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Magnitudes of sea-level lowstands of the past 500,000 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/10.1007/978-3-662-28603-6_13openalex-snapshot
General Circulation of Water Masses in the Red Sea
inferredcites →https://doi.org/10.1007/978-3-662-28603-6_28openalex-snapshot
Late Pleistocene and Holocene Planktonic Foraminifera from the Red Sea
inferredcites →https://doi.org/10.1007/978-3-662-28603-6_35openalex-snapshot
Radiocarbon Chronology of Red Sea Sediments
inferredcites →https://doi.org/10.1007/978-94-017-4841-4openalex-snapshot
Milankovitch and Climate
inferredcites →https://doi.org/10.1016/0025-3227(93)90062-zopenalex-snapshot
A one million-year-long sequence of marine terraces on Sumba Island, Indonesia
inferredcites →https://doi.org/10.1016/0031-0182(88)90005-3openalex-snapshot
Paleoceanographic record of the last glacial/interglacial cycle in the Red Sea and Gulf of Aden
inferredcites →https://doi.org/10.1016/0277-3791(87)90003-5openalex-snapshot
Oxygen isotopes, ice volume and sea level
inferredcites →https://doi.org/10.1016/0377-8398(93)90015-popenalex-snapshot
Northern Levantine and Adriatic Quaternary planktic foraminifera; Reconstruction of paleoenvironmental gradients
inferredcites →https://doi.org/10.1016/1040-6182(95)00023-copenalex-snapshot
Red Sea outflow during the last glacial maximum
inferredcites →https://doi.org/10.1016/s0198-0254(06)80378-xopenalex-snapshot
Revised reconstruction of Middle and Late Pleistocene sea-level changes based on new chronologic and morphologic investigations in Barbados, West Indies
inferredcites →https://doi.org/10.1029/90pa01881openalex-snapshot
Paleoenvironmental events during the last 13,000 years in the central Red Sea as recorded by pteropoda
inferredcites →https://doi.org/10.1029/90pa01976openalex-snapshot
Evidence for Red Sea surface circulation from oxygen isotopes of modern surface waters and planktonic foraminiferal tests
inferredcites →https://doi.org/10.1029/94pa01648openalex-snapshot
Glacial conditions in the Red Sea
inferredcites →https://doi.org/10.1029/95pa03838openalex-snapshot
Three hundred eighty thousand year long stable isotope and faunal records from the Red Sea: Influence of global sea level change on hydrography
inferredcites →https://doi.org/10.1029/96gl01279openalex-snapshot
Pleistocene sea levels and tectonic uplift based on dating of corals from Sumba Island, Indonesia
inferredcites →https://doi.org/10.1038/324137a0openalex-snapshot
Oxygen isotopes and sea level
inferredcites →https://doi.org/10.1038/342637a0openalex-snapshot
A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation
inferredcites →https://doi.org/10.1038/41201openalex-snapshot
A warm future in the past
inferredcites →https://doi.org/10.1111/j.1439-0485.1981.tb00088.xopenalex-snapshot
Paleoecological Relations of Foraminifera in a Desert-Enclosed Sea -The Gulf of Aqaba (Elat), Red Sea

What points at this work

Incoming claims: where this work appears in other papers’ reference lists and arguments.

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inferred← citeshttps://doi.org/10.1002/jqs.693openalex-snapshot
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inferred← citeshttps://doi.org/10.1002/jqs.865openalex-snapshot
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inferred← citeshttps://doi.org/10.1002/mmnz.200600022openalex-snapshot
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inferred← citeshttps://doi.org/10.1002/tax.602019openalex-snapshot
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inferred← citeshttps://doi.org/10.1006/jhev.1999.0307openalex-snapshot
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inferred← citeshttps://doi.org/10.1006/jhev.2002.0562openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/978-1-4419-1560-3_10openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/978-1-4939-5614-2_5openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/978-3-030-04333-9_10openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/978-3-032-17498-7_16openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/978-3-319-48657-4_365-1openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/978-3-319-93806-6_365openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/978-3-319-99408-6_15openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/978-3-319-99408-6_27openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/978-3-319-99408-6_28openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/978-3-319-99408-6_32openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/978-3-540-33761-4_15openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/978-3-642-39979-4_15openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/978-3-642-55828-3_3openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/978-3-662-45201-1_1openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/978-90-481-2719-1_7openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/978-90-481-8569-6_1openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/978-90-481-9036-2_5openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/978-94-024-1106-5_4openalex-snapshot
Holocene Large Mammal Extinctions in Palawan Island, Philippines
inferred← citeshttps://doi.org/10.1007/s00227-005-0197-9openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s00227-008-1124-7openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s00227-010-1423-7openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s00227-010-1577-3openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s00367-019-00570-6openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s10228-009-0111-4openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s10498-011-9149-9openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s10530-018-1660-0openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s10592-016-0886-6openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s10709-011-9547-3openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s10750-024-05572-9openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s10750-026-06307-8openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s10750-026-06355-0openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s10963-015-9085-5openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s11001-015-9262-zopenalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s11430-014-5049-3openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s11457-005-9004-5openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s11457-026-09509-2openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s11852-018-0644-7openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s12303-018-0049-5openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s12517-012-0641-3openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s12517-013-0851-3openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s12517-015-1884-6openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s12526-019-00995-3openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s12526-026-01686-6openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s12665-018-7747-1openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s13131-023-2265-8openalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s44289-025-00073-6openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/b0-08-043751-6/06116-8openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/b978-0-08-095975-7.00613-6openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/b978-0-12-391851-2.00002-7openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/b978-0-12-815507-3.00002-2openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/b978-0-323-90085-0.00016-4openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/b978-0-323-99931-1.00049-0openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/b978-0-444-53643-3.00132-1openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.avrs.2022.100031openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.biocon.2004.01.020openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.csr.2008.11.005openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.csr.2016.07.009openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.cub.2017.11.021openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.cub.2022.04.034openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.dsr2.2003.11.002openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.earscirev.2014.09.007openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.earscirev.2021.103730openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.epsl.2004.06.008openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.epsl.2006.09.033openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.epsl.2007.06.008openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.epsl.2009.05.027openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.epsl.2009.12.054openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.epsl.2011.08.026openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.epsl.2013.03.036openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.epsl.2013.09.013openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.epsl.2015.08.037openalex-snapshot
Red Sea isolation history suggested by Plio-Pleistocene seismic reflection sequences
inferred← citeshttps://doi.org/10.1016/j.epsl.2016.09.060openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.gca.2005.09.008openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.gca.2011.05.029openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.gca.2020.07.017openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.geomorph.2007.03.012openalex-snapshot
Geomorphological study of long-term erosion on a tropical volcanic ocean island: Tahiti-Nui (French Polynesia)
inferred← citeshttps://doi.org/10.1016/j.geomorph.2008.05.037openalex-snapshot
Quaternary marine terraces as indicators of neotectonic activity of the Ierapetra normal fault SE Crete (Greece)
inferred← citeshttps://doi.org/10.1016/j.geomorph.2012.07.019openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.geomorph.2012.08.012openalex-snapshot
Tectonic influences on the preservation of marine terraces: Old and new evidence from Santa Catalina Island, California
inferred← citeshttps://doi.org/10.1016/j.geomorph.2013.04.037openalex-snapshot
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inferred← citeshttps://doi.org/10.1016/j.geomorph.2013.07.019openalex-snapshot
Quaternary sea-level change and slope instability in coastal areas: Insights from the Vasto Landslide (Adriatic coast, central Italy)
inferred← citeshttps://doi.org/10.1016/j.geomorph.2014.08.006openalex-snapshot
Seafloor morphology of the Montenegro/N. Albania Continental Margin (Adriatic Sea—Central Mediterranean)
inferred← citeshttps://doi.org/10.1016/j.geomorph.2020.107489openalex-snapshot
Quantitative estimation of provenance contributions to loess deposits in Eastern China and implication for paleo-dust storm activity
inferred← citeshttps://doi.org/10.1016/j.geomorph.2026.110421openalex-snapshot
Morphotectonic evolution of the Kaş–Demre Karst Plateau: Cascade-type poljes, submerged poljes and Demre Stream Canyon, Western Taurus–Türkiye
inferred← citeshttps://doi.org/10.1016/j.gexplo.2009.10.001openalex-snapshot
Formation of Thetis Deep metal-rich sediments in the absence of brines, Red Sea
inferred← citeshttps://doi.org/10.1016/j.gexplo.2019.106342openalex-snapshot
Linkage of sulfur isotopic enrichment to sulfur and arsenic release in the coastal aquifers of southwestern Taiwan
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2004.09.010openalex-snapshot
Cenozoic ice sheet history from East Antarctic Wilkes Land continental margin sediments
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2007.03.003openalex-snapshot
Sea-level curves: Perplexities of an end-user in morphotectonic applications
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2009.03.021openalex-snapshot
Influence of regional parameters on the surface mass balance of the Eurasian ice sheet during the peak Saalian (140 kya)
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2016.06.013openalex-snapshot
Interplay between regional uplift and glacio-eustasy in the Crotone Basin (Calabria, southern Italy) since 0.45 Ma: A review
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2024.104527openalex-snapshot
Contourite-like deposits suggest stronger-than-present circulation in the Plio-Pleistocene Red Sea
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.105131openalex-snapshot
Dynamics of the North African climate over the last 600 kyr based on mineralogical and geochemical investigations of deep sediments in the western Mediterranean Sea
inferred← citeshttps://doi.org/10.1016/j.jasrep.2023.104167openalex-snapshot
Changing climates and emerging patterns: Prehistoric human diet of Sri Lanka from Late Pleistocene through Late Holocene
inferred← citeshttps://doi.org/10.1016/j.jcz.2015.10.005openalex-snapshot
On the origin of the recent herpetofauna of Sicily: Comparative phylogeography using homologous mitochondrial and nuclear genes
inferred← citeshttps://doi.org/10.1016/j.jembe.2010.01.019openalex-snapshot
Late Pleistocene population expansion of Scylla paramamosain along the coast of China: A population dynamic response to the Last Interglacial sea level highstand
inferred← citeshttps://doi.org/10.1016/j.jembe.2013.09.012openalex-snapshot
Genetic diversity, population structure, and demographic history of exploited sea urchin populations (Tripneustes gratilla) in the Philippines
inferred← citeshttps://doi.org/10.1016/j.jembe.2019.151181openalex-snapshot
Genetic characterization of green turtles (Chelonia mydas) from São Tomé and Príncipe: Insights on species recruitment and dispersal in the Gulf of Guinea
inferred← citeshttps://doi.org/10.1016/j.jhevol.2009.08.004openalex-snapshot
The presence of a large cercopithecine (cf. Theropithecus sp.) in the ‘Ubeidiya formation (Early Pleistocene, Israel)
inferred← citeshttps://doi.org/10.1016/j.jhevol.2014.08.003openalex-snapshot
Out of Africa, but how and when? The case of hamadryas baboons (Papio hamadryas)
inferred← citeshttps://doi.org/10.1016/j.jhydrol.2010.05.038openalex-snapshot
Effects of Karst and geological structure on groundwater flow: The case of Yarqon-Taninim Aquifer, Israel
inferred← citeshttps://doi.org/10.1016/j.jnc.2017.01.004openalex-snapshot
Employing DNA barcoding as taxonomy and conservation tools for fish species censuses at the southeastern Mediterranean, a hot-spot area for biological invasion
inferred← citeshttps://doi.org/10.1016/j.jsames.2020.102566openalex-snapshot
Late Pleistocene-Holocene fossils from Mirim Lake, Southern Brazil, and their paleoenvironmental significance: I - Vertebrates
inferred← citeshttps://doi.org/10.1016/j.jsames.2020.102605openalex-snapshot
Geological and taphonomic significance of electron spin resonance (ESR) ages of Middle-Late Pleistocene marine shells from barrier-lagoon systems of Southern Brazil
inferred← citeshttps://doi.org/10.1016/j.jsames.2021.103546openalex-snapshot
Late Pleistocene-Holocene fossils from Mirim Lake, southern Brazil, and their paleoenvironmental significance: II – Mollusks
inferred← citeshttps://doi.org/10.1016/j.jsames.2021.103662openalex-snapshot
The influence of coastal evolution on the paleobiogeography of the bivalve Anomalocardia flexuosa (Linné, 1767) along the southwestern Atlantic Ocean
inferred← citeshttps://doi.org/10.1016/j.jseaes.2017.03.028openalex-snapshot
Land-sea duel in the late Quaternary at the mouth of a small river with high sediment yield
inferred← citeshttps://doi.org/10.1016/j.jseaes.2020.104634openalex-snapshot
Depositional sequences of the Mekong river delta and adjacent shelf over the past 140 kyr, southern Vietnam
inferred← citeshttps://doi.org/10.1016/j.jvolgeores.2013.08.013openalex-snapshot
Volcanic evolution of the South Sandwich volcanic arc, South Atlantic, from multibeam bathymetry
inferred← citeshttps://doi.org/10.1016/j.mambio.2011.01.006openalex-snapshot
A new species of Micronycteris (Chiroptera: Phyllostomidae) from Saint Vincent, Lesser Antilles
inferred← citeshttps://doi.org/10.1016/j.margeo.2005.09.006openalex-snapshot
The effect of paleo-oceanographic changes on the sedimentary recording of hydrothermal activity in the Red Sea during the last 30,000 years
inferred← citeshttps://doi.org/10.1016/j.margeo.2006.08.006openalex-snapshot
Glacial/interglacial instabilities of the Western Boundary Under Current during the last 365 kyr from Sm/Nd ratios of the sedimentary clay-size fractions at ODP site 646 (Labrador Sea)
inferred← citeshttps://doi.org/10.1016/j.margeo.2006.09.012openalex-snapshot
Shoreface migrations at the shelf edge and sea-level changes around the Last Glacial Maximum (Gulf of Lions, NW Mediterranean)
inferred← citeshttps://doi.org/10.1016/j.margeo.2009.06.014openalex-snapshot
Sediment accumulation on a cold-water carbonate mound at the Southwest Rockall Trough margin
inferred← citeshttps://doi.org/10.1016/j.margeo.2010.01.019openalex-snapshot
Sea-level rise during Termination II inferred from large benthic foraminifers: IODP Expedition 310, Tahiti Sea Level
inferred← citeshttps://doi.org/10.1016/j.margeo.2014.11.006openalex-snapshot
Stratigraphic architecture of the Montenegro/N. Albania Continental Margin (Adriatic Sea—Central Mediterranean)
inferred← citeshttps://doi.org/10.1016/j.margeo.2015.05.012openalex-snapshot
Late Pleistocene–Holocene evolution of the Doce River delta, southeastern Brazil: Implications for the understanding of wave-influenced deltas
inferred← citeshttps://doi.org/10.1016/j.margeo.2015.09.002openalex-snapshot
Episodic, rapid sea-level rises on the central Mediterranean shelves after the Last Glacial Maximum: A review
inferred← citeshttps://doi.org/10.1016/j.margeo.2022.106730openalex-snapshot
Intermediate water variability of the subtropical Northeastern Atlantic during 490–424 ka (late MIS 13 and MIS 12)
inferred← citeshttps://doi.org/10.1016/j.margeo.2024.107326openalex-snapshot
New chronology for submerged relict paleoshorelines and associated rates of crustal vertical movements offshore the Marzamemi village, Sicily (Southern Italy)
inferred← citeshttps://doi.org/10.1016/j.marmicro.2005.08.002openalex-snapshot
Impact of late Quaternary environmental changes on deep-sea benthic foraminiferal faunas of the Red Sea
inferred← citeshttps://doi.org/10.1016/j.marmicro.2019.03.002openalex-snapshot
Reconstruction of surface water dynamics in the North Atlantic during the Mid-Pleistocene (~540–400 ka), as inferred from coccolithophores and planktonic foraminifera
inferred← citeshttps://doi.org/10.1016/j.marmicro.2022.102181openalex-snapshot
The evolution of seafloor environmental conditions in the southern Red Sea continental shelf during the last 30 ka
inferred← citeshttps://doi.org/10.1016/j.marmicro.2025.102474openalex-snapshot
Deep-sea benthic foraminifera respond to rapid environmental changes in the central Red Sea during the last glacial period
inferred← citeshttps://doi.org/10.1016/j.marpetgeo.2014.03.015openalex-snapshot
Multi-sourced depositional sequences in the Neogene to Quaternary succession of the Venice area (northern Italy)
inferred← citeshttps://doi.org/10.1016/j.marpetgeo.2016.11.009openalex-snapshot
Genesis of the Northern Adriatic Sea (Northern Italy) since early Pliocene
inferred← citeshttps://doi.org/10.1016/j.marpetgeo.2019.104204openalex-snapshot
Emergence of a submarine canyon, Crotone Basin, southern Italy
inferred← citeshttps://doi.org/10.1016/j.marpetgeo.2020.104675openalex-snapshot
The evolution of a coastal wedge in response to Plio-Pleistocene climate change: The Northern Adriatic case
inferred← citeshttps://doi.org/10.1016/j.marpetgeo.2023.106453openalex-snapshot
Slip-rates and time recurrences of the seismogenic Sant’Eufemia normal fault (SE Tyrrhenian Sea), a multiscale and multidisciplinary approach
inferred← citeshttps://doi.org/10.1016/j.marpetgeo.2024.106829openalex-snapshot
Formation of dolomites from the newly discovered ancient cold seep in the Middle Dongsha area of the South China Sea
inferred← citeshttps://doi.org/10.1016/j.measurement.2018.05.052openalex-snapshot
Shallow water acoustic techniques to investigate transitional environments: A case study over Boka Kotorska Bay
inferred← citeshttps://doi.org/10.1016/j.meegid.2016.05.036openalex-snapshot
Detailed phylogenetic analysis of primate T-lymphotropic virus type 1 (PTLV-1) sequences from orangutans ( Pongo pygmaeus ) reveals new insights into the evolutionary history of PTLV-1 in Asia
inferred← citeshttps://doi.org/10.1016/j.orggeochem.2009.03.001openalex-snapshot
Distribution of Crenarchaeota tetraether membrane lipids in surface sediments from the Red Sea
inferred← citeshttps://doi.org/10.1016/j.palaeo.2006.11.020openalex-snapshot
Orbital-scale stratigraphy and high-resolution analysis of biogenic components and deep-water oxygenation conditions in the Japan Sea during the last 640 kyr
inferred← citeshttps://doi.org/10.1016/j.palaeo.2008.04.003openalex-snapshot
The first evidence for the past presence of the tiger Panthera tigris (L.) on the island of Palawan, Philippines: Extinction in an island population
inferred← citeshttps://doi.org/10.1016/j.palaeo.2008.09.009openalex-snapshot
West coast dune plumes: Climate driven contrasts in dunefield morphogenesis along the western and southern South African coasts
inferred← citeshttps://doi.org/10.1016/j.palaeo.2009.06.003openalex-snapshot
Tropical marine climate during the late Paleozoic ice age using trace element analyses of brachiopods
inferred← citeshttps://doi.org/10.1016/j.palaeo.2010.05.018openalex-snapshot
The western North Atlantic record of MIS 13 to 10: Changes in primary productivity, organic carbon accumulation and benthic foraminiferal assemblages in sediments from the Blake Outer Ridge (ODP Site 1058)
inferred← citeshttps://doi.org/10.1016/j.palaeo.2012.03.005openalex-snapshot
The meridional temperature gradient in the eastern North Atlantic during MIS 11 and its link to the ocean–atmosphere system
inferred← citeshttps://doi.org/10.1016/j.palaeo.2012.04.011openalex-snapshot
Origin of deep water in the Japan Sea over the last 145kyr
inferred← citeshttps://doi.org/10.1016/j.palaeo.2013.09.005openalex-snapshot
Calcareous plankton response to orbital and millennial-scale climate changes across the Middle Pleistocene in the western Mediterranean
inferred← citeshttps://doi.org/10.1016/j.palaeo.2013.12.001openalex-snapshot
Landscape evolution during the late Quaternary at the Doce River mouth, Espírito Santo State, Southeastern Brazil
inferred← citeshttps://doi.org/10.1016/j.palaeo.2015.11.009openalex-snapshot
Central Mediterranean Mid-Pleistocene paleoclimatic variability and its association with global climate
inferred← citeshttps://doi.org/10.1016/j.palaeo.2016.07.006openalex-snapshot
Sea surface water variability during the Mid-Brunhes inferred from calcareous plankton in the western Mediterranean (ODP Site 975)
inferred← citeshttps://doi.org/10.1016/j.palaeo.2022.111377openalex-snapshot
Pollen-based quantitative paleoclimatic record spanning the Mid-Brunhes Event in the Nihewan Basin, north China
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111907openalex-snapshot
Climate-induced surface water variability at Monte San Nicola type-section (Sicily, southern Italy): New data across the Gelasian GSSP
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111980openalex-snapshot
Impact of hydrological changes and vertical motions on Pleistocene marine environments of the eastern coast of the island of Rhodes (Greece)
inferred← citeshttps://doi.org/10.1016/j.palaeo.2026.113679openalex-snapshot
Modes of deep-water circulation in the subtropical South Atlantic over the last 770 kyr revealed by a zonal δ13C gradient
inferred← citeshttps://doi.org/10.1016/j.palaeo.2026.114213openalex-snapshot
Glacial–interglacial provenance shifts in Laizhou Bay: deciphering Yellow River avulsion history from detrital zircon records
inferred← citeshttps://doi.org/10.1016/j.ppees.2012.01.003openalex-snapshot
Pollination, biogeography and phylogeny of oceanic island bellflowers (Campanulaceae)
inferred← citeshttps://doi.org/10.1016/j.quageo.2010.05.002openalex-snapshot
Comparative dating of a Bison-bearing late-Pleistocene deposit, Térapa, Sonora, Mexico
inferred← citeshttps://doi.org/10.1016/j.quaint.2005.11.015openalex-snapshot
East European loess–palaeosol sequences: Palynology, stratigraphy and correlation
inferred← citeshttps://doi.org/10.1016/j.quaint.2005.12.010openalex-snapshot
Long-term palaeoenvironmental changes recorded in palynologically studied loess–palaeosol and ESR-dated marine deposits of Northern Eurasia: Implications for sea–land correlation
inferred← citeshttps://doi.org/10.1016/j.quaint.2008.05.015openalex-snapshot
The great arc of dispersal of modern humans: Africa to Australia
inferred← citeshttps://doi.org/10.1016/j.quaint.2010.07.009openalex-snapshot
Palaeozoology of Palawan Island, Philippines
inferred← citeshttps://doi.org/10.1016/j.quaint.2011.02.043openalex-snapshot
Early to Middle Pleistocene Homo dispersals from Africa to Eurasia: Geological, climatic and environmental constraints
inferred← citeshttps://doi.org/10.1016/j.quaint.2012.08.2102openalex-snapshot
Loess record of climatic changes during MIS 12–10 in the Jingyuan section, northwestern Chinese Loess Plateau
inferred← citeshttps://doi.org/10.1016/j.quaint.2013.07.020openalex-snapshot
ESR dating of Pleistocene mammals and marine shells from the coastal plain of Rio Grande do Sul state, southern Brazil
inferred← citeshttps://doi.org/10.1016/j.quaint.2013.10.037openalex-snapshot
The stratigraphy and paleogeography of the Middle Paleolithic open-air site of ‘Ein Qashish, Northern Israel
inferred← citeshttps://doi.org/10.1016/j.quaint.2015.03.034openalex-snapshot
The last occurrence of Megaceroides algericus Lyddekker, 1890 (Mammalia, Cervidae) during the middle Holocene in the cave of Bizmoune (Morocco, Essaouira region)
inferred← citeshttps://doi.org/10.1016/j.quaint.2015.11.145openalex-snapshot
Magnitudes of sea-level falls at lowstands of the past 900,000 years inferred from gravels underlying the Nobi Plain, central Japan
inferred← citeshttps://doi.org/10.1016/j.quaint.2017.03.042openalex-snapshot
Sea-level variations during Marine Isotope Stage 7 and coastal tectonics in the eastern Seto Inland Sea area, western Japan
inferred← citeshttps://doi.org/10.1016/j.quaint.2017.06.025openalex-snapshot
Late Quaternary sea-level changes and early human societies in the central and eastern Mediterranean Basin: An interdisciplinary review
inferred← citeshttps://doi.org/10.1016/j.quaint.2017.06.031openalex-snapshot
Transition from incised valley to barrier island systems during MIS 5e in the northern Chiba area, Kanto Plain, central Japan
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