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Hydrological changes in the Mediterranean Sea over the last 30,000 years
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What this work says
Outgoing claims: the papers this work cites, builds on, or argues with.
inferredcites →https://doi.org/10.1016/0016-7037(88)90132-9openalex-snapshot
Further evaluation of long-chain alkenones as indicators of paleoceanographic conditions
inferredcites →https://doi.org/10.1016/0031-0182(96)85043-7openalex-snapshot
Late quaternary chronology and paleoclimates of the eastern Mediterranean
inferredcites →https://doi.org/10.1016/0034-6667(80)90023-8openalex-snapshot
Multidimensional scaling as a research tool in quaternary palynology: A review of theory and methods
inferredcites →https://doi.org/10.1016/0168-9622(88)90042-5openalex-snapshot
Normalization of oxygen and hydrogen isotope data
inferredcites →https://doi.org/10.1016/j.quascirev.2003.06.020openalex-snapshot
Constraints on hydrological and paleotemperature variations in the Eastern Mediterranean region in the last 140ka given by the δD values of speleothem fluid inclusions
inferredcites →https://doi.org/10.1016/j.quascirev.2004.02.018openalex-snapshot
Glacial Mediterranean sea surface temperatures based on planktonic foraminiferal assemblages
inferredcites →https://doi.org/10.1016/j.quascirev.2006.02.006openalex-snapshot
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
inferredcites →https://doi.org/10.1016/s0016-7037(02)01031-1openalex-snapshot
Sea–land oxygen isotopic relationships from planktonic foraminifera and speleothems in the Eastern Mediterranean region and their implication for paleorainfall during interglacial intervals
inferredcites →https://doi.org/10.1016/s0031-0182(00)00049-3openalex-snapshot
Present-day coccolith fluxes recorded in central eastern Mediterranean sediment traps and surface sediments
inferredcites →https://doi.org/10.1016/s0031-0182(00)00053-5openalex-snapshot
Temperature and salinity variations of Mediterranean Sea surface waters over the last 16,000 years from records of planktonic stable oxygen isotopes and alkenone unsaturation ratios
inferredcites →https://doi.org/10.1016/s0031-0182(97)00021-7openalex-snapshot
Temperature and salinity records of the Tyrrhenian Sea during the last 18,000 years
inferredcites →https://doi.org/10.1016/s0277-3791(01)00101-9openalex-snapshot
Sea-level and deep water temperature changes derived from benthic foraminifera isotopic records
inferredcites →https://doi.org/10.1016/s0277-3791(01)00107-xopenalex-snapshot
Constraints on the ocean oxygen isotopic enrichment between the Last Glacial Maximum and the Holocene: Paleoceanographic implications
inferredcites →https://doi.org/10.1016/s0967-0637(97)89915-3openalex-snapshot
Evaluation of long-chain alkenones as paleo-temperature indicators in the Mediterranean Sea
inferredcites →https://doi.org/10.1016/s0967-0653(98)80361-xopenalex-snapshot
10.1016/s0967-0653(98)80361-x
inferredcites →https://doi.org/10.1029/1999gl900353openalex-snapshot
Alkenones in the northwestern Mediterranean Sea: Interannual variability and vertical transfer
inferredcites →https://doi.org/10.1029/1999pa000411openalex-snapshot
Calibration of stable isotopic data: An enriched δ18O standard used for source gas mixing detection and correction
inferredcites →https://doi.org/10.1029/1999pa000488openalex-snapshot
On the late Pleistocene‐Holocene sapropel record of climatic and oceanographic variability in the eastern Mediterranean
inferredcites →https://doi.org/10.1029/1999pa900044openalex-snapshot
Dansgaard‐Oeschger and Heinrich event imprints in Alboran Sea paleotemperatures
inferredcites →https://doi.org/10.1029/2000pa000502openalex-snapshot
Variability of the western Mediterranean Sea surface temperature during the last 25,000 years and its connection with the Northern Hemisphere climatic changes
inferredcites →https://doi.org/10.1029/2000pa000617openalex-snapshot
Eastern Mediterranean surface water temperatures and δ18O composition during deposition of sapropels in the late Quaternary
inferredcites →https://doi.org/10.1029/2005gc001054openalex-snapshot
Global temperature calibration of the alkenone unsaturation index (UK′37) in surface waters and comparison with surface sediments
inferredcites →https://doi.org/10.1029/92jd01920openalex-snapshot
Paleoclimatic tracers: An investigation using an atmospheric general circulation model under ice age conditions: 2. Water isotopes
inferredcites →https://doi.org/10.1029/92jd01921openalex-snapshot
Paleoclimatic tracers: An investigation using an atmospheric general circulation model under ice age conditions: 1. Desert dust
inferredcites →https://doi.org/10.1029/94pa01183openalex-snapshot
An ocean general circulation model view of the glacial Mediterranean thermohaline circulation
inferredcites →https://doi.org/10.1029/98pa02736openalex-snapshot
Modeling the paleocirculation of the Mediterranean: The Last Glacial Maximum and the Holocene with emphasis on the formation of sapropel S1
inferredcites →https://doi.org/10.1038/320350a0openalex-snapshot
Direct dating of the oxygen-isotope record of the last deglaciation by 14C accelerator mass spectrometry
inferredcites →https://doi.org/10.1038/358485a0openalex-snapshot
Changes in surface salinity of the North Atlantic Ocean during the last deglaciation
inferredcites →https://doi.org/10.1126/science.1059549openalex-snapshot
Sea Level Change Through the Last Glacial Cycle
inferredcites →https://doi.org/10.1126/science.1063649openalex-snapshot
Mediterranean Sea Surface Radiocarbon Reservoir Age Changes Since the Last Glacial Maximum
inferredcites →https://doi.org/10.1126/science.289.5483.1321openalex-snapshot
Hydrological Impact of Heinrich Events in the Subtropical Northeast Atlantic
inferredcites →https://doi.org/10.1126/science.290.5498.1905openalex-snapshot
Glacial Climate Instability
inferredcites →https://doi.org/10.1175/1520-0469(1986)043<1726:tiocop>2.0.co;2openalex-snapshot
The Influence of Changing Orbital Parameters and Surface Boundary Conditions on Climate Simulations for the Past 18 000 Years
What points at this work
Incoming claims: where this work appears in other papers’ reference lists and arguments.
inferred← citeshttps://doi.org/10.11646/zootaxa.4998.1.1zenodo-depositor-declared
Evidence-based checklist of the Mediterranean Sea fishes
inferred← citeshttps://doi.org/10.1002/2013pa002466openalex-snapshot
Sea surface temperature variations in the western Mediterranean Sea over the last 20 kyr: A dual‐organic proxy (U K′ 37 and LDI) approach
inferred← citeshttps://doi.org/10.1002/2013pa002553openalex-snapshot
Solar forcing of Nile discharge and sapropel S1 formation in the early to middle Holocene eastern Mediterranean
inferred← citeshttps://doi.org/10.1002/2015gl065397openalex-snapshot
The climate variability in northern Levant over the past 20,000 years
inferred← citeshttps://doi.org/10.1002/2017pa003227openalex-snapshot
Circulation Changes in the Eastern Mediterranean Sea Over the Past 23,000 Years Inferred From Authigenic Nd Isotopic Ratios
inferred← citeshttps://doi.org/10.1002/jqs.1360openalex-snapshot
Late glacial to Holocene planktic foraminifera bioevents and climatic record in the South Adriatic Sea
inferred← citeshttps://doi.org/10.1007/978-3-319-96794-3_14openalex-snapshot
Holocene Climate Development of North Africa and the Arabian Peninsula
inferred← citeshttps://doi.org/10.1007/s00367-025-00822-8openalex-snapshot
Sensitivity analysis of the physicochemical oceanographic drivers on the gas hydrate thickness variability associated with the last glacial Maximum - the European continental margins as a study case
inferred← citeshttps://doi.org/10.1007/s10113-014-0588-xopenalex-snapshot
21,000 Years of Ethiopian African monsoon variability recorded in sediments of the western Nile deep-sea fan
inferred← citeshttps://doi.org/10.1007/s10641-022-01252-6openalex-snapshot
Potential and limitations of applying the mean temperature approach to fossil otolith assemblages
inferred← citeshttps://doi.org/10.1007/s10933-023-00301-zopenalex-snapshot
Sedimentology and stratigraphy of the Jordan River Dureijat archeological site reveal subtle late Pleistocene water-level changes at Lake Hula, Jordan Valley, Israel
inferred← citeshttps://doi.org/10.1016/b978-0-08-095975-7.01210-9openalex-snapshot
History of Water in the Middle East and North Africa
inferred← citeshttps://doi.org/10.1016/b978-0-12-416042-2.00001-xopenalex-snapshot
Paleoclimate Variability in the Mediterranean Region
inferred← citeshttps://doi.org/10.1016/j.catena.2024.108236openalex-snapshot
Environmental and climatic significance of the Pliocene-Pleistocene calcretes in North Africa
inferred← citeshttps://doi.org/10.1016/j.crte.2012.01.002openalex-snapshot
The last glacial-interglacial transition and dinoflagellate cysts in the western Mediterranean Sea
inferred← citeshttps://doi.org/10.1016/j.crte.2012.02.001openalex-snapshot
Mg/Ca-paleothermometry in the western Mediterranean Sea on planktonic foraminifer species Globigerina bulloides: Constraints and implications
inferred← citeshttps://doi.org/10.1016/j.gca.2009.11.022openalex-snapshot
Geochemical evidence for a large methane release during the last deglaciation from Marmara Sea sediments
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2018.08.006openalex-snapshot
The Last Glacial Maximum and Heinrich event I on the Iberian Peninsula: A regional climate modelling study for understanding human settlement patterns
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.105086openalex-snapshot
Circulation changes in the Mediterranean Sea over the last 30,000 years – Constraints from deep-water Nd isotopes
inferred← citeshttps://doi.org/10.1016/j.jafrearsci.2015.11.010openalex-snapshot
Hydrogeochemical and stable isotope data of groundwater of a multi-aquifer system: Northern Gafsa basin – Central Tunisia
inferred← citeshttps://doi.org/10.1016/j.margeo.2010.12.011openalex-snapshot
Diagenetic Mg-rich calcite in Mediterranean sediments: Quantification and impact on foraminiferal Mg/Ca thermometry
inferred← citeshttps://doi.org/10.1016/j.marmicro.2021.101997openalex-snapshot
Mediterranean faunal evolution and biochronological events during the last 24 kyr
inferred← citeshttps://doi.org/10.1016/j.palaeo.2009.05.005openalex-snapshot
Abrupt climate change, sea surface salinity and paleoproductivity in the western Mediterranean Sea (Gulf of Lion) during the last 28 kyr
inferred← citeshttps://doi.org/10.1016/j.palaeo.2009.10.015openalex-snapshot
Environmental and climatic changes in the central Mediterranean Sea (Siculo–Tunisian Strait) during the last 30ka based on dinoflagellate cyst and planktonic foraminifera assemblages
inferred← citeshttps://doi.org/10.1016/j.palaeo.2010.02.039openalex-snapshot
The nature of transitions from dry to wet condition during sapropel events in the Eastern Mediterranean Sea
inferred← citeshttps://doi.org/10.1016/j.palaeo.2011.02.008openalex-snapshot
A 250ka sedimentary record from a small karstic lake in the Northern Levant (Yammoûneh, Lebanon)
inferred← citeshttps://doi.org/10.1016/j.palaeo.2014.11.011openalex-snapshot
Coccolithophore productivity and surface water dynamics in the Alboran Sea during the last 25 kyr
inferred← citeshttps://doi.org/10.1016/j.palaeo.2022.110924openalex-snapshot
High-frequency modification of the central Mediterranean seafloor environment over the last 74 ka
inferred← citeshttps://doi.org/10.1016/j.palaeo.2022.111291openalex-snapshot
Climate evolution in the Adriatic Sea across the last deglaciation: A multiproxy approach combining biomarkers and calcareous plankton
inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.112977openalex-snapshot
Holocene palaeoclimatic evolution in the North Ionian Basin of the Mediterranean Sea: A multiproxy approach
inferred← citeshttps://doi.org/10.1016/j.quaint.2012.07.516openalex-snapshot
A 250ka sedimentary record from a small karstic lake in the northern Levant (Yammoûneh, Lebanon) – Paleoclimatic implications
inferred← citeshttps://doi.org/10.1016/j.quaint.2020.01.024openalex-snapshot
Uranium isotopes as tracers of groundwater evolution in the Complexe Terminal aquifer of southern Tunisia
inferred← citeshttps://doi.org/10.1016/j.quascirev.2009.07.017openalex-snapshot
Climatic variability during the last ∼90ka of the southern and northern Levantine Basin as evident from marine records and speleothems
inferred← citeshttps://doi.org/10.1016/j.quascirev.2009.12.005openalex-snapshot
Controlling factors on a paleo-lake oxygen isotope record (Yammoûneh, Lebanon) since the Last Glacial Maximum
inferred← citeshttps://doi.org/10.1016/j.quascirev.2010.02.006openalex-snapshot
100,000 Years of African monsoon variability recorded in sediments of the Nile margin
inferred← citeshttps://doi.org/10.1016/j.quascirev.2015.10.030openalex-snapshot
20,000 years of Nile River dynamics and environmental changes in the Nile catchment area as inferred from Nile upper continental slope sediments
inferred← citeshttps://doi.org/10.1016/j.quascirev.2016.03.026openalex-snapshot
The timing of Mediterranean sapropel deposition relative to insolation, sea-level and African monsoon changes
inferred← citeshttps://doi.org/10.1016/j.quascirev.2017.03.015openalex-snapshot
North-African paleodrainage discharges to the central Mediterranean during the last 18,000 years: A multiproxy characterization
inferred← citeshttps://doi.org/10.1016/j.quascirev.2017.09.011openalex-snapshot
Human responses and non-responses to climatic variations during the last Glacial-Interglacial transition in the eastern Mediterranean
inferred← citeshttps://doi.org/10.1016/j.quascirev.2019.105872openalex-snapshot
Hydro-climate research of the late quaternary of the Eastern Mediterranean-Levant region based on speleothems research – A review
inferred← citeshttps://doi.org/10.1016/j.quascirev.2022.107502openalex-snapshot
LGM glaciers in the SE Mediterranean? First evidence from glacial landforms and 36Cl dating on Mount Lebanon
inferred← citeshttps://doi.org/10.1016/j.quascirev.2023.108053openalex-snapshot
Middle Eastern cloud distillation throughout the Holocene - Quantified using oxygen isotopes from speleothems and deep-sea cores
inferred← citeshttps://doi.org/10.1016/j.quascirev.2026.109921openalex-snapshot
Continuous speleothem record from central Tunisia (the Mine cave) reveals climatic events for the last 27 ka
inferred← citeshttps://doi.org/10.1016/j.revmic.2012.03.003openalex-snapshot
Evolution of the sebkha Dreîaa (South-Eastern Tunisia, Gulf of Gabes) during the Late Holocene: Response of ostracod assemblages
inferred← citeshttps://doi.org/10.1017/qua.2020.99openalex-snapshot
Thermal impact of Heinrich stadials in cave temperature and speleothem oxygen isotope records
inferred← citeshttps://doi.org/10.1029/2009pa001735openalex-snapshot
Hydrology in the Sea of Marmara during the last 23 ka: Implications for timing of Black Sea connections and sapropel deposition
inferred← citeshttps://doi.org/10.1029/2009pa001740openalex-snapshot
Millennial-scale sea surface temperature changes in the eastern Mediterranean (Nile River Delta region) over the last 27,000 years
inferred← citeshttps://doi.org/10.1029/2012pa002291openalex-snapshot
A precise search for drastic temperature shifts of the past 40,000 years in southeastern Europe
inferred← citeshttps://doi.org/10.1029/2018pa003452openalex-snapshot
Western Mediterranean Sea Paleothermometry Over the Last Glacial Cycle Based on the Novel RI‐OH Index
inferred← citeshttps://doi.org/10.1029/2019pa003827openalex-snapshot
Suborbital Hydrological Variability Inferred From Coupled Benthic and Planktic Foraminiferal‐Based Proxies in the Southeastern Mediterranean During the Last 19 ka
inferred← citeshttps://doi.org/10.1029/2020pa004153openalex-snapshot
Changes in the Intermediate Water Masses of the Mediterranean Sea During the Last Climatic Cycle—New Constraints From Neodymium Isotopes in Foraminifera
inferred← citeshttps://doi.org/10.1029/2021pa004289openalex-snapshot
A 1‐Million‐Year Record of Environmental Change in the Central Mediterranean Sea From Organic Molecular Proxies
inferred← citeshttps://doi.org/10.1029/2024pa004951openalex-snapshot
Influence of Mediterranean Oceanographic and Environmental Conditions on Molecular Proxy‐Based Sea Surface Temperature Reconstructions During the Last Interglacial
inferred← citeshttps://doi.org/10.1038/s41561-023-01328-7openalex-snapshot
Strong temperature gradients in the ice age North Atlantic Ocean revealed by plankton biogeography
inferred← citeshttps://doi.org/10.1038/s41597-024-03166-7openalex-snapshot
ForCenS-LGM: a dataset of planktonic foraminifera species assemblage composition for the Last Glacial Maximum
inferred← citeshttps://doi.org/10.1038/s41598-022-10217-9openalex-snapshot
Phases of stability during major hydroclimate change ending the Last Glacial in the Levant
inferred← citeshttps://doi.org/10.1126/sciadv.aba4844openalex-snapshot
Atmospheric circulation over Europe during the Younger Dryas
inferred← citeshttps://doi.org/10.1177/0959683610386819openalex-snapshot
Climatic, vegetation and cultural change in the eastern Mediterranean during the mid-Holocene environmental transition
inferred← citeshttps://doi.org/10.1515/geo-2017-0019openalex-snapshot
Marine sediment cores database for the Mediterranean Basin: a tool for past climatic and environmental studies
inferred← citeshttps://doi.org/10.1594/pangaea.962852openalex-snapshot
ForCenS-LGM – a compilation of planktonic foraminifera assemblage composition for the Last Glacial Maximum
inferred← citeshttps://doi.org/10.2110/jsr.2014.21openalex-snapshot
Genesis and Evolution of A Beach-Ridge Plain Reflecting Relative Sea-Level Rise: A Case Study From Trab El Makhadha Gulf of Gabes, Southeastern Tunisia
inferred← citeshttps://doi.org/10.3390/jmse11122345openalex-snapshot
Towards an Integrated and Accurate Planktonic-Foraminiferal-Deduced Bio-Chrono-Stratigraphic Framework of Late Quaternary Mediterranean Marine Cores
inferred← citeshttps://doi.org/10.3390/jmse8100792openalex-snapshot
Population Genetic Diversity of Two Marine Gobies (Gobiiformes: Gobiidae) from the North-Eastern Atlantic and the Mediterranean Sea
inferred← citeshttps://doi.org/10.3906/tar-1206-53openalex-snapshot
Improved Zonal Method Predictions in a Rectangular Furnace by Smoothing the Exchange Areas
inferred← citeshttps://doi.org/10.3906/yer-1109-7openalex-snapshot
Emerging multi-proxy records of Late Quaternary Palaeoclimate dynamics in Turkey and the surrounding region
inferred← citeshttps://doi.org/10.4000/paleo.4668openalex-snapshot
Étude et description de la sépulture de l’enfant de l’abri Labattut (vallon de Castelmerle, Sergeac, Dordogne, France)
inferred← citeshttps://doi.org/10.5194/cp-11-855-2015openalex-snapshot
Eastern Mediterranean Sea circulation inferred from the conditions of S1 sapropel deposition
inferred← citeshttps://doi.org/10.5194/cp-12-91-2016openalex-snapshot
Holocene climate variability in the North-Western Mediterranean Sea (Gulf of Lions)
inferred← citeshttps://doi.org/10.5194/cp-16-1245-2020openalex-snapshot
Contrasting late-glacial paleoceanographic evolution between the upper and lower continental slope of the western South Atlantic
inferred← citeshttps://doi.org/10.5194/cp-7-1261-2011openalex-snapshot
Hydrological variability in the Northern Levant: a 250 ka multi-proxy record from the Yammoûneh (Lebanon) sedimentary sequence
inferred← citeshttps://doi.org/10.5194/cp-9-1065-2013openalex-snapshot
Tracking atmospheric and riverine terrigenous supplies variability during the last glacial and the Holocene in central Mediterranean
inferred← citeshttps://doi.org/10.5194/cp-9-1375-2013openalex-snapshot
Seemingly divergent sea surface temperature proxy records in the central Mediterranean during the last deglaciation
inferred← citeshttps://doi.org/10.5194/cp-9-499-2013openalex-snapshot
Paleohydrology reconstruction and Holocene climate variability in the South Adriatic Sea
inferred← citeshttps://doi.org/10.5194/cp-9-767-2013openalex-snapshot
Deglacial and Holocene vegetation and climatic changes in the southern Central Mediterranean from a direct land–sea correlation
inferred← citeshttps://doi.org/10.70675/1ab5f4cdza04fz4cedz9ea6zc1ec99248563openalex-snapshot
Restitution des changements de l’hydrologie des masses d’eaux intermédiaires et profondes de la Méditerranée au cours des derniers 145 ka à partir de la mesure de la composition isotopique du Nd de foraminifères
inferred← citeshttps://doi.org/10.70675/4c2c6457zfdecz46e6zb5e3zb272d2e6de8eopenalex-snapshot
Facteurs de contrôle sur le fonctionnement du système turbiditique du Rhône depuis le dernier maximum glaciaire
inferred← citeshttps://doi.org/10.70675/55c3ff40z6fefz416bza0b5z9b64bf106ce5openalex-snapshot
Les environnements du détroit Siculo-Tunisien et paléohydrologie de la Méditerranée pendant le Quaternaire Supérieur
inferred← citeshttps://doi.org/10.70675/a180aff7z5545z445dz9c67z09a9a419ad75openalex-snapshot
Variabilité climatique et environnementale du dernier cycle glaciaire en Méditerranée occidentale : apports des nouveaux biomarqueurs organiques
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