Articles | Volume 37, issue 2
https://doi.org/10.5194/jm-37-403-2018
© Author(s) 2018. 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-37-403-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Assessing proxy signatures of temperature, salinity, and hypoxia in the Baltic Sea through foraminifera-based geochemistry and faunal assemblages
Jeroen Groeneveld
CORRESPONDING AUTHOR
Center for Marine Environmental Sciences (MARUM), University of
Bremen, Klagenfurter Strasse 2–4, 28359 Bremen, Germany
Department of Geology, Lund University, Sölvegatan 12, 223 62
Lund, Sweden
Helena L. Filipsson
Department of Geology, Lund University, Sölvegatan 12, 223 62
Lund, Sweden
William E. N. Austin
School of Geography and Sustainable Development, University of St.
Andrews, North Street, St. Andrews, KY16 9AL, UK
Scottish Association for Marine Science, Scottish Marine Institute,
Oban, PA37 1AQ, UK
Kate Darling
School of Geography and Sustainable Development, University of St.
Andrews, North Street, St. Andrews, KY16 9AL, UK
School of Geosciences, University of Edinburgh, James Hutton Road,
Edinburgh, EH9 3FE, UK
David McCarthy
School of Geography and Sustainable Development, University of St.
Andrews, North Street, St. Andrews, KY16 9AL, UK
Nadine B. Quintana Krupinski
Department of Geology, Lund University, Sölvegatan 12, 223 62
Lund, Sweden
Clare Bird
School of Geosciences, University of Edinburgh, James Hutton Road,
Edinburgh, EH9 3FE, UK
Biological and Environmental Sciences, University of Stirling,
Stirling, FK9 4LA, UK
Magali Schweizer
School of Geosciences, University of Edinburgh, James Hutton Road,
Edinburgh, EH9 3FE, UK
LPG-BIAF UMR CNRS 6112, University of Angers, 2 bd Lavoisier, 49045
Angers CEDEX 01, France
Related authors
Lukas Jonkers, Tonke Strack, Montserrat Alonso-Garcia, Simon D'haenens, Robert Huber, Michal Kucera, Iván Hernández-Almeida, Chloe L. C. Jones, Brett Metcalfe, Rajeev Saraswat, Lóránd Silye, Sanjay K. Verma, Muhamad Naim Abd Malek, Gerald Auer, Cátia F. Barbosa, Maria A. Barcena, Karl-Heinz Baumann, Flavia Boscolo-Galazzo, Joeven Austine S. Calvelo, Lucilla Capotondi, Martina Caratelli, Jorge Cardich, Humberto Carvajal-Chitty, Markéta Chroustová, Helen K. Coxall, Renata M. de Mello, Anne de Vernal, Paula Diz, Kirsty M. Edgar, Helena L. Filipsson, Ángela Fraguas, Heather L. Furlong, Giacomo Galli, Natalia L. García Chapori, Robyn Granger, Jeroen Groeneveld, Adil Imam, Rebecca Jackson, David Lazarus, Julie Meilland, Marína Molčan Matejová, Raphael Morard, Caterina Morigi, Sven N. Nielsen, Diana Ochoa, Maria Rose Petrizzo, Andrés S. Rigual-Hernández, Marina C. Rillo, Matthew L. Staitis, Gamze Tanık, Raúl Tapia, Nishant Vats, Bridget S. Wade, and Anna E. Weinmann
J. Micropalaeontol., 44, 145–168, https://doi.org/10.5194/jm-44-145-2025, https://doi.org/10.5194/jm-44-145-2025, 2025
Short summary
Short summary
Our study provides guidelines improving the reuse of marine microfossil assemblage data, which are valuable for understanding past ecosystems and environmental change. Based on a survey of 113 researchers, we identified key data attributes required for effective reuse. Analysis of a selection of datasets available online reveals a gap between the attributes scientists consider essential and the data currently available, highlighting the need for clearer data documentation and sharing practices.
Babette A.A. Hoogakker, Catherine Davis, Yi Wang, Stephanie Kusch, Katrina Nilsson-Kerr, Dalton S. Hardisty, Allison Jacobel, Dharma Reyes Macaya, Nicolaas Glock, Sha Ni, Julio Sepúlveda, Abby Ren, Alexandra Auderset, Anya V. Hess, Katrin J. Meissner, Jorge Cardich, Robert Anderson, Christine Barras, Chandranath Basak, Harold J. Bradbury, Inda Brinkmann, Alexis Castillo, Madelyn Cook, Kassandra Costa, Constance Choquel, Paula Diz, Jonas Donnenfield, Felix J. Elling, Zeynep Erdem, Helena L. Filipsson, Sebastián Garrido, Julia Gottschalk, Anjaly Govindankutty Menon, Jeroen Groeneveld, Christian Hallmann, Ingrid Hendy, Rick Hennekam, Wanyi Lu, Jean Lynch-Stieglitz, Lélia Matos, Alfredo Martínez-García, Giulia Molina, Práxedes Muñoz, Simone Moretti, Jennifer Morford, Sophie Nuber, Svetlana Radionovskaya, Morgan Reed Raven, Christopher J. Somes, Anja S. Studer, Kazuyo Tachikawa, Raúl Tapia, Martin Tetard, Tyler Vollmer, Xingchen Wang, Shuzhuang Wu, Yan Zhang, Xin-Yuan Zheng, and Yuxin Zhou
Biogeosciences, 22, 863–957, https://doi.org/10.5194/bg-22-863-2025, https://doi.org/10.5194/bg-22-863-2025, 2025
Short summary
Short summary
Paleo-oxygen proxies can extend current records, constrain pre-anthropogenic baselines, provide datasets necessary to test climate models under different boundary conditions, and ultimately understand how ocean oxygenation responds on longer timescales. Here we summarize current proxies used for the reconstruction of Cenozoic seawater oxygen levels. This includes an overview of the proxy's history, how it works, resources required, limitations, and future recommendations.
Raúl Tapia, Sze Ling Ho, Hui-Yu Wang, Jeroen Groeneveld, and Mahyar Mohtadi
Biogeosciences, 19, 3185–3208, https://doi.org/10.5194/bg-19-3185-2022, https://doi.org/10.5194/bg-19-3185-2022, 2022
Short summary
Short summary
We report census counts of planktic foraminifera in depth-stratified plankton net samples off Indonesia. Our results show that the vertical distribution of foraminifera species routinely used in paleoceanographic reconstructions varies in hydrographically distinct regions, likely in response to food availability. Consequently, the thermal gradient based on mixed layer and thermocline dwellers also differs for these regions, suggesting potential implications for paleoceanographic reconstructions.
Lukas Jonkers, Geert-Jan A. Brummer, Julie Meilland, Jeroen Groeneveld, and Michal Kucera
Clim. Past, 18, 89–101, https://doi.org/10.5194/cp-18-89-2022, https://doi.org/10.5194/cp-18-89-2022, 2022
Short summary
Short summary
The variability in the geochemistry among individual foraminifera is used to reconstruct seasonal to interannual climate variability. This method requires that each foraminifera shell accurately records environmental conditions, which we test here using a sediment trap time series. Even in the absence of environmental variability, planktonic foraminifera display variability in their stable isotope ratios that needs to be considered in the interpretation of individual foraminifera data.
Zhaojia Liu, Nicole S. Khan, Howard K. Y. Yu, Magali Schweizer, Jennifer S. Walker, and Celia Schunter
J. Micropalaeontol., 45, 679–698, https://doi.org/10.5194/jm-45-679-2026, https://doi.org/10.5194/jm-45-679-2026, 2026
Short summary
Short summary
We studied how genetic material from foraminifera in Hong Kong mangroves and mudflats varies through seasons and how this affects records of past sea levels. Over 2 years, communities in mangroves were relatively stable, allowing accurate estimates of elevation relative to the sea. The mudflat–mangrove transitional zone changed with season, causing biased estimates. Mangroves are therefore more accurate than mudflats for tracking past sea-level change.
Helen K. Coxall, Thomas M. Cronin, Kate Darling, Katrine Husum, Tamara Handl, Brian T. Huber, Megh M. Kanvinde, Mohammad Razmjooei, Flor Vermassen, Antje H. L. Voelker, Tirza M. Weitkamp, and Matt O'Regan
J. Micropalaeontol., 45, 581–622, https://doi.org/10.5194/jm-45-581-2026, https://doi.org/10.5194/jm-45-581-2026, 2026
Short summary
Short summary
Today’s sea-ice-covered Arctic Ocean hosts only one species of calcifying planktonic foraminifera, unlike warmer oceans with diverse communities. Fossils show that other species once inhabited the Arctic, but their identities and environmental significance remain uncertain. Using detailed microscopy and hundreds of shell measurements, we resolve these fossil species and establish a new taxonomic framework providing the foundation for improved reconstructions of Quaternary Arctic climate history.
Florian Börgel, Itzel Ruvalcaba Baroni, Leonie Barghorn, Leonard Borchert, Bronwyn Cahill, Cyril Dutheil, Leonie Esters, Małgorzata Falarz, Helena L. Filipsson, Matthias Gröger, Jari Hänninen, Magnus Hieronymus, Erko Jakobson, Mehdi Pasha Karami, Karol Kuliński, Taavi Liblik, H. E. Markus Meier, Gabriele Messori, Lev Naumov, Thomas Neumann, Piia Post, Gregor Rehder, Anna Rutgersson, and Georg Sebastian Voelker
Earth Syst. Dynam., 17, 415–450, https://doi.org/10.5194/esd-17-415-2026, https://doi.org/10.5194/esd-17-415-2026, 2026
Short summary
Short summary
This review explains how weather patterns, guided by the polar jet stream, influence the Baltic Sea’s climate and ecosystem. It covers the North Atlantic Oscillation, blocking events and other processes and discusses how they affect temperature, rainfall, and storms from days to decades. These shifts then impact oxygen levels, productivity, and acidification in the Baltic Sea. Physical links are fairly well known, but biogeochemical pathways remain uncertain.
Constance Choquel, Emmanuelle Geslin, Edouard Metzger, Bruno Jesus, Antoine Prins, Emilie Houliez, Magali Schweizer, Thierry Jauffrais, Éric Bénéteau, and Aurélia Mouret
J. Micropalaeontol., 45, 51–72, https://doi.org/10.5194/jm-45-51-2026, https://doi.org/10.5194/jm-45-51-2026, 2026
Short summary
Short summary
We studied how tiny shelled organisms called foraminifera living in coastal mudflats respond to changes in their microscopic algae food. By monitoring a French mudflat every month for 3 years, we showed that seasonal environmental changes strongly shape both algae and foraminifera. Using simple algae traits such as size and shape explained feeding patterns better than identifying algae species, offering a clearer way to predict ecosystem responses to environmental change.
Alex Houston, Mark H. Garnett, and William E. N. Austin
Biogeosciences, 22, 4851–4864, https://doi.org/10.5194/bg-22-4851-2025, https://doi.org/10.5194/bg-22-4851-2025, 2025
Short summary
Short summary
Saltmarshes accumulate carbon through plant growth and older material deposited during tidal inundation. We found that more energy was required to decompose old carbon than younger carbon, and the youngest carbon was also the most susceptible to decomposition in a degradation scenario. Protecting saltmarshes can help prevent carbon losses and reduce CO2 emissions. Including this vulnerable stored carbon in climate policies and carbon credit systems could make them more accurate and effective.
Clare Bird, Kate Darling, Rabecca Thiessen, and Anna J. Pieńkowski
Biogeosciences, 22, 4545–4577, https://doi.org/10.5194/bg-22-4545-2025, https://doi.org/10.5194/bg-22-4545-2025, 2025
Short summary
Short summary
The polar planktonic foraminifer Neogloboquadrina pachyderma eats diatoms. Unlike other planktonic species, it also keeps the diatom chloroplasts (photosynthesising organelles) inside its cell. In benthic foraminifera, this is known as kleptoplasty, and the roles of these stolen chloroplasts are diverse. Their role in N. pachyderma needs to be investigated to find out if stored chloroplasts enable N. pachyderma to live in polar waters and under the ice, where no other planktonic species survive.
Lukas Jonkers, Tonke Strack, Montserrat Alonso-Garcia, Simon D'haenens, Robert Huber, Michal Kucera, Iván Hernández-Almeida, Chloe L. C. Jones, Brett Metcalfe, Rajeev Saraswat, Lóránd Silye, Sanjay K. Verma, Muhamad Naim Abd Malek, Gerald Auer, Cátia F. Barbosa, Maria A. Barcena, Karl-Heinz Baumann, Flavia Boscolo-Galazzo, Joeven Austine S. Calvelo, Lucilla Capotondi, Martina Caratelli, Jorge Cardich, Humberto Carvajal-Chitty, Markéta Chroustová, Helen K. Coxall, Renata M. de Mello, Anne de Vernal, Paula Diz, Kirsty M. Edgar, Helena L. Filipsson, Ángela Fraguas, Heather L. Furlong, Giacomo Galli, Natalia L. García Chapori, Robyn Granger, Jeroen Groeneveld, Adil Imam, Rebecca Jackson, David Lazarus, Julie Meilland, Marína Molčan Matejová, Raphael Morard, Caterina Morigi, Sven N. Nielsen, Diana Ochoa, Maria Rose Petrizzo, Andrés S. Rigual-Hernández, Marina C. Rillo, Matthew L. Staitis, Gamze Tanık, Raúl Tapia, Nishant Vats, Bridget S. Wade, and Anna E. Weinmann
J. Micropalaeontol., 44, 145–168, https://doi.org/10.5194/jm-44-145-2025, https://doi.org/10.5194/jm-44-145-2025, 2025
Short summary
Short summary
Our study provides guidelines improving the reuse of marine microfossil assemblage data, which are valuable for understanding past ecosystems and environmental change. Based on a survey of 113 researchers, we identified key data attributes required for effective reuse. Analysis of a selection of datasets available online reveals a gap between the attributes scientists consider essential and the data currently available, highlighting the need for clearer data documentation and sharing practices.
Irina Polovodova Asteman, Emilie Jaffré, Agata Olejnik, Maria Holzmann, Mary McGann, Kjell Nordberg, Jean-Charles Pavard, Delia Rösel, and Magali Schweizer
J. Micropalaeontol., 44, 119–143, https://doi.org/10.5194/jm-44-119-2025, https://doi.org/10.5194/jm-44-119-2025, 2025
Short summary
Short summary
Small boat harbours are suggested to cause pollution and alien species introductions. Here we analysed surface sediments in Hinsholmskilen harbour (Sweden) for benthic foraminifera and potentially toxic elements. Molecular and morphological analyses of foraminifera show the presence of two alien species, Trochammina hadai and Ammonia confertitesta, whilst pollution is mostly low for Cd, Co, Ni, and Pb. In contrast, As, Zn, Cu, Hg, and Cr have high levels due to the use of these elements in boat paints.
Flor Vermassen, Clare Bird, Tirza M. Weitkamp, Kate F. Darling, Hanna Farnelid, Céline Heuzé, Allison Y. Hsiang, Salar Karam, Christian Stranne, Marcus Sundbom, and Helen K. Coxall
Biogeosciences, 22, 2261–2286, https://doi.org/10.5194/bg-22-2261-2025, https://doi.org/10.5194/bg-22-2261-2025, 2025
Short summary
Short summary
We provide the first systematic survey of planktonic foraminifera in the high Arctic Ocean. Our results describe the abundance and species composition under summer sea ice. They indicate that the polar specialist N. pachyderma is the only species present, with subpolar species absent. The data set will be a valuable reference for continued monitoring of the state of planktonic foraminifera communities as they respond to the ongoing sea-ice decline and the “Atlantification” of the Arctic Ocean.
Babette A.A. Hoogakker, Catherine Davis, Yi Wang, Stephanie Kusch, Katrina Nilsson-Kerr, Dalton S. Hardisty, Allison Jacobel, Dharma Reyes Macaya, Nicolaas Glock, Sha Ni, Julio Sepúlveda, Abby Ren, Alexandra Auderset, Anya V. Hess, Katrin J. Meissner, Jorge Cardich, Robert Anderson, Christine Barras, Chandranath Basak, Harold J. Bradbury, Inda Brinkmann, Alexis Castillo, Madelyn Cook, Kassandra Costa, Constance Choquel, Paula Diz, Jonas Donnenfield, Felix J. Elling, Zeynep Erdem, Helena L. Filipsson, Sebastián Garrido, Julia Gottschalk, Anjaly Govindankutty Menon, Jeroen Groeneveld, Christian Hallmann, Ingrid Hendy, Rick Hennekam, Wanyi Lu, Jean Lynch-Stieglitz, Lélia Matos, Alfredo Martínez-García, Giulia Molina, Práxedes Muñoz, Simone Moretti, Jennifer Morford, Sophie Nuber, Svetlana Radionovskaya, Morgan Reed Raven, Christopher J. Somes, Anja S. Studer, Kazuyo Tachikawa, Raúl Tapia, Martin Tetard, Tyler Vollmer, Xingchen Wang, Shuzhuang Wu, Yan Zhang, Xin-Yuan Zheng, and Yuxin Zhou
Biogeosciences, 22, 863–957, https://doi.org/10.5194/bg-22-863-2025, https://doi.org/10.5194/bg-22-863-2025, 2025
Short summary
Short summary
Paleo-oxygen proxies can extend current records, constrain pre-anthropogenic baselines, provide datasets necessary to test climate models under different boundary conditions, and ultimately understand how ocean oxygenation responds on longer timescales. Here we summarize current proxies used for the reconstruction of Cenozoic seawater oxygen levels. This includes an overview of the proxy's history, how it works, resources required, limitations, and future recommendations.
William Hiles, Lucy C. Miller, Craig Smeaton, and William E. N. Austin
Biogeosciences, 21, 929–948, https://doi.org/10.5194/bg-21-929-2024, https://doi.org/10.5194/bg-21-929-2024, 2024
Short summary
Short summary
Saltmarsh soils may help to limit the rate of climate change by storing carbon. To understand their impacts, they must be accurately mapped. We use drone data to estimate the size of three saltmarshes in NE Scotland. We find that drone imagery, combined with tidal data, can reliably inform our understanding of saltmarsh size. When compared with previous work using vegetation communities, we find that our most reliable new estimates of stored carbon are 15–20 % smaller than previously estimated.
K. Mareike Paul, Martijn Hermans, Sami A. Jokinen, Inda Brinkmann, Helena L. Filipsson, and Tom Jilbert
Biogeosciences, 20, 5003–5028, https://doi.org/10.5194/bg-20-5003-2023, https://doi.org/10.5194/bg-20-5003-2023, 2023
Short summary
Short summary
Seawater naturally contains trace metals such as Mo and U, which accumulate under low oxygen conditions on the seafloor. Previous studies have used sediment Mo and U contents as an archive of changing oxygen concentrations in coastal waters. Here we show that in fjords the use of Mo and U for this purpose may be impaired by additional processes. Our findings have implications for the reliable use of Mo and U to reconstruct oxygen changes in fjords.
Christiane Schmidt, Emmanuelle Geslin, Joan M. Bernhard, Charlotte LeKieffre, Mette Marianne Svenning, Helene Roberge, Magali Schweizer, and Giuliana Panieri
Biogeosciences, 19, 3897–3909, https://doi.org/10.5194/bg-19-3897-2022, https://doi.org/10.5194/bg-19-3897-2022, 2022
Short summary
Short summary
This study is the first to show non-selective deposit feeding in the foraminifera Nonionella labradorica and the possible uptake of methanotrophic bacteria. We carried out a feeding experiment with a marine methanotroph to examine the ultrastructure of the cell and degradation vacuoles using transmission electron microscopy (TEM). The results revealed three putative methanotrophs at the outside of the cell/test, which could be taken up via non-targeted grazing in seeps or our experiment.
Raúl Tapia, Sze Ling Ho, Hui-Yu Wang, Jeroen Groeneveld, and Mahyar Mohtadi
Biogeosciences, 19, 3185–3208, https://doi.org/10.5194/bg-19-3185-2022, https://doi.org/10.5194/bg-19-3185-2022, 2022
Short summary
Short summary
We report census counts of planktic foraminifera in depth-stratified plankton net samples off Indonesia. Our results show that the vertical distribution of foraminifera species routinely used in paleoceanographic reconstructions varies in hydrographically distinct regions, likely in response to food availability. Consequently, the thermal gradient based on mixed layer and thermocline dwellers also differs for these regions, suggesting potential implications for paleoceanographic reconstructions.
Inda Brinkmann, Christine Barras, Tom Jilbert, Tomas Næraa, K. Mareike Paul, Magali Schweizer, and Helena L. Filipsson
Biogeosciences, 19, 2523–2535, https://doi.org/10.5194/bg-19-2523-2022, https://doi.org/10.5194/bg-19-2523-2022, 2022
Short summary
Short summary
The concentration of the trace metal barium (Ba) in coastal seawater is a function of continental input, such as riverine discharge. Our geochemical records of the severely hot and dry year 2018, and following wet year 2019, reveal that prolonged drought imprints with exceptionally low Ba concentrations in benthic foraminiferal calcium carbonates of coastal sediments. This highlights the potential of benthic Ba / Ca to trace past climate extremes and variability in coastal marine records.
Lukas Jonkers, Geert-Jan A. Brummer, Julie Meilland, Jeroen Groeneveld, and Michal Kucera
Clim. Past, 18, 89–101, https://doi.org/10.5194/cp-18-89-2022, https://doi.org/10.5194/cp-18-89-2022, 2022
Short summary
Short summary
The variability in the geochemistry among individual foraminifera is used to reconstruct seasonal to interannual climate variability. This method requires that each foraminifera shell accurately records environmental conditions, which we test here using a sediment trap time series. Even in the absence of environmental variability, planktonic foraminifera display variability in their stable isotope ratios that needs to be considered in the interpretation of individual foraminifera data.
Cited articles
Alve, E.: Colonization of new habitats by benthic foraminifera: A review,
Earth Sci. Rev.,
46, 167–185, 1999.
Alve, E. and Murray, J. W.: Marginal marine environments of the Skagerrak
and Kattegat: a
baseline study of living (stained) benthic foraminiferal ecology,
Palaeogeogr.
Palaeocl., 146, 171–193, 1999.
Andrén, T., Jørgensen, B. B., Cotterill, C., and Expedition 347
Scientists: Baltic Sea Paleoenvironment, Proc. IODP, 347, College Station, TX (Integrated Ocean Drilling Program),
https://doi.org/10.2204/iodp.proc.347.2015, 2015.
Anjar, J., Adrielsson, L., Bennike, O., Björck, S., Filipsson, H. L.,
Groeneveld, J., Knudsen, K. L.,
Larsen, N. K., and Möller, P.: Palaeoenvironmental history of the Baltic
Sea basin during
Marine Isotope Stage 3, Quaternary Sci. Rev., 34, 81–92, 2012.
Austin, W. E. N., Cage, A. G., and Scourse, J. D.: Mid-latitude shelf seas:
a NW European perspective
on the seasonal dynamics of temperature, salinity, and oxygen isotopes,
Holocene, 16,
937–947, 2006.
Bahr, A., Schönfeld, J., Hofmann, J., Voigt, S., Aurahs, R., Kucera, M.,
Flögel, S., Jentzen, A., and
Gerdes, A.: Comparison of Ba∕Ca and δ18Owater as
freshwater proxies: A multi-species
core-top study on planktonic foraminifera from the vicinity of the Orinoco
River mouth, Earth
Planet. Sc. Lett., 383, 45–57, 2013.
Barker, S., Greaves, M., and Elderfield, H.: A study of cleaning procedures
used for foraminiferal
Mg∕Ca paleothermometry, Geochem. Geophys. Geosys., 4, 8407,
https://doi.org/10.1029/2003GC000559,
2003.
Barras, C., Mouret, A., Nardelli, M. P., Metzger, E., Petersen, J., La, C.,
Filipsson, H. L., and Jorissen, F.:
Experimental calibration of manganese incorporation in foraminiferal
calcite, Geochim. Cosmochim. Ac., 237, 49–64, 2018.
Barrientos, N., Lear, C. H., Jakobsson, M., Stranne, C., O'Regan, M.,
Cronin, T. M., Gukov, A. Y., and
Coxall, H. K.: Arctic Ocean benthic foraminifera Mg∕Ca ratios and global
Mg∕Ca-temperature calibrations: New constraints at low temperatures, Geochim.
Cosmochim. Ac., 236, 240–259,
https://doi.org/10.1016/j.gca.2018.02.036, 2018.
Bauch, H. A., Erlenkeuser, H., Bauch, D., Mueller-Lupp, T., and Taldenkova,
E.: Stable oxygen and
carbon isotopes in modern benthic foraminifera from the Laptev Sea shelf:
implications for
reconstructing proglacial and profluvial environments in the Arctic, Mar. Micropaleontol., 51, 285–300, 2004.
Bemis, B. E., Spero, H. J., Bijma, J., and Lea, D. W.: Reevaluation of the
oxygen isotopic composition of
planktonic foraminifera: Experimental results and revised paleotemperature
equations,
Paleoceanography, 13, 150–160, 1998.
Bernard, P. C., van Grieken, R. E., and Brügmann, L.: Geochemistry of
suspended matter from the
Baltic Sea. 1. Results of individual particle characterization by automated
electron
microprobe, Mar. Chem., 26, 155–177, 1989.
Björck, S.: A review of the history of the Baltic Sea, 13.0–8.0 ka BP,
Quat. Internat., 27, 19–40, 1995.
Björck, S.: The late quaternary development of the Baltic Sea Basin, in:
Assessment of Climate Change for the Baltic Sea Basin, edited by: The BACC Author Team, Springer-Verlag, Berlin-Heidelberg, 398–407, 2008.
Boström, K., Wiborg, L., and Ingri, J.: Geochemistry and origin of
ferromanganese concretions in the
Gulf of Bothnia, Mar. Geol., 50, 1–24, 1982.
Branson, O., Redfern, S. A. T., Tyliszczak, T., Sadekov, A., Langer, G.,
Kimoto, K., and Elderfield, H.: The
coordination of Mg in foraminiferal calcite, Earth Planet. Sc. Lett., 383,
134–141, 2013.
Burdige, D. J.: The biogeochemistry of manganese and iron reduction in
marine sediments, Earth Sci. Rev., 35, 249–284, 1993.
Burton, J. D., Statham, P. J., and Elderfield, H.: Trace metals as tracers
in the ocean, Philos.
T. R. Soc. Lond., 325, 127–145, 1988.
Butruille, C., Krossa, V. R., Schwab, C., and Weinelt, M.: Reconstruction of
mid- to late-Holocene
winter temperatures in the Skagerrak region using benthic foraminiferal
Mg∕Ca and δ18O,
Holocene, 27, 1–10, https://doi.org/10.1177/0959683616652701, 2016.
Calvert, S. E. and Pedersen, T. F.: Geochemistry of recent oxic and anoxic
marine sediments:
Implications for the geological record, Mar. Geol., 113, 67–88, 1993.
Canfield, D. E., Thamdrup, B., and Hansen, J. W.: The anaerobic degradation
of organic matter in
Danish coastal sediments: Iron reduction, manganese reduction, and sulfate
reduction,
Geochim. Cosmochim. Ac., 57, 3867–3883, 1993.
Charrieau, L. M., Filipsson, H. L., Ljung, K., Chierici, M., Knudsen, K. L.,
and Kritzberg, E.: The effects of
multiple stressors on the distribution of coastal benthic foraminifera: A
case study from the
Skagerrak-Baltic Sea region, Mar. Micropaleontol., 139, 42–56, 2018.
Conley, D. J., Carstensen, J., Aigars, J., Axe, P., Bonsdorff, E., Eremina,
T., Haahti, B.-M., Humborg, C.,
Jonsson, P., Kotta, J., Lännegren, C., Larsson, U., Maximov, A., Medina,
M. R., Lysiak-Pastuszak, E., Remeikaite-Nikiene, N., Walve, J., Wilhelms, S., and
Zillén, L.: Hypoxia is
increasing in the coastal zone of the Baltic Sea, Environ. Sci. Technol., 45,
6777–6783, 2011.
Conradsen, K., Bergsten, H., Knudsen, K. L., Nordberg, K., and Seidenkrantz,
M. S.: Recent
benthic foraminiferal distribution in the Kattegat-Skagerrak, Scandinavia,
J. Foramin. Res., 32,
53–68, 1994.
Corliss, B. H.: Microhabitats of benthic foraminifera within deep-sea sediments, Nature, 314, 435–438, 1985.
Darling, K. F., Schweizer, M., Knudsen, K. L., Evans, K. M., Bird, C.,
Roberts, A., Filipsson, H. L., Kim, J.-H., Gudmundsson, G., Wade, C. M., Sayer, M. D., and Austin, W. E. N.: The
genetic diversity,
phylogeography and morphology of Elphidiidae (foraminifera) in the Northeast
Atlantic,
Mar. Micropaleontol., 129, 1–23, https://doi.org/10.1016/j.marmicro.2016.09.001,
2016.
Dekens, P. S., Lea, D. W., Pak, D. K., and Spero, H. J.: Core top
calibration of Mg∕Ca in tropical
foraminifera: Refining paleotemperature estimation, Geochem., Geophys,.
Geosys., 3, 1–29,
https://doi.org/10.1029/2001GC000200, 2002.
de Nooijer, L. J., Brombacher, A., Mewes, A., Langer, G., Nehrke, G., Bijma, J.,
and Reichart, G.-J.: Ba incorporation in benthic foraminifera, Biogeosciences, 14, 3387–3400, https://doi.org/10.5194/bg-14-3387-2017, 2017.
Diaz, R. J. and Rosenberg, R.: Spreading dead zones and consequences for
marine ecosystems,
Science, 321, 926–929, https://doi.org/10.1126/science.1156401, 2008.
Dijkstra, N., Quintana Krupinski, N. B., Yamane, M., Obrochta, S. P.,
Yokoyama, Y., and Slomp, C. P.:
Holocene refreshing and reoxygenation of a Bothnian Sea estuary led to
enhanced
phosphorus burial, Estuar. Coast., 41, 139–157, 2018.
Dissard, D., Nehrke, G., Reichart, G. J., and Bijma, J.: The impact of
salinity on the Mg∕Ca and Sr∕Ca
ratio in the benthic foraminifera Ammonia tepida: Results from culture experiments,
Geochim. Cosmochim. Ac., 74, 928–940, 2010.
Diz, P., Barras, C., Geslin, E., Reichart, G. J., Metzger, E., Jorissen, F.,
and Bijma, J.: Incorporation
of Mg and Sr and oxygen and carbon stable isotope fractionation in cultured
Ammonia tepida, Mar. Micropaleontol., 92–93, 16–28, 2012.
Dyrssen, D.: The Baltic-Kattegat-Skagerrak estuarine system, Estuaries, 16,
446–452, 1993.
Elderfield, H. and Ganssen, G.: Past temperatures and δ18O of
surface ocean waters inferred from
foraminiferal Mg∕Ca ratios, Nature, 405, 442–445, 2000.
Elderfield, H., Yu. J., Anand, P., Kiefer, T., and Nyland, B.: Calibrations
for benthic foraminiferal
Mg∕Ca paleothermometry and the carbonate ion hypothesis, Earth Planet. Sc.
Lett., 250, 633–649, https://doi.org/10.1016/j.epsl.2006.07.041, 2006.
Ellis, B. F. and Messina, A. R.: Catalogue of Foraminifera,
Micropaleontology Press, New York,
The American Museum of Natural History, 1940.
Epstein, S., Buchsbaum, R., Lowenstam, H. A., and Urey, H. C.: Revised
carbonate-water
isotopic temperature scale, Geol. Soc. Am. Bull., 64, 1315–1325,
1953.
Erbs-Hansen, D. R., Knudsen, K. L., Gary, A. C., Gyllencreutz, R., and
Jansen, E.: Holocene
climatic development in Skagerrak, eastern North Atlantic: Foraminiferal and
stable isotopic
evidence, Holocene, 22, 301–312, 2012.
Evans, D. and Müller, W.: Deep time foraminifera Mg∕Ca
paleothermometry: Nonlinear correction
for secular change in seawater Mg∕Ca, Paleoceanography, 27, PA4205,
https://doi.org/10.1029/2012PA002315, 2012.
Feyling-Hanssen, R. W.: Foraminifera in Late Quaternary Deposits from the
Oslofjord Area, Skrifter
(Norges geologiske undersøkelse), Universitetsforlaget, Oslo, 225, 1964.
Feyling-Hanssen, R. W.: The foraminifer Elphidium excavatum (Terquem) and its variant forms,
Micropaleontology, 18, 337–354, 1972.
Feyling-Hanssen, R. W., Jørgensen, J. A., Knudsen, K. L., and Andersen,
A. I.: Late Quaternary
foraminifera from Vendsyssel, Denmark and Sandnes, Norway, Bull. Geol. Soc.
Den., 21, 61–317, 1971.
Filipsson, H. L. and Nordberg, K.: Climate variations, an overlooked
factor influencing the
recent marine environment. An example from Gullmar Fjord, Sweden,
illustrated by benthic
foraminifera and hydrographic data, Estuaries, 27, 867–881, 2004a.
Filipsson, H. L. and Nordberg, K.: A 200-year environmental record of a
low-oxygen fjord,
Sweden, elucidated by benthic foraminifera, sediment characteristics and
hydrographic
data, J. Foram. Res., 34, 277–293, https://doi.org/10.2113/34.4.277, 2004b.
Filipsson, H. L., Nordberg, K., and Gustafsson, M.: Seasonal study of
δ18O and δ13C in living
(stained) benthic foraminifera from two Swedish fjords, Mar. Micropaleontol., 53,
159–172, 2004.
Filipsson, H. L., McCorkle, D. C., Mackensen, A., Bernhard, J. M.,
Andersson, L. S., Naustvoll, L. J.,
Caballero-Alfonso, A. M., Nordberg, K., and Danielssen, D. S.: Seasonal
variability of stable
carbon isotopes (δ13CDIC) in the Skagerrak and the Baltic
Sea: Distinguishing between mixing
and biological productivity, Palaeogeogr. Palaeocl., 483,
15–30, 2017.
Fontanier, C., Duros, P., Toyofuku, T., Oguri, K., Koho, K. A., Buscail, R.,
Gremare, A., Radakovitch, O., Deflandre, B., De Nooijer, L. J., Bichon, S., Goubet, S.,
Ivanovsky, A., Chabaud, G., Menniti, C., Reichart, G.-J., and Kitazato, H.: Living (stained) deep-sea foraminifera off Hachinohe
(NE Japan, Western
Pacific): Environmental interplay in oxygen-depleted ecosystems, J. Foram.
Res., 44, 281–299,
2014.
Froelich, P. N., Klinkhammer, G. P., Bender, M. L., Luedtke, N. A., Heath,
G. R., Cullen, D., Dauphin, P.,
Hammond, D., Hartman, B., and Maynard, V.: Early oxidation of organic matter
in
pelagic sediments of the eastern equatorial Atlantic: suboxic diagenesis,
Geochim.
Cosmochim. Ac., 43, 1075–1090, 1979.
Fröhlich, K., Grabczak, J., and Rozanski, K.: Deuterium and oxygen-18 in
the Baltic Sea, Chem. Geol.,
72, 77–83, 1988.
Geslin, E., Heinz, P., Jorissen, F., and Hemleben, Ch.: Migratory responses
of deep-sea benthic
foraminifera to variable oxygen conditions: laboratory investigations, Mar. Micropaleontol., 53,
227–243, 2004.
Glock, N., Eisenhauer, A., Liebetrau, V., Wiedenbeck, M., Hensen, C., and Nehrke, G.:
EMP and SIMS studies on Mn∕Ca and Fe∕Ca
systematics in benthic foraminifera from the Peruvian OMZ: a contribution to the
identification of potential redox proxies and the impact of cleaning
protocols, Biogeosciences, 9, 341–359, https://doi.org/10.5194/bg-9-341-2012, 2012.
Goldberg, T., Archer, C., Vance, D., Thamdrup, B., McAnena, A., and Poulton,
S. W.: Controls on Mo
isotope fractionation in a Mn-rich anoxic marine sediment, Gullmar Fjord,
Sweden, Chem.
Geol., 296–297, 73–82, 2012.
Grasshoff, K. and Voipio, A.: Chemical Oceanography, in: The Baltic Sea, edited by: Voipio, A.,
Elsevier
Oceanography Series 30, Amsterdam, 183–218, 1981.
Greaves, M., Caillon, N., Rebaubier, H., Bartoli, G., Bohaty, S., Cacho, I.,
Clarke, L., Cooper, M. Daunt, C., Delaney, M., deMenocal, P., Dutton, A., Eggins, S.,
Elderfield, H., Garbe-Schönberg, D., Goddard, E., Green, D., Groeneveld, J., Hastings, D.,
Hathorne, E., Kimoto, K., Klinkhammer, G., Labeyrie, L., Lea, D. W., Marchitto, T.,
Martinez-Boti, M. A., Mortyn, P. G., Ni, Y., Nürnberg, D., Paradis, G., Pena, L.,
Quinn, T., Rosenthal, Y., Russell, A., Sagawa, T., Sosdian, S., Stott, L., Tachikawa, K.,
Tappa, E., Thunell, R., and Wilson, P. A.: Interlaboratory comparison
study of calibration
standards for foraminiferal Mg∕Ca thermometry, Geochem. Geophys. Geosyst.,
9, Q08010, https://doi.org/10.1029/2008GC001974, 2008.
Groeneveld, J. and Filipsson, H. L.: Mg∕Ca and Mn∕Ca
ratios in benthic foraminifera: the potential to reconstruct past variations in
temperature and hypoxia in shelf regions, Biogeosciences, 10, 5125–5138, https://doi.org/10.5194/bg-10-5125-2013, 2013.
Grunert, P., Rosenthal, Y., Jorissen, F., Holbourn, A., Zhou, X., and
Piller, W.: Mg∕Ca-temperature
calibration for costate Bulimina species (B. costata, B. inflata, B. mexicana): A
paleothermometer for hypoxic environments, Geochim. Cosmochim. Ac., 220,
36–54, 2018.
Gustafsson, M. and Nordberg, K.: Living (stained) benthic foraminifera and
their response to the
seasonal hydrographic cycle, periodic hypoxia and to primary production in
Havstens
Fjord on the Swedish west coast, Estuar. Coast. Shelf Sci., 51, 743–761,
2000.
Gustafsson, B. G. and Westman, P.: On the causes for salinity variations in
the Baltic Sea
during the last 8500 years, Paleoceanography, 17, 1–14, https://doi.org/10.1029/2000PA000572,
2002.
Hall, J. M. and Chan, L. -H.: Li/Ca in multiple species of benthic and
planktonic foraminifera:
Thermocline, latitudinal, and glacial-interglacial variation, Geochim.
Cosmochim. Ac., 68, 529–545, 2004.
Hall, T. A.: BioEdit: a user-friendly biological sequence alignment editor
and analysis program for
Windows 95/98/NT, Nucl. Acid. S., 41, 95–98, 1999.
Hammer, Ø., Harper, D. A. T., and Ryan, P. D.: PAST: Paleontological
Statistics Software Package for
Education and Data Analysis, Palaeontol. Electron., 4, 4,
2001.
Hartman, M.: Zur Geochemie von Mangan und Eisen in der Ostsee, Meyniana, 14,
3–20, 1964.
Hathorne, E. C., James, R. H., and Lampitt, R. S.: Environmental versus
biomineralization controls on the intratest variation in the trace element
composition of the planktonic
foraminifera G. inflata and G. scitula, Paleoceanography, 24, PA4204, https://doi.org/10.1029/2009PA001742,
2009.
Havach, S. M., Chandler, G. T., Wilson-Fenelli, A., and Shaw, T. J.:
Experimental determination of
trace element partition coefficients in cultured benthic foraminifera,
Geochim. Cosmochim.
Ac., 65, 1277–1283, 2001.
Haynes, J. R.: Supposed pronounced ecophenotypy in foraminifera, J.
Micropaleontology, 11, 59–63,
1992.
Hayward, B. W., Holzmann, M., Grenfell, H. R., Pawlowski, J., and Triggs, C.
M.: Morphological distinction of molecular types in Ammonia – towards a taxonomic
revision of the world's most commonly misidentified foraminifera, Mar. Micropaleontol., 50, 237–271, 2004.
Hayward, B. W., Figueira, B. O., Sabaa, A. T., and Buzas, M. A.: Multi-year
life spans of high salt marsh agglutinated foraminifera from New Zealand,
Mar. Micropaleontol., 109, 54–65, 2014.
Hjalmarsson, S., Chierici, M., and Anderson, L. G.: Carbon dynamics in a
productive coastal region –
The Skagerrak, J. Mar. Sys., 82, 245–251, 2010.
Holzmann, M. and Pawlowski, J.: Taxonomic relationships in the genus
Ammonia (Foraminifera)
based on ribosomal DNA sequences, J. Micropaleont., 19, 85–95, 2000.
Holzmann, M. and Pawlowski, J.: An updated classification of rotaliid
foraminifera based on
ribosomal DNA phylogeny, Mar. Micropaleontol., 132, 18–34, 2017.
Hönisch, B., Allen, K. A., Russell, A. D., Eggins, S. M., Bijma, J.,
Spero, H. J., Lea, D. W., and Yu, J.:
Planktic foraminifers as recorders of sea water Ba∕Ca, Mar. Micropaleontol., 79,
52–57, 2011.
Huang, E., Mulitza, S., Paul, A., Groeneveld, J., Steinke, S., and Schulz,
M.: Response of eastern
tropical Atlantic central waters to Atlantic meridional overturning
circulation changes during
the Last Glacial Maximum and Heinrich Stadial 1, Paleoceanography, 27,
PA3229,
https://doi.org/10.1029/2012PA002294, 2012.
Huckriede, H. and Meischner, D.: Origin and environment of manganese-rich
sediments within black-shale basins, Geochim. Cosmochim. Ac., 60, 1399–1413, 1996.
Ingri, J., Löfvendahl, R., and Boström, K.: Chemistry of suspended
particles in the southern Baltic Sea,
Mar. Chem., 32, 73–87, 1991.
Jakobsson, M., Björck, S., Alm, G., Andrén, T., Lindeberg, G., and
Svensson, N. O.: Reconstructing the
Younger Dryas ice dammed lake in the Baltic Basin: bathymetry, area and
volume, Global
Planet. Change, 57, 355–370, 2007.
Jilbert, T. and Slomp, C. P.: Rapid high-amplitude variability in Baltic
Sea hypoxia during the
Holocene, Geology, 41, 1183–1186, 2013.
Jones, R. W.: Henry Bowman Brady (1835–1891): the man, the scientist and the
scientific legacy, in: Landmarks in Foraminiferal Micropalaeontology, History and Development, edited by: Bowden, J., Gregory, F. J., and Henderson, A. S., The
Micropalaentological Society,
Special Publications, Geological Society, London, 23–30, 2013.
Jorissen, F. J., de Stigter, H. C., and Widmark, J. G. V.: A conceptual
model explaining benthic
foraminiferal microhabitats, Mar. Micropaleontol., 26, 3–15, 1995.
Keeling, R. F. and Garcia, H. E.: The change in oceanic O2 inventory
associated with recent global
warming, P. Natl. Acad. Sci. USA, 99, 7848–7853, 2002.
Kisakürek, B., Eisenhauer, T., Böhm, F., Garbe-Schönberg, D.,
and Erez, J.: Controls on shell Mg∕Ca
and Sr∕Ca in cultured planktonic foraminifera, Globigerinoides ruber (white), Earth Planet. Sc.
Lett., 273, 260–269, https://doi.org/10.1016/j.epsl.2008.06.026, 2008.
Klinkhammer, G. P., Mix, A. C., and Haley, B. A.: Increased dissolved
terrestrial input to the coastal
ocean during the deglaciation, Geochem. Geophys. Geosys., 10, Q03009,
https://doi.org/10.1029/2008GC002219, 2009.
Koho, K. A., de Nooijer, L. J., and Reichart, G. J.: Combining benthic
foraminiferal ecology and shell
Mn∕Ca to deconvolve past bottom water oxygenation and paleoproductivity,
Geochim.
Cosmochim. Ac., 165, 294–306, 2015.
Koho, K. A., de Nooijer, L. J., Fontanier, C., Toyofuku, T., Oguri, K., Kitazato, H.,
and Reichart, G.-J.: Benthic foraminiferal Mn∕Ca ratios
reflect microhabitat preferences, Biogeosciences, 14, 3067–3082, https://doi.org/10.5194/bg-14-3067-2017, 2017.
Kotilainen, A. T., Arppe, L., Dobosz, S., Jansen, E., Kabel, K., Karhu, J., Kotilainen, M. M.,
Kuijpers, A., Lougheed, B. C., Meier, H. E. M., Moros, M., Neumann, T., Porsche, C.,
Poulsen, N. Rasmussen, P., Ribeiro, S., Risebrobakken, B., Ryabchuk, D.,
Schimanke, S., Snowball, I., Spiridonov, M., Virtasalo, J. J., Weckström, K., Witkowski, A., and Zhamoida, V.: Echoes from the past: A healthy Baltic Sea
requires more effort, Ambio, 43, 60–68, 2014.
Kotthoff, U., Groeneveld, J., Ash, J. L., Fanget, A.-S., Krupinski, N. Q., Peyron, O., Stepanova, A.,
Warnock, J., Van Helmond, N. A. G. M., Passey, B. H., Clausen, O. R., Bennike, O.,
Andrén, E., Granoszewski, W., Andrén, T., Filipsson, H. L., Seidenkrantz, M.-S.,
Slomp, C. P., and Bauersachs, T.: Reconstructing Holocene temperature and salinity
variations in the western Baltic Sea region: a multi-proxy comparison from the
Little Belt (IODP Expedition 347, Site M0059), Biogeosciences, 14, 5607–5632, https://doi.org/10.5194/bg-14-5607-2017, 2017.
Kremling, K. and Wilhelm, G.: Recent increase of the calcium concentrations
in the Baltic Sea
waters, Mar. Poll. Bull., 34, 763–767, 1997.
Kristensen, P. H. and Knudsen, K. L.: Palaeoenvironments of a complete
Eemian sequences at
Mommark, South Denmark: foraminifera, ostracods and stable isotopes, Boreas,
35, 349–366,
2006.
Kristjánsdóttir, G. B., Lea, D. W., Jennings, A. E., Pak, D. K., and
Belanger, C.: New spatial Mg∕Ca-temperature calibrations for three Arctic, benthic foraminifera and
reconstruciton of north
Iceland shelf temperature for the past 4000 years, Geochem. Geophys.
Geosys., 8, Q03P21,
https://doi.org/10.1029/2006GC001425, 2007.
Lea, D. and Boyle, E.: Barium content of benthic foraminifera controlled by
bottom-water
composition, Nature, 338, 751–753, 1989.
Lea, D. W. and Boyle, E. A.: Barium in planktonic foraminifera, Geochim.
Cosmochim. Ac., 55, 3321–3331, 1991.
Lea, D. W. and Spero, H. J.: Assessing the reliability of paleochemical
tracers: Barium uptake in the
shells of planktonic foraminifera, Paleoceanography, 9, 445–452,
1994.
Lea, D. W., Mashiotta, T. A., and Spero, H. J.: Controls on magnesium and
strontium uptake in
planktonic foraminifera determined by live culturing, Geochim. Cosmochim.
Ac., 63, 2369–2379, 1999.
Lear, C. H., Rosenthal, Y., and Slowey, N.: Benthic foraminiferal
Mg∕Ca-paleothermometry: A revised
core-top calibration, Geochim. Cosmochim. Ac., 66, 3375–3387, 2002.
Lenz, C., Jilbert, T., Conley, D. J., and Slomp, C. P.: Hypoxia-driven
variations in iron and manganese
shuttling in the Baltic Sea over the past 8 kyrs, Geochem. Geophys.
Geosys., 16,
3754–3766, https://doi.org/10.1002/2015GC005960, 2015.
Loeblich, A. R. and Tappan, H.: Part C, Protista 2, Sarcodina, Chiefly
`Thecamoebians' and
Foraminiferida, in: Treatise on Invertebrate Paleontology, edited by: Moore, R. C., The
Geological Society of America and the University of Kansas, 900 pp.,
1964.
Löfvendahl, R., Åberg, G., and Hamilton, P. J.: Strontium in rivers
of the Baltic Basin, Aquat. Sci.,
52, 315–329, 1990.
Lutze, G. F.: Zur Foraminiferen-Fauna der Ostsee, Meyniana, 15, 75–142,
1965.
Madden, T.: The BLAST Sequence Analysis Tool, in: The NCBI Handbook, edited by: McEntyre, J. and Ostell,
J., Bethesda (MD): National Center for Biotechnology Information
(US), Chapter
16, available at: http://www.ncbi.nlm.nih.gov/books/NBK21097/ (last access: June 2016),
2002.
Matthäus, W. and Schinke, H.: The influence of river runoff on deep
water conditions of the Baltic
Sea, Hydrobiologia, 393, 1–10, 1999.
McCorkle, D. C., Corliss, B. H., and Farnham, C. A.: Vertical distributions
and stable isotopic
compositions of live (stained) benthic foraminifera from the North Carolina
and California
continental margins, Deep-Sea Res. Pt. I, 44, 983–1024, 1997.
McKay, C. L., Groeneveld, J., Filipsson, H. L., Gallego-Torres, D., Whitehouse, M. J.,
Toyofuku, T., and Romero, O. E.: A comparison of benthic foraminiferal Mn∕Ca
and sedimentary Mn∕Al as proxies of relative bottom-water
oxygenation in the low-latitude NE Atlantic upwelling system, Biogeosciences, 12, 5415–5428, https://doi.org/10.5194/bg-12-5415-2015, 2015.
McKenna, C., Berx, B., and Austin, W. E. N.: The decomposition of the
Faroe-Shetland Channel water
masses using Parametric Optimum Multi-Parameter analysis, Deep-Sea Res. Pt. I,
107, 9–21,
2016.
Mehrbach, C., Culberso, C. H., Hawley, J. E., and Pytkowic, R. M.:
Measurement of apparent
dissociation constants of carbonic acid in seawater at atmospheric pressure,
Limnol.
Oceanogr., 18, 897–907, 1973.
Meier, H. E. M., Andersson, H. C., Eilola, K., Gustafsson, B. G., Kuznetsov,
I., Müller-Karulis, B.,
Neumann, T., and Savchuk, O. P.: Hypoxia in future climates: A model
ensemble study for the
Baltic Sea, Geophys. Res. Lett., 38, L24608, https://doi.org/10.1029/2011GL049929,
2011.
Mertens, K. N., Bringue, M., van Nieuwenhove, N., Takano, Y., Pospelova, V., Rochon, A.,
de Vernal, A., Radi, T., Dale, B., Patterson, R. T., Weckström, K., Andren, E., Louwye, S., and Matsuoka, K.: Process length variation of the cyst of the
dinoflagellate Protoceratium
reticulatum in the North Pacific and Baltic-Skagerrak region: calibration as an annual
density
proxy and first evidence of pseudo-cryptic speciation, J. Quaternary Sci., 27,
734–744, 2012.
Mohrholz, V., Naumann, M., Nausch, G., Krüger, S., and Gräwe, U.:
Fresh oxygen for the Baltic Sea –
An exceptional saline inflow after a decade of stagnation, J. Mar. Sys.,
148, 152–166, 2015.
Murray, J. W. (Ed.): Ecology and applications of benthic foraminifera,
Cambridge University Press, Cambridge, 426 pp., 2006.
Murray, J. W.: Biodiversity of living benthic foraminifera: How many species
are there?, Mar. Micropaleontol., 64, 163–176, https://doi.org/10.1016/j.marmicro.2007.04.002, 2007.
Murray, J. W. and Alve, E.: The distribution of agglutinated Foraminifera
in NW European seas:
baseline data for the interpretation of fossil assemblages, Palaeontol.
Electron., 14, 14A, 1–41,
2011.
Nardelli, M. P., Barras, C., Metzger, E., Mouret, A., Filipsson, H. L., Jorissen, F.,
and Geslin, E.: Experimental evidence for foraminiferal calcification
under anoxia, Biogeosciences, 11, 4029–4038, https://doi.org/10.5194/bg-11-4029-2014, 2014.
Nehring, D.: Hydrographic and chemical conditions in the Western and Central
Baltic Sea from 1979
to 1988 – a comparison, Mar. Sci. Rep., 2, 2–45, 1990.
Ní Fhlaithearta, S., Reichart, G.-J., Jorissen, F. J., Fontanier, C.,
Rohling, E. J., Thomson, J., and De
Lange, G. J.: Reconstructing the seafloor environment during sapropel
formation using
benthic foraminiferal trace metals, stable isotopes, and sediment
composition,
Paleoceanography, 25, PA4225, https://doi.org/10.1029/2009PA001869, 2010.
Ning, W., Ghosh, A., Jilbert, T., Slomp, C. P., Khan, M., Nyberg, J.,
Conley, D. J., and Filipsson, H. L.:
Evolving coastal character of a Baltic Sea inlet during the Holocene
shoreline regression:
impact on coastal zone hypoxia, J. Paleolimno., 55, 319–338,
https://doi.org/10.1007/s10933-016-9882-6,
2016.
Ning, W., Andersson, P. S., Ghosh, A., Khan, M., and Filipsson, H. L.:
Quantitative salinity
reconstructions of the Baltic Sea during the mid-Holocene, Boreas, 46,
100–110, https://doi.org/10.1111/bor.12156, 2017.
Nordberg, K. and Bergsten, H.: Biostratigraphic and sedimentological
evidence of hydrographic
changes in the Kattegat during the later part of the Holocene, Mar. Geol.,
83, 135–158, 1988.
Nürnberg, D.: Taking the temperature of past ocean surfaces, Science,
289, 1698–1699, https://doi.org/10.1126/science.289.5485.1698, 2000.
Ohlson, M. and Anderson, L.: Recent investigation of total carbonate in the
Baltic Sea: changes from
the past as a result of acid rain?, Mar. Chem., 30, 259–267, 1991.
Osterman, L. E., Poore, R. Z., Swarzenski, P. W., and Turner, R. E.:
Reconstructing a 180 yr
record of natural and anthropogenic induced low-oxygen conditions from
Louisiana
continental shelf sediments, Geology, 33, 329–332, https://doi.org/10.1130/G21341.1,
2005.
Pawlowski, J.: Introduction to the molecular systematics of foraminifera,
Micropaleontology, 46, 1–12, 2000.
Pawlowski, J. and Holzmann, M.: Diversity and geographic distribution of
benthic foraminifera: a
molecular perspective, Biodivers. Conserv., 17, 317–328,
2008.
Pawlowski, J. and Holzmann, M.: A plea for DNA barcoding of foraminifera,
J. Foram. Res., 44, 62–67,
2014.
Pedersen, T. F. and Price, N. B.: The geochemistry of manganese carbonate
in Panama Basin
sediments, Geochim. Cosmochim. Ac., 46, 59–68, 1982.
Petersen, J., Riedel, B., Barras, C., Pays, O., Guihéneuf, A.,
Mabilleau, G., Schweizer, M., Meysman, F.
J. R., and Jorissen, F. J.: Improved methodology for measuring pore
patterns in the benthic
foraminiferal genus Ammonia, Mar. Micropaleontol., 128, 1–13, 2016.
Petersen, J., Barras, C., Bézos, A., La, C., de Nooijer, L. J., Meysman, F. J. R.,
Mouret, A., Slomp, C. P., and Jorissen, F. J.: Mn∕Ca intra- and inter-test variability
in the benthic foraminifer Ammonia tepida, Biogeosciences, 15, 331–348, https://doi.org/10.5194/bg-15-331-2018, 2018.
Pierrot, D., Lewis, E., Wallace, D. W. R. (Eds.): MS Excel program developed for CO2 system
calculations, ORNL/CDIAC-105, Carbon Dioxide Inf. Anal. Cent., Oak Ridge Natl. Lab, US
Dep. of Energy, Oak Ridge, Tenn., 2006.
Pillet, L., Voltski, I., Korsun, S., and Pawlowski, J.: Molecular phylogeny
of Elphidiidae
(foraminifera), Mar. Micropaleontol., 103, 1–14, 2013.
Platon, E., Sen Gupta, B. K., Rabalais, N. N., and Turner, R. E.: Effect of
seasonal hypoxia on the
benthic foraminiferal community of the Louisiana inner continental shelf:
The 20th century
record, Mar. Micropaleontol., 54, 263–283, 2005.
Polovodova, I. and Schönfeld, J.: Foraminiferal test abnormalities in
the western Baltic Sea, J. Foram.
Res., 38, 318–336, 2008.
Polyak, L., Stanovoy, V., and Lubinski, D. J.: Stable isotopes in benthic
foraminiferal calcite from
a river-influenced Arctic marine environment, Kara and Pechora Seas,
Paleoceanography, 18,
1003, https://doi.org/10.1029/2001PA000752, 2003.
Punning, J.-M., Martma, T., Kessel, H., and Vaikmäe, R.: The isotopic
composition of oxygen and
carbon in the subfossil mollusc shells of the Baltic Sea as an indicator of
palaeosalinity,
Boreas, 17, 27–31, 1988.
Raitzsch, M., Kuhnert, H., Groeneveld, J., and Bickert, T.: Benthic
foraminifer Mg∕Ca anomalies in
South Atlantic core top sediments and their implications for
paleothermometry,
Geochem. Geophys. Geosys., 9, Q05010, https://doi.org/10.1029/2007GC001788,
2008.
Raitzsch, M., Dueñas-Bohórquez, A., Reichart, G.-J., de Nooijer, L. J., and
Bickert, T.: Incorporation of Mg and Sr in calcite of cultured benthic foraminifera:
impact of calcium concentration and associated calcite saturation
state, Biogeosciences, 7, 869–881, https://doi.org/10.5194/bg-7-869-2010, 2010.
Raitzsch, M., Hathorne, E. C., Kuhnert, H., Groeneveld, J., and Bickert, T.:
Modern and late
Pleistocene B∕Ca ratios of the benthic foraminifer Planulina wuellerstorfi determined with
laser ablation ICP-MS, Geology, 39, 1039–1042, https://doi.org/10.1130/G32009.1,
2011.
Regenberg, M., Nürnberg, D., Steph, S., Groeneveld, J., Garbe-Schönberg, D., Tiedemann, R., and Dullo, W.: Assessing the effect of dissolution
on planktonic foraminiferal Mg/Ca ratios: Evidence from Caribbean
core tops, Geochem. Geophys. Geosyst., 7, Q07P15, https://doi.org/10.1029/2005GC001019, 2006.
Roberts, A., Austin, W. E. N., Evans, K., Bird, C., Schweizer, M., and
Darling, K.: A new integrated
approach to taxonomy: the fusion of molecular and morphological systematics
with type
material in benthic foraminifera, PLoS One, 11, e0158754,
https://doi.org/10.1371/journal.pone.0158754, 2016.
Sadekov, A. Y., Eggins, S. M., and De Deckker, P.: Characterization of Mg∕Ca
distributions in
planktonic foraminifera species by electron microprobe mapping, Geochem.
Geophys. Geosys., 6, Q12P06, https://doi.org/10.1029/2005GC000973, 2005.
Salminen, R. (Ed.): Geochemical Atlas of Europe. Part 1: Background
information, methodology
and maps, Geological Survey of Finland, Espoo, 526 pp., 2005.
Schmiedl, G., Pfeilsticker, M., Hemleben, Ch., and Mackensen, A.:
Environmental and biological effects on the stable isotope composition of
recent deep-sea benthic foraminifera from the western Mediterranean Sea,
Mar. Micropaleontol., 51, 129–152, 2004.
Scholz, F., Hensen, C., Noffke, A., Rohde, A., Liebetrau, V., and Wallmann,
K.: Early diagenesis of
redox-sensitive trace metals in the Peru upwelling area – response to
ENSO-related oxygen
fluctuations in the water column, Geochim. Cosmochim. Ac., 75, 7257–7276,
2011.
Schönfeld, J. and Numberger, L.: The benthic foraminiferal response to
the 2004 spring bloom in the
western Baltic Sea, Mar. Micropaleontol., 65, 78–95, 2007.
Schweizer, M.: How long after death is DNA preserved in situ in intertidal
foraminifera?, J. Micropal., 34, 217–219, 2015.
Schweizer, M., Pawlowski, J., Duijnstee, I. A. P., Kouwenhoven, T. J., and
van der Zwaan, G. J.: Molecular phylogeny of the foraminiferal genus
Uvigerina based on ribosomal DNA sequences, Mar. Micropaleontol., 57, 51–67, 2005.
Schweizer, M., Pawlowski, J., Kouwenhoven, T. J., Guiard, J., and van der
Zwaan, B.: Molecular phylogeny of Rotaliida (Foraminifera) based on complete
small subunit rDNA sequences, Mar. Micropaleontol., 66, 233–246, 2008.
Schweizer, M., Pawlowski, J., Kouwenhoven, T., and van der Zwaan, B.:
Molecular phylogeny of common cibicidids and related Rotaliida
(Foraminifera) based on small subunit rDNA sequences, J. Foram. Res., 39,
300–315, 2009.
Schweizer, M., Jorissen, F., and Geslin, E.: Contributions of molecular
phylogenetics to foraminiferal taxonomy: General overview and an example
with Pseudoeponides falsobeccarii Rouvillois, 1974, C. R. Palevol., 10, 95–105, 2011a.
Schweizer, M., Polovodova, I., Nikulina, A., and Schönfeld, J.:
Molecular identification of Ammonia and Elphidium species (Foraminifera, Rotaliida) from the
Kiel Fjord (SW Baltic Sea) with rDNA sequences, Helgoland Mar. Res., 65,
1–10, 2011b.
Segev, E. and Erez, J.: Effect of Mg∕Ca ratio in seawater on shell
composition in shallow benthic foraminifera, Geochem. Geophys. Geosys., 7,
Q02P09, https://doi.org/10.1029/2005GC000969,
2006.
Skirbekk, K., Hald, M., Marchitto, T. M., Junttila, J., Kristensen, D. K.,
and Sörensen, S. A.:
Benthic foraminiferal growth seasons implied from Mg∕Ca-temperature
correlations for
three Arctic species, Geochem. Geophys. Geosys., 17, 4684–4704,
https://doi.org/10.1002/2016GC006505, 2016.
Tappan, H. and Loeblich, A. R.: Foraminiferal Evolution, Diversification,
and Extinction, J.
Paleontology, 62, 695–714, 1988.
Toyofuku, T., Suzuki, M., Suga, H., Sakai, S., Suzuki, A., Ishikawa, T., De
Nooijer, L. J., Schiebel, R.,
Kawahata, H., and Kitazato, H.: Mg∕Ca and δ18O in the brackish
shallow-water benthic
foraminifer Ammonia beccarii, Mar. Micropaleontol., 78, 113–120, 2011.
Tribovillard, N., Algeo, T. J., Lyons, T., and Riboulleau, A.: Trace metals
as paleoredox and
paleoproductivity proxies: An update, Chem. Geol., 232, 12–32,
2006.
Turner, D. R., Dickson, A. G., and Whitfield, M.: Water-rock partition
coefficients and the composition of
natural waters – a reassessment, Mar. Chem., 9, 211–218, 1980.
Van Helmond, N. A. G. M., Krupinski, N. Q., Lougheed, B. C., Obrochta, S.
P., Andrén, T., and Slomp, C.
P.: Seasonal hypoxia was a natural feature of the coastal zone in the Little
Belt, Denmark,
during the past 8 ka, Mar. Geol., 387, 45–57, https://doi.org/10.1016/j.margeo.2017.03.008,
2017.
Weber, A. A.-T. and Pawlowski, J.: Wide occurrence of SSU rDNA
intragenomic polymorphism in
foraminifera and its implications for molecular species identification,
Protist, 165, 645–661,
2014.
Weldeab, S., Lea, D. W., Schneider, R. R., and Andersen, N.: 155,000 years
of West African
monsoon and ocean thermal evolution, Science, 316, 1303–1307, 2007.
White, T. J., Bruns, T., Lee, S. J. W. T., and Taylor, J. W.: Amplification and
direct sequencing of fungal
ribosomal RNA genes for phylogenetics, PCR protocols: a Guide to Methods and
Applications, 18, 315–322, 1990.
Widerlund, A. and Andersson, P. S.: Late Holocene freshening of the Baltic
Sea derived from high-resolution strontium isotope analyses of mollusk shells, Geology, 39,
187–190, 2011.
Wit, J. C., de Nooijer, L. J., Barras, C., Jorissen, F. J., and Reichart, G. J.:
A reappraisal of the vital effect in cultured benthic foraminifer Bulimina marginata on Mg∕Ca values: assessing temperature uncertainty
relationships, Biogeosciences, 9, 3693–3704, https://doi.org/10.5194/bg-9-3693-2012, 2012.
Zillén, L., Conley, D. J., Andrén, T., Andrén, E., and
Björck, S.: Past occurrences of hypoxia in the Baltic
Sea and the role of climate variability, environmental change and human
impact, Earth-Sci.
Rev., 91, 77–92, 2008.
Short summary
Current climate and environmental changes strongly affect shallow marine and coastal areas like the Baltic Sea. The combination of foraminiferal geochemistry and environmental parameters demonstrates that in a highly variable setting like the Baltic Sea, it is possible to separate different environmental impacts on the foraminiferal assemblages and therefore use chemical factors to reconstruct how seawater temperature, salinity, and oxygen varied in the past and may vary in the future.
Current climate and environmental changes strongly affect shallow marine and coastal areas like...