021-26658-1, 2021.
Scher, H. D., Whittaker, J. M., Williams, S. E., Latimer, J. C., Kordesch, W. E. C., and Delaney, M. L.: Onset of Antarctic Circumpolar Current 30 million years ago as Tasmanian Gateway aligned with westerlies, Nature, 523, 580, https://doi.org/10.1038/nature14598, 2015.
Schreck, M. and Matthiessen, J.: Batiacasphaera micropapillata:
Palaeobiogeographic distribution and palaeoecological implications of a
critical Neogene species complex, Biological and Geological Perspectives of
Dinoflagellates, The Micropalaeontological Society, Sp. Publ.
Geol. Soc. Lond., 5, 301–314, 2013.
Sijp, W. P., Anna, S., Dijkstra, H. A., Flögel, S., Douglas, P. M., and
Bijl, P. K.: The role of ocean gateways on cooling climate on long time
scales, Glob. Planet. Change, 119, 1–22,
https://doi.org/10.1016/j.gloplacha.2014.04.004, 2014.
Sijp, W. P., Heydt, A. S., and Bijl, P. K.: Model simulations of early
westward flow across the Tasman Gateway during the early Eocene, Clim. Past, 12, 807–817, https://doi.org/10.5194/cp-12-807-2016, 2016.
Sluijs, A., Brinkhuis, H., Stickley, C., Warnaar, J., Williams, G., and
Fuller, M.: Dinoflagellate cysts from the Eocene/Oligocene transition in the
Southern Ocean; results from ODP Leg 189, Proceedings of the Ocean Drilling
Program, Scientific Results, 189, 1–42,
https://doi.org/10.2973/odp.proc.sr.189.104.2003, 2003.
Sluijs, A., Pross, J., and Brinkhuis, H.: From greenhouse to icehouse;
organic-walled dinoflagellate cysts as paleoenvironmental indicators in the
Paleogene, Earth-Sci. Rev., 68, 281–315,
https://doi.org/10.1016/j.earscirev.2004.06.001, 2005.
Stickley, C. E., Brinkhuis, H., Schellenberg, S. A., Sluijs, A., Röhl,
U., Fuller, M., Grauert, M., Huber, M., Warnaar, J., and Williams, G. L.:
Timing and nature of the deepening of the Tasmanian Gateway,
Paleoceanography, 19, PA4027, https://doi.org/10.1029/2004pa001022, 2004a.
Stickley, C. E, Brinkhuis, H., McGonigal, K., Chaproniere, G., Fuller, M.,
Kelly, D., Nürnberg, D., Pfuhl, H., Schellenberg, S., and Schönfeld,
J.: Late Cretaceous–Quaternary biomagnetostratigraphy of ODP Sites 1168,
1170, 1171, and 1172, Tasmanian Gateway, Proceedings of the Ocean Drilling
Program, Scientific Results, 189, 1–57,
https://doi.org/10.2973/odp.proc.sr.189.111.2004, 2004b.
Stover, L., Brinkhuis, H., Damassa, S., De Verteuil, L., Helby, R., Monteil,
E., Partridge, A., Powell, A., Riding, J., and Smelror, M.:
Mesozoic-Tertiary dinoflagellates, acritarchs and prasinophytes, Palynology, 2, 641–750, 1996.
van Hinsbergen, D. J., de Groot, L. V., van Schaik, S. J., Spakman, W.,
Bijl, P. K., Sluijs, A., Langereis, C. G., and Brinkhuis, H.: A
Paleolatitude Calculator for Paleoclimate Studies, PLoS One, 10, e0126946,
https://doi.org/10.1371/journal.pone.0126946, 2015.
van Simaeys, S., Brinkhuis, H., Pross, J. r., Williams, G. L., and Zachos,
J. C.: Arctic dinoflagellate migrations mark the strongest Oligocene
glaciations, Geology, 33, 709–712, https://doi.org/10.1130/G21634.1, 2005.
Wall, D. and Dale, B.: “Living fossils” in western Atlantic plankton,
Nature, 211, 1025–1026, 1966.
Wall, D., Dale, B., Lohmann, G., and Smith, W. K.: The environmental and
climatic distribution of dinoflagellate cysts in modern marine sediments
from regions in the North and South Atlantic Oceans and adjacent seas,
Mar. Micropaleontol., 2, 121–200, 1977.
Warny, S., Wrenn, J. H., Bart, P. J., and Askin, R.: Palynology of the
NBP03–01A transect in the Northern Basin, western Ross Sea, Antarctica: A
late Pliocene record, Palynology, 30, 151–182,
https://doi.org/10.1080/01916122.2006.9989624, 2006.
Warny, S., Kymes, C. M., Askin, R. A., Krajewski, K. P., and Bart, P. J.:
Remnants of Antarctic vegetation on King George Island during the early
Miocene Melville glaciation, Palynology, 40, 66–82,
https://doi.org/10.1080/01916122.2014.999954, 2016.
Weatherall, P., Marks, K. M., Jakobsson, M., Schmitt, T., Tani, S., Arndt,
J. E., Rovere, M., Chayes, D., Ferrini, V., and Wigley, R.: A new digital
bathymetric model of the world's oceans, Earth Space Sci., 2,
331–345, https://doi.org/10.1002/2015EA000107, 2015.
Westerhold, T., Marwan, N., Drury, A. J., Liebrand, D., Agnini, C.,
Anagnostou, E., Barnet, J. S. K., Bohaty, S. M., De Vleeschouwer, D.,
Florindo, F., Frederichs, T., Hodell, D. A., Holbourn, A. E., Kroon, D.,
Lauretano, V., Littler, K., Lourens, L. J., Lyle, M., Palike, H., Rohl, U.,
Tian, J., Wilkens, R. H., Wilson, P. A., and Zachos, J. C.: An
astronomically dated record of Earth's climate and its predictability over
the last 66 million years, Science, 369, 1383–1387,
https://doi.org/10.1126/science.aba6853, 2020.
Whittaker, J. M., Williams, S. E., and Müller, R. D.: Revised tectonic
evolution of the Eastern Indian Ocean, Geochem. Geophy. Geosy.,
14, 1891–1909, https://doi.org/10.1002/ggge.20120, 2013.
Williams, G. L., Fensome, R. A., and Macrae, R.: The Lentin and Williams
index of fossil dinoflagellates 2017 Edition, American Association of
Stratigraphic Palynologists Foundation
(AASP), Contributions Series Number 48, Dallas, Texas, USA, 2017.
Williams, S. E., Whittaker, J. M., Halpin, J. A., and Müller, R. D.:
Australian-Antarctic breakup and seafloor spreading: Balancing geological
and geophysical constraints, Earth-Sci. Rev., 188, 41–58,
https://doi.org/10.1016/j.earscirev.2018.10.011, 2019.
Wrenn, J. H. and Beckman, S. W.: Maceral, total organic carbon, and
palynological analyses of ross ice shelf project site j9 cores, Science,
216, 187–189, https://doi.org/10.1126/science.216.4542.187, 1982.
Young, J. R., Bown P. R., and Lees J. A.: mikrotax website. International
Nannoplankton Association, available at:
https://www.mikrotax.org (last access: 19 Juni 2019), 2017.
Zachos, J. C., Stott, L. D., and Lohmann, K. C.: Evolution of early Cenozoic
marine temperatures, Paleoceanography, 9, 353–387,
https://doi.org/10.1029/93PA03266, 1994.
Zonneveld, K. A. F., Versteegh, G. J. M., Kasten, S., Eglinton, T. I.,
Emeis, K. C., Huguet, C., Koch, B. P., de Lange, G. J., de Leeuw, J. W.,
Middelburg, J. J., Mollenhauer, G., Prahl, F. G., Rethemeyer, J., and
Wakeham, S. G.: Selective preservation of organic matter in marine
environments; processes and impact on the sedimentary record,
Biogeosciences, 7, 483–511, https://doi.org/10.5194/bg-7-483-2010, 2010.
Zonneveld, K. A. F., Marret, F., Versteegh, G. J. M., Bogus, K., Bonnet, S.,
Bouimetarhan, I., Crouch, E., de Vernal, A., Elshanawany, R., Edwards, L.,
Esper, O., Forke, S., Grøsfjeld, K., Henry, M., Holzwarth, U., Kielt,
J.-F., Kim, S.-Y., Ladouceur, S., Ledu, D., Chen, L., Limoges, A., Londeix,
L., Lu, S. H., Mahmoud, M. S., Marino, G., Matsouka, K., Matthiessen, J.,
Mildenhal, D. C., Mudie, P., Neil, H. L., Pospelova, V., Qi, Y., Radi, T.,
Richerol, T., Rochon, A., Sangiorgi, F., Solignac, S., Turon, J.-L.,
Verleye, T., Wang, Y., Wang, Z., and Young, M.: Atlas of modern
dinoflagellate cyst distribution based on 2405 data points, Rev. Palaeobot.
Palyno., 191, 1–197, https://doi.org/10.1016/j.revpalbo.2012.08.003, 2013.
Short summary
We use marine microfossil (dinocyst) assemblage data as well as seismic and tectonic investigations to reconstruct the oceanographic history south of Australia 37–20 Ma as the Tasmanian Gateway widens and deepens. Our results show stable conditions with typically warmer dinocysts south of Australia, which contrasts with the colder dinocysts closer to Antarctica, indicating the establishment of modern oceanographic conditions with a strong Southern Ocean temperature gradient and frontal systems.
We use marine microfossil (dinocyst) assemblage data as well as seismic and tectonic...
