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2. The impact of cascading currents on the Bari Canyon System, SW-Adriatic Margin (Central Mediterranean) F. Trincardi et al. 10.1016/j.margeo.2007.01.013
3. Impact of climate and sea level changes on the ventilation of intermediate water and benthic foraminifer assemblages in the Gulf of Lions, off South France, during MIS 6 and 7 A. Cortina et al. 10.1016/j.palaeo.2011.06.005
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5. Paleoenvironmental changes across the Cenomanian/Turonian Boundary Event (Oceanic Anoxic Event 2) as indicated by benthic foraminifera from the Demerara Rise (ODP Leg 207) O. Friedrich et al. 10.1016/j.revmic.2006.04.003
6. A Window Into Eastern Mediterranean Productivity Conditions Over Three Pliocene Precession‐Forced Climate Cycles A. Cutmore et al. 10.1029/2022PA004550
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8. Foraminiferal response to the deposition of insolation cycle 90 sapropel in different Mediterranean areas S. Stefanelli & L. Capotondi 10.1144/jm.27.1.45
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21. Late Glacial to Recent distribution pattern of deep-water Uvigerina species in the north-eastern Atlantic J. Schönfeld & A. Altenbach 10.1016/j.marmicro.2005.05.004
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23. Climatic cycles as expressed in sediments of the PROMESS1 borehole PRAD1‐2, central Adriatic, for the last 370 ka: 2. Paleoenvironmental evolution A. Piva et al. 10.1029/2007GC001785
24. Paleoclimate and paleoceanography over the past 20,000 yr in the Mediterranean Sea Basins as indicated by sediment elemental proxies F. Martinez-Ruiz et al. 10.1016/j.quascirev.2014.09.018
25. Holocene Climatic Optimum centennial-scale paleoceanography in the NE Aegean (Mediterranean Sea) M. Triantaphyllou et al. 10.1007/s00367-015-0426-2
26. Marine and terrestrial climate variability in the western Mediterranean Sea during marine isotope stages 20 and 19 F. Toti et al. 10.1016/j.quascirev.2020.106486
27. Paleoproductivity Modes in Central Mediterranean During MIS 20—MIS 18: Calcareous Plankton and Alkenone Variability P. Maiorano et al. 10.1029/2021PA004259
28. Trace-elemental derived paleoceanographic and paleoclimatic conditions for Pleistocene Eastern Mediterranean sapropels D. Gallego-Torres et al. 10.1016/j.palaeo.2010.05.001
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31. Different nutrient sources forcing increased productivity during eastern Mediterranean S1 sapropel formation as reflected by calcareous dinoflagellate cysts K. Meier et al. 10.1029/2003PA000895
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33. Ephemeral signature of anoxia in the southwest Mediterranean coastal lagoon (southeast Tunisia) similar to the sapropel S1 R. Lakhdar & R. Talbi 10.1007/s41207-024-00505-3
34. On the late Pleistocene‐Holocene sapropel record of climatic and oceanographic variability in the eastern Mediterranean S. Calvert & M. Fontugne 10.1029/1999PA000488
35. A review of palaeoclimates and palaeoenvironments in the Levant and Eastern Mediterranean from 25,000 to 5000 years BP: setting the environmental background for the evolution of human civilisation S. Robinson et al. 10.1016/j.quascirev.2006.02.006
36. Uniform climate development between the subtropical and subpolar Northeast Atlantic across marine isotope stage 11 J. Helmke et al. 10.5194/cp-4-181-2008
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38. Late Quaternary paleoclimatic and paleoenviromental changes in the Tyrrhenian Sea M. Gabriella Carboni et al. 10.1016/j.quascirev.2004.09.009
39. The transition from natural to anthropogenic-dominated environmental change in Italy and the surrounding regions since the Neolithic: An introduction G. Zanchetta et al. 10.1016/j.quaint.2013.05.009
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45. Benthic environmental changes in the Eastern Mediterranean Sea during sapropel S5 deposition C. Morigi 10.1016/j.palaeo.2008.10.010
46. Palaeoceanography and numerical modelling: the Mediterranean Sea at times of sapropel formation E. Rohling et al. 10.1144/GSL.SP.2000.181.01.13
47. Variation of deepwater convection in the western Mediterranean Sea (Gulf of Lion) during the last 28 ka T. Melki 10.1016/j.quaint.2011.04.001
48. Geochemistry of an exotic sediment layer above sapropel S-1: mud expulsion from the Urania Basin, eastern Mediterranean? A. Hübner et al. 10.1016/S0025-3227(03)00085-9
49. Climate variability during MIS 20–18 as recorded by alkenone-SST and calcareous plankton in the Ionian Basin (central Mediterranean) M. Marino et al. 10.1016/j.palaeo.2020.110027
50. Holocene Climate Optimum and Last Glacial Maximum in the Mediterranean: the marine oxygen isotope record E. Rohling & S. De Rijk 10.1016/S0025-3227(98)00020-6
51. Environmental control on Mediterranean salinity and δ18O E. Rohling 10.1029/1999PA900042
52. The role of the oceanic oxygen minima in generating biodiversity in the deep sea A. Rogers 10.1016/S0967-0645(99)00107-1
53. Sediment microfabric records mass sedimentation of colonial cyanobacteria and extensive syndepositional metazoan reworking in Pliocene sapropels S. Löhr et al. 10.1002/dep2.49
54. Late Pleistocene to Holocene tephrostratigraphic record from the Northern Ionian Sea B. Caron et al. 10.1016/j.margeo.2012.04.001
55. Foraminiferal records of bottom-water oxygenation and surface-water productivity in the southern Japan Sea during 160–15ka: Associations with insolation changes K. Usami et al. 10.1016/j.marmicro.2013.03.006
56. Palynofacies Analysis of Inner Continental Shelf and Middle Slope Sediments offshore Egypt, South-eastern Mediterranean S. Kholeif & M. Ibrahim 10.1016/j.geobios.2009.10.006
57. Colonization of new habitats by benthic foraminifera: a review E. Alve 10.1016/S0012-8252(99)00016-1
58. Sub-millennial scale climatic oscillations in the central Adriatic during the Lateglacial: palaeoceanographic implications A. Asioli et al. 10.1016/S0277-3791(00)00147-5
59. Ecological Constraints of Plankton Bio-Indicators for Water Column Stratification and Productivity: A Case Study of the Holocene North Aegean Sedimentary Record C. Giamali et al. 10.3390/jmse9111249
60. Oxygen and evolutionary patterns in the sea: Onshore/offshore trends and recent recruitment of deep-sea faunas D. Jacobs & D. Lindberg 10.1073/pnas.95.16.9396
61. Polychaetes distributed across oceans—examples of widely recorded species from abyssal depths of the Atlantic and Pacific Oceans K. Meißner et al. 10.1093/zoolinnean/zlad069
62. Variability of the western Mediterranean Sea surface temperature during the last 25,000 years and its connection with the Northern Hemisphere climatic changes I. Cacho et al. 10.1029/2000PA000502
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65. Does fossil pigment and DNA data from Mediterranean sediments invalidate the use of green sulfur bacterial pigments and their diagenetic derivatives as proxies for the assessment of past photic zone euxinia? J. Sinninghe Damsté & E. Hopmans 10.1111/j.1462-2920.2008.01609.x
66. Large-scale response of the Eastern Mediterranean thermohaline circulation to African monsoon intensification during sapropel S1 formation T. Tesi et al. 10.1016/j.quascirev.2017.01.020
67. Climate-induced surface water variability at Monte San Nicola type-section (Sicily, southern Italy): New data across the Gelasian GSSP M. Addante et al. 10.1016/j.palaeo.2023.111907
68. Multiproxy ecosystem response of abrupt Holocene climatic changes in the northeastern Mediterranean sedimentary archive and hydrologic regime C. Giamali et al. 10.1017/qua.2019.38
69. Foraminiferal record and environmental changes during the deposition of the Early–Middle Pleistocene sapropels in southern Italy S. Stefanelli et al. 10.1016/j.palaeo.2004.10.001
70. Patterns of organic carbon and nitrogen isotopic compositions of latest Pliocene sapropels from six locations across the Mediterranean Sea M. Arnaboldi & P. Meyers 10.1016/j.palaeo.2005.09.027
71. Marine nitrogen cycling dynamics under altering redox conditions: Insights from deposition of sapropels S1 and the ambiguous S2 in the Eastern Mediterranean Sea Z. van Kemenade et al. 10.1016/j.gca.2023.06.018
72. Circulation changes and nutrient concentrations in the late Quaternary Aegean Sea: A nonsteady state concept for sapropel formation J. Casford et al. 10.1029/2000PA000601
73. Simulations of ecosystem response during the sapropel S1 deposition event D. Bianchi et al. 10.1016/j.palaeo.2005.09.032
74. Reconstructing the seafloor environment during sapropel formation using benthic foraminiferal trace metals, stable isotopes, and sediment composition S. Ní Fhlaithearta et al. 10.1029/2009PA001869
75. A stratigraphically controlled multiproxy chronostratigraphy for the eastern Mediterranean J. Casford et al. 10.1029/2007PA001422
76. Lack of denitrification causes a difference in benthic foraminifera living in the oxygen deficient zones of the Bay of Bengal and the Arabian Sea T. Suokhrie et al. 10.1016/j.marpolbul.2020.110992
77. Duration of S1, the most recent sapropel in the eastern Mediterranean Sea, as indicated by accelerator mass spectrometry radiocarbon and geochemical evidence D. Mercone et al. 10.1029/1999PA000397
78. Changes in the Intermediate Water Masses of the Mediterranean Sea During the Last Climatic Cycle—New Constraints From Neodymium Isotopes in Foraminifera C. Colin et al. 10.1029/2020PA004153
79. The role of foraminifera as indicators of the Late Pleistocene–Holocene palaeoclimatic fluctuations on the deltaic environment: The example of Tiber delta succession (Tyrrhenian margin, Italy) L. Di Bella et al. 10.1016/j.quaint.2013.04.015
80. Review of recent advances in the interpretation of eastern Mediterranean sapropel S1 from geochemical evidence J. Thomson et al. 10.1016/S0025-3227(98)00089-9
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