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Temporal variability in the northern Arabian Sea oxygen minimum zone (OMZ) during the last 225,000 years

https://doi.org/10.1029/98pa02203
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Outgoing claims: the papers this work cites, builds on, or argues with.

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Physical Oceanography of the Indian Ocean
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Nitrogen Isotope Fractionation in the Modern Ocean: Implications for the Sedimentary Record
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The Use of Nitrogen Isotopic Ratio for Reconstruction of Past Changes in Surface Ocean Nutrient Utilization
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Seasonal variability of ?15N in settling particles in the Arabian Sea and its palaeogeochemical significance
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Oceanographic atlas of the International Indian ocean expedition
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Geochemical studies of the recent sapropel and associated sediment from the Hellenic Outer Ridge, eastern Mediterranean Sea. I: Mineralogy and chemical composition
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The ratio in the Cenozoic Bengal Abyssal Fan sediments and its use as a paleostream energy indicator
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Stable-isotope studies of planktonic foraminifera in North Atlantic core tops
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The Marine Oxygen Isotope Record in Pleistocene Coral, Barbados, West Indies
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Holocene Variations of Monsoon Rainfall in Rajasthan
inferredcites →https://doi.org/10.1016/0033-5894(83)90024-8openalex-snapshot
Estimates of Holocene Precipitation for Rajasthan, India, Based on Pollen and Lake-Level Data
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Age Dating and the Orbital Theory of the Ice Ages: Development of a High-Resolution 0 to 300,000-Year Chronostratigraphy
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Origin and Consequences of Cyclic Ice Rafting in the Northeast Atlantic Ocean During the Past 130,000 Years
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inferredcites →https://doi.org/10.1016/0146-6291(78)90552-0openalex-snapshot
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inferredcites →https://doi.org/10.1016/0304-4203(75)90009-2openalex-snapshot
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inferredcites →https://doi.org/10.1016/0304-4203(92)90028-9openalex-snapshot
Fluxes of amino acids and hexosamines to the deep Arabian Sea
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Planktonic foraminifera of the northern Indian Ocean: Distribution and preservation in surface sediments
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Thermocline circulation and ventilation in the Indian Ocean derived from water mass analysis
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Radiocarbon Age Calibration of Marine Samples Back to 9000 Cal Yr BP
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Late Pleistocene Variability of the Carbon Isotopic Composition of Organic Matter in the Eastern Mediterranean: Monitor of Changes in Carbon Sources and Atmospheric CO2 Concentrations
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inferredcites →https://doi.org/10.1029/pa005i002p00147openalex-snapshot
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inferredcites →https://doi.org/10.1029/pa005i003p00409openalex-snapshot
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inferredcites →https://doi.org/10.1038/280554a0openalex-snapshot
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inferredcites →https://doi.org/10.1038/295494a0openalex-snapshot
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inferredcites →https://doi.org/10.1038/296056a0openalex-snapshot
Climatic conditions deduced from a 150-kyr oxygen isotope–pollen record from the Arabian Sea
inferredcites →https://doi.org/10.1038/304046a0openalex-snapshot
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inferredcites →https://doi.org/10.1038/31750openalex-snapshot
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Century-scale events in monsoonal climate over the past 24,000 years
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Correlations between climate records from North Atlantic sediments and Greenland ice
inferredcites →https://doi.org/10.1038/366552a0openalex-snapshot
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inferredcites →https://doi.org/10.1038/373506a0openalex-snapshot
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inferredcites →https://doi.org/10.1038/375305a0openalex-snapshot
Correlation between climate events in the North Atlantic and China during the last glaciation
inferredcites →https://doi.org/10.1038/384549a0openalex-snapshot
Mechanism of the biological response to winter cooling in the northeastern Arabian Sea
inferredcites →https://doi.org/10.1038/385241a0openalex-snapshot
Low-latitude glacial cooling in the Southern Hemisphere from amino-acid racemization in emu eggshells
inferredcites →https://doi.org/10.1038/385707a0openalex-snapshot
Interhemispheric synchrony of the last deglaciation inferred from alkenone palaeothermometry
inferredcites →https://doi.org/10.1126/science.194.4270.1121openalex-snapshot
Variations in the Earth's Orbit: Pacemaker of the Ice Ages
inferredcites →https://doi.org/10.1126/science.207.4434.943openalex-snapshot
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inferredcites →https://doi.org/10.1126/science.214.4516.59openalex-snapshot
Monsoon Climate of the Early Holocene: Climate Experiment with the Earth's Orbital Parameters for 9000 Years Ago
inferredcites →https://doi.org/10.1126/science.236.4808.1547openalex-snapshot
Precise Timing of the Last Interglacial Period from Mass Spectrometric Determination of Thorium-230 in Corals
inferredcites →https://doi.org/10.1126/science.263.5148.796openalex-snapshot
The Timing of High Sea Levels Over the Past 200,000 Years
inferredcites →https://doi.org/10.1126/science.269.5220.46openalex-snapshot
Late Glacial Stage and Holocene Tropical Ice Core Records from Huascarán, Peru
inferredcites →https://doi.org/10.1126/science.274.5289.943openalex-snapshot
Nonstationary Phase of the Plio-Pleistocene Asian Monsoon
inferredcites →https://doi.org/10.1144/gsl.sp.1992.064.01.06openalex-snapshot
Foraminiferal production and monsoonal upwelling in the Arabian Sea: evidence from sediment traps
inferredcites →https://doi.org/10.1144/gsl.sp.1992.064.01.20openalex-snapshot
Late Pliocene and Pleistocene climatic oscillations and monsoon upwelling recorded in sediments from the Owen Ridge, northwestern Arabian Sea
inferredcites →https://doi.org/10.1179/030801878791926001openalex-snapshot
A Voyage of Discovery. George Deacon 70th Anniversary Volume
inferredcites →https://doi.org/10.2113/gsjfr.15.4.254openalex-snapshot
Field and laboratory studies on the ontogeny and ecology of some globorotaliid species from the Sargasso Sea off Bermuda
inferredcites →https://doi.org/10.2113/gsjfr.6.4.258openalex-snapshot
Planktonic foraminifera from near the West African coast and a consideration of faunal parcelling in the North Atlantic
inferredcites →https://doi.org/10.2307/1484724openalex-snapshot
Significance of Distribution of Planktonic Foraminifera in the Equatorial Atlantic Undercurrent
inferredcites →https://doi.org/10.2307/1485035openalex-snapshot
Winter Distribution of Planktonic Foraminifera between the Grand Banks and the Caribbean
inferredcites →https://doi.org/10.2307/1485143openalex-snapshot
Seasonal Distribution of Planktonic Foraminifera in the Western North Atlantic
inferredcites →https://doi.org/10.2307/1485406openalex-snapshot
Ecology of Planktonic Foraminifera and Biogeographic Patterns of Life and Fossil Assemblages in the Indian Ocean
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The Benthic Foraminiferal Faunas of Sites 725, 726, and 728 (Oman Margin, Northwestern Arabian Sea)
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The eastern tropical Pacific as a source of 15N‐enriched nitrate in seawater off southern California
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Modern planktonic foraminifera

What points at this work

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

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Asian Winter Monsoon Controlling Productivity Variations in North Arabian Sea During the Holocene
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Late Holocene primary productivity and sea surface temperature variations in the northeastern Arabian Sea: Implications for winter monsoon variability
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Coherent pan‐Asian climatic and isotopic response to orbital forcing of tropical insolation
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Varying responses to I ndian monsoons during the past 220 kyr recorded in deep‐sea sediments in inner and outer regions of the G ulf of A den
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Methane hydrates in Quaternary climate change : the clathrate gun hypothesis
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Diagenetic modulation of the magnetic properties in sediments from the Northern Indian Ocean
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Did the Indo‐Asian summer monsoon decrease during the Holocene following insolation?
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Palaeoproductivity evolution in the centre of the western Pacific warm pool during the last 250 ka
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Late Quaternary record of Indian summer monsoon‐induced stratification and productivity collapse in the Andaman Sea
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The Toba Volcanic Event and Interstadial/Stadial Climates at the Marine Isotopic Stage 5 to 4 Transition in the Northern Indian Ocean
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Palaeoenvironmental changes in the arid and sub arid belt (Sahara-Sahel-Arabian Peninsula) from 150 kyr to present
inferred← citeshttps://doi.org/10.1007/978-3-030-47279-5_7openalex-snapshot
Extreme Morphological Plasticity Within Orbulina-“Praeorbulina-Like” Assemblages Related to Environmental Stress
inferred← citeshttps://doi.org/10.1007/978-3-030-51506-5_26openalex-snapshot
Marine Mammals of the Arabian Seas
inferred← citeshttps://doi.org/10.1007/978-3-540-44930-0_8openalex-snapshot
Geochemical implications for changing dust supply by the Indian Monsoon system to the Arabian Sea during the last glacial cycle
inferred← citeshttps://doi.org/10.1007/978-90-481-2719-1_3openalex-snapshot
Pleistocene Climate Change in Arabia: Developing a Framework for Hominin Dispersal over the Last 350 ka
inferred← citeshttps://doi.org/10.1007/978-94-007-6016-5_2openalex-snapshot
Monsoonal Fluctuations vs Marine Productivity during Past 10,000 Years — A Study Based on Sediment Core Retrieved from Southeastern Arabian Sea
inferred← citeshttps://doi.org/10.1007/978-94-007-7817-7_3openalex-snapshot
Asian Monsoon Variability Recorded in Other Archives
inferred← citeshttps://doi.org/10.1007/s00367-005-0012-0openalex-snapshot
Paleomonsoon precipitation deduced from a sediment core from the equatorial Indian Ocean
inferred← citeshttps://doi.org/10.1007/s00367-019-00570-6openalex-snapshot
Last 35,000-year water column temperature and productivity variation in the Eastern Arabian Sea: monsoon and global climate connection
inferred← citeshttps://doi.org/10.1007/s00367-022-00736-9openalex-snapshot
Glacial-interglacial differences in carbonate burial in the equatorial Indian Ocean
inferred← citeshttps://doi.org/10.1007/s00382-007-0308-zopenalex-snapshot
Simulation of the evolutionary response of global summer monsoons to orbital forcing over the past 280,000 years
inferred← citeshttps://doi.org/10.1007/s10531-020-02056-9openalex-snapshot
A highly diverse living benthic foraminiferal assemblage in the oxygen deficient zone of the southeastern Arabian Sea
inferred← citeshttps://doi.org/10.1007/s11430-020-9720-yopenalex-snapshot
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inferred← citeshttps://doi.org/10.1007/s11430-025-1860-0openalex-snapshot
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Late Quaternary changes in surface productivity and oxygen minimum zone (OMZ) in the northwestern Arabian Sea: Micropaleontologic and sedimentary record at ODP site 728A
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Late Glacial–Holocene record of benthic foraminiferal morphogroups from the eastern Arabian Sea OMZ: Paleoenvironmental implications
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Benthic foraminiferal response to changes in the northwestern Arabian Sea oxygen minimum zone (OMZ) during past $$\sim$$145 kyr
inferred← citeshttps://doi.org/10.1007/s12040-021-01796-8openalex-snapshot
Glacial–interglacial contrast in deep-water δ13C of the Arabian Sea
inferred← citeshttps://doi.org/10.1007/s12517-025-12291-5openalex-snapshot
Role of monsoonal changes in surface hydrography of the northwest Arabian Sea during the past 145 ka
inferred← citeshttps://doi.org/10.1007/s12526-013-0178-zopenalex-snapshot
Agglutinated foraminifera (superfamily Hormosinacea) across the Indian margin oxygen minimum zone (Arabian Sea)
inferred← citeshttps://doi.org/10.1007/s12594-013-0086-7openalex-snapshot
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Molecular and isotopic signatures of oil-driven bacterial sulfate reduction at seeps in the southern Gulf of Mexico
inferred← citeshttps://doi.org/10.1016/j.chemgeo.2022.121300openalex-snapshot
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Response of trace metal redox proxies in continental shelf environment: The Eastern Arabian Sea scenario
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Global distribution of naturally occurring marine hypoxia on continental margins
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Impact of oxygen-depleted water on the vertical distribution of chaetognaths in the northeastern Arabian Sea
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Factors influencing the distribution of epibenthic megafauna across the Peruvian oxygen minimum zone
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Carbonate and carbon fluctuations in the Eastern Arabian Sea over 140ka: Implications on productivity changes?
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Holocene monsoon and sea level-related changes of sedimentation in the northeastern Arabian Sea
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Observed variability of monsoon blooms in the north-central Arabian Sea and its implication on oxygen concentration: A bio-argo study
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Sequence stratigraphy in organic-rich marine mudstone successions using chemostratigraphic datasets
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Multi-proxy reconstruction of surface water pCO2 in the northern Arabian Sea since 29ka
inferred← citeshttps://doi.org/10.1016/j.epsl.2011.06.019openalex-snapshot
New Arabian Sea records help decipher orbital timing of Indo-Asian monsoon
inferred← citeshttps://doi.org/10.1016/j.epsl.2023.118117openalex-snapshot
Precessional pacing of early Proterozoic redox cycles
inferred← citeshttps://doi.org/10.1016/j.gca.2004.03.015openalex-snapshot
Geochemical evidence for abrupt changes in relative strength of the Arabian monsoons during a stadial/interstadial climate transition
inferred← citeshttps://doi.org/10.1016/j.gca.2004.05.044openalex-snapshot
Phosphorus burial as a function of paleoproductivity and redox conditions in Arabian Sea sediments
inferred← citeshttps://doi.org/10.1016/j.gca.2009.08.028openalex-snapshot
Millennial/centennial-scale thermocline ventilation changes in the Indian Ocean as reflected by aragonite preservation and geochemical variations in Arabian Sea sediments
inferred← citeshttps://doi.org/10.1016/j.gca.2012.03.038openalex-snapshot
Selenium as paleo-oceanographic proxy: A first assessment
inferred← citeshttps://doi.org/10.1016/j.gca.2017.02.032openalex-snapshot
The influence of oxygen exposure time on the composition of macromolecular organic matter as revealed by surface sediments on the Murray Ridge (Arabian Sea)
inferred← citeshttps://doi.org/10.1016/j.gca.2026.07.030openalex-snapshot
Particulate manganese shuttling shapes molybdenum and thallium isotope compositions in surface sediments of the Arabian Sea oxygen minimum zone
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2024.104397openalex-snapshot
Surface oceanographic changes from ∼ 25,000 to 3500 cal yr BP in the eastern Arabian Sea
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2024.104398openalex-snapshot
Abrupt intensification of AMOC and monsoonal winds during mid-MIS4 (Heinrich Event 6) in the western Arabian Sea
inferred← citeshttps://doi.org/10.1016/j.gloplacha.2026.105373openalex-snapshot
Orbital forcing regulated Arabian Sea denitrification during the late Pleistocene
inferred← citeshttps://doi.org/10.1016/j.jembe.2010.12.015openalex-snapshot
Oxygen minimum seafloor ecological (mal) functioning
inferred← citeshttps://doi.org/10.1016/j.jhevol.2008.09.004openalex-snapshot
Out of Africa and into an ice age: on the role of global climate change in the late Pleistocene migration of early modern humans out of Africa
inferred← citeshttps://doi.org/10.1016/j.jseaes.2010.08.002openalex-snapshot
A prolonged warm and humid interval during marine isotope stage 13–15 as revealed by hydrographic reconstructions from the South China Sea (IMAGES MD972142)
inferred← citeshttps://doi.org/10.1016/j.jseaes.2021.104882openalex-snapshot
Indian monsoon wind variability since ~11 kyr in the northwestern and northeastern Arabian Sea
inferred← citeshttps://doi.org/10.1016/j.jseaes.2021.104904openalex-snapshot
Ocean acidification in the Northern Indian ocean : A review
inferred← citeshttps://doi.org/10.1016/j.jseaes.2022.105094openalex-snapshot
Mid-Holocene intensification of the oxygen minimum zone in the northeastern Arabian Sea
inferred← citeshttps://doi.org/10.1016/j.jseaes.2022.105102openalex-snapshot
Geochemistry and granulometry as indicators of paleoclimate, weathering, and provenance of sediments for the past 1,00,000 years in the eastern Arabian Sea
inferred← citeshttps://doi.org/10.1016/j.jseaes.2026.107130openalex-snapshot
Integrated paleo lithogenic and redox signals in NE Arabian Sea sediments since 16 ka: A major element geochemistry approach
inferred← citeshttps://doi.org/10.1016/j.margeo.2005.02.028openalex-snapshot
Precessional forcing of coccolithophore assemblages in the northern Arabian Sea: Implications for monsoonal dynamics during the last 200,000 years
inferred← citeshttps://doi.org/10.1016/j.margeo.2005.05.004openalex-snapshot
Monsoon related changes in sea surface productivity and water column denitrification in the Eastern Arabian Sea during the last glacial cycle
inferred← citeshttps://doi.org/10.1016/j.margeo.2006.05.013openalex-snapshot
Sedimentary trace element records over the last 200 kyr from within and below the northern Arabian Sea oxygen minimum zone
inferred← citeshttps://doi.org/10.1016/j.margeo.2006.05.014openalex-snapshot
Recent and Late Quaternary pteropod preservation on the Pakistan shelf and continental slope
inferred← citeshttps://doi.org/10.1016/j.margeo.2010.04.005openalex-snapshot
Highstand vs. lowstand turbidite system growth in the Makran active margin: Imprints of high-frequency external controls on sediment delivery mechanisms to deep water systems
inferred← citeshttps://doi.org/10.1016/j.margeo.2010.06.003openalex-snapshot
Late Quaternary record of pteropod preservation from the Andaman Sea
inferred← citeshttps://doi.org/10.1016/j.margeo.2013.11.010openalex-snapshot
Equatorial Indian Ocean productivity during the last 33kyr and possible linkage to Westerly Jet variability
inferred← citeshttps://doi.org/10.1016/j.margeo.2022.106958openalex-snapshot
A ∼ 50 kyr record of carbonate (pteropods) preservation from the Laccadive Sea, Northern Indian Ocean
inferred← citeshttps://doi.org/10.1016/j.margeo.2023.107165openalex-snapshot
Mineralogy, geochemistry and genesis of the polymetallic crusts from the Chagos-Laccadive Ridge, Arabian Sea, India
inferred← citeshttps://doi.org/10.1016/j.margeo.2024.107307openalex-snapshot
Centennial-millennial scale global climate-linked monsoonal and non-monsoonal changes in the eastern Arabian Sea during the last 42,800 years
inferred← citeshttps://doi.org/10.1016/j.margeo.2024.107416openalex-snapshot
Evolution process of chemical weathering and sediment sources in the Makran Continental margin since the Younger Dryas
inferred← citeshttps://doi.org/10.1016/j.marmicro.2006.02.004openalex-snapshot
Late Quaternary millennial-scale variability in pelagic aragonite preservation off Somalia
inferred← citeshttps://doi.org/10.1016/j.marmicro.2006.07.004openalex-snapshot
Live (Rose Bengal stained) and dead benthic foraminifera from the oxygen minimum zone of the Pakistan continental margin (Arabian Sea)
inferred← citeshttps://doi.org/10.1016/j.marmicro.2006.11.004openalex-snapshot
Reconstruction of Indian monsoon variability over the past 230,000 years: Planktic foraminiferal evidence from the NW Arabian Sea open-ocean upwelling area
inferred← citeshttps://doi.org/10.1016/j.marmicro.2011.01.006openalex-snapshot
High occurrence of Orbulina suturalis and “Praeorbulina-like specimens” in sediments of the northern Arabian Sea during the Last Glacial Maximum
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.marpetgeo.2014.05.007openalex-snapshot
Monsoon-influenced variation in productivity and lithogenic sediment flux since 110 ka in the offshore Mahanadi Basin, northern Bay of Bengal
inferred← citeshttps://doi.org/10.1016/j.marpolbul.2021.112883openalex-snapshot
Untangling the effect of organic matter and dissolved oxygen on living benthic foraminifera in the southeastern Arabian Sea
inferred← citeshttps://doi.org/10.1016/j.orggeochem.2004.01.012openalex-snapshot
The effect of maturity and depositional redox conditions on archaeal tetraether lipid palaeothermometry
inferred← citeshttps://doi.org/10.1016/j.palaeo.2006.08.008openalex-snapshot
Millennial-scale paleoclimate cycles recorded in widespread Palaeozoic deeper water rhythmites of North America
inferred← citeshttps://doi.org/10.1016/j.palaeo.2007.01.014openalex-snapshot
Sea surface temperatures during the SW and NE monsoon seasons in the western Arabian Sea over the past 20,000 years
inferred← citeshttps://doi.org/10.1016/j.palaeo.2008.01.012openalex-snapshot
A major change in monsoon-driven productivity in the tropical Indian Ocean during ca 1.2–0.9 Myr: Foraminiferal faunal and stable isotope data
inferred← citeshttps://doi.org/10.1016/j.palaeo.2011.10.013openalex-snapshot
Astronomical forcing of Northwest African climate and glacial history during the late Messinian (6.5–5.5Ma)
inferred← citeshttps://doi.org/10.1016/j.palaeo.2015.02.036openalex-snapshot
Contrasting sea surface temperature of summer and winter monsoon variability in the northern Arabian Sea over the last 25 ka
inferred← citeshttps://doi.org/10.1016/j.palaeo.2015.06.006openalex-snapshot
Evolution of productivity and monsoonal dynamics in the eastern Arabian Sea during the past 68ka using dinoflagellate cyst records
inferred← citeshttps://doi.org/10.1016/j.palaeo.2016.09.014openalex-snapshot
A first look at factors affecting aragonite compensation depth in the eastern Arabian Sea
inferred← citeshttps://doi.org/10.1016/j.palaeo.2016.10.035openalex-snapshot
Holocene strengthening of the Oxygen Minimum Zone in the northwestern Arabian Sea linked to changes in intermediate water circulation or Indian monsoon intensity?
inferred← citeshttps://doi.org/10.1016/j.palaeo.2018.11.040openalex-snapshot
Indian Summer Monsoon variations and competing influences between hemispheres since ~35 ka recorded in Tengchongqinghai Lake, southwestern China
inferred← citeshttps://doi.org/10.1016/j.palaeo.2020.109969openalex-snapshot
Source shifts to periplatform deposits during the early to middle Miocene in response to climatic and oceanographic forcing, Maldives, western Indian Ocean
inferred← citeshttps://doi.org/10.1016/j.palaeo.2020.110018openalex-snapshot
A paleoproductivity shift in the northwestern Bay of Bengal (IODP Site U1445) across the Mid-Pleistocene transition in response to weakening of the Indian summer monsoon
inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110755openalex-snapshot
Remote forcing of winter cooling in the Arabian Sea: Implications for the NE monsoon
inferred← citeshttps://doi.org/10.1016/j.palaeo.2022.110844openalex-snapshot
Monsoon-related changes in surface hydrography and productivity in the Bay of Bengal over the last 45 kyr BP
inferred← citeshttps://doi.org/10.1016/j.palaeo.2022.110891openalex-snapshot
Late Quaternary variations in the Oxygen Minimum Zone linked to monsoon shifts as seen in the sediment of the outer continental shelf of the eastern Arabian Sea
inferred← citeshttps://doi.org/10.1016/j.palaeo.2023.111443openalex-snapshot
Editorial preface to special issue: Recent advances in Indian Ocean paleoceanography and paleoclimate
inferred← citeshttps://doi.org/10.1016/j.palaeo.2024.112287openalex-snapshot
Asian winter monsoon controls marine primary productivity in north Arabian Sea during the Holocene
inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.113384openalex-snapshot
Decoding the sedimentary responses to the monsoon seasonality and ocean circulation in the southeast Arabian Sea during the last 50 ka
inferred← citeshttps://doi.org/10.1016/j.pocean.2008.03.001openalex-snapshot
Vertical zonation and distributions of calanoid copepods through the lower oxycline of the Arabian Sea oxygen minimum zone
inferred← citeshttps://doi.org/10.1016/j.quaint.2008.10.010openalex-snapshot
Carbonate and organic carbon content changes over last 20ka in the Southeastern Arabian Sea: Paleoceanographic implications
inferred← citeshttps://doi.org/10.1016/j.quaint.2014.11.052openalex-snapshot
Benthic foraminiferal diversity response to the climate induced changes in the eastern Arabian Sea oxygen minimum zone during the last 30kaBP
inferred← citeshttps://doi.org/10.1016/j.quaint.2014.12.014openalex-snapshot
Stalagmite δ18O variations in southern India reveal divergent trends of Indian Summer Monsoon and East Asian Summer Monsoon during the last interglacial
inferred← citeshttps://doi.org/10.1016/j.quaint.2015.01.005openalex-snapshot
Orbital-scale climate variability in Arabia as a potential motor for human dispersals
inferred← citeshttps://doi.org/10.1016/j.quaint.2018.03.027openalex-snapshot
Rapid switch in monsoon-wind induced surface hydrographic conditions of the eastern Arabian Sea during the last deglaciation
inferred← citeshttps://doi.org/10.1016/j.quaint.2018.08.005openalex-snapshot
Significant seasonal contrast in the Arabian Sea during deglaciation: Evidence from oxygen isotopic analyses of individual planktic foraminifera
inferred← citeshttps://doi.org/10.1016/j.quaint.2020.08.024openalex-snapshot
Paleoenvironment of the Central Himalaya during late MIS 3 using stable isotopic compositions of lacustrine organic matter occluded in diatoms and sediments
inferred← citeshttps://doi.org/10.1016/j.quaint.2021.04.002openalex-snapshot
The equatorial Indian Ocean upper water-column structure influenced by cross-basinal water exchange over the last ~40000 years
inferred← citeshttps://doi.org/10.1016/j.quaint.2021.07.017openalex-snapshot
Astronomical forcing of vegetation and climate change during the Late Pliocene–Early Pleistocene of the Nihewan Basin, North China
inferred← citeshttps://doi.org/10.1016/j.quaint.2022.03.016openalex-snapshot
Indian monsoon variability during the past ∼8.5 cal kyr as recorded in the sediments of the northeastern Arabian Sea
inferred← citeshttps://doi.org/10.1016/j.quaint.2024.05.007openalex-snapshot
Reconstructing hypoxia on the eastern Arabian sea continental shelf during the past ∼7400 years: A multi-proxy approach
inferred← citeshttps://doi.org/10.1016/j.quaint.2026.110200openalex-snapshot
High-resolution planktonic foraminiferal and geochemical proxy records reveal Holocene monsoon-driven changes and solar-cycle imprints in the northeastern Arabian Sea
inferred← citeshttps://doi.org/10.1016/j.quascirev.2004.10.002openalex-snapshot
Evolution and variability of the Asian monsoon system: state of the art and outstanding issues
inferred← citeshttps://doi.org/10.1016/j.quascirev.2006.11.010openalex-snapshot
The timing of orbital-scale Indian monsoon changes
inferred← citeshttps://doi.org/10.1016/j.quascirev.2007.10.001openalex-snapshot
Variation in production, input and preservation of metastable calcium carbonate off Somalia during the last 90,000 years
inferred← citeshttps://doi.org/10.1016/j.quascirev.2009.06.001openalex-snapshot
Book Review
inferred← citeshttps://doi.org/10.1016/j.quascirev.2012.10.008openalex-snapshot
Bi-hemispheric forcing for Indo-Asian monsoon during glacial terminations
inferred← citeshttps://doi.org/10.1016/j.quascirev.2013.07.031openalex-snapshot
A 500,000 year record of Indian summer monsoon dynamics recorded by eastern equatorial Indian Ocean upper water-column structure
inferred← citeshttps://doi.org/10.1016/j.quascirev.2013.08.014openalex-snapshot
Millennial-scale ice rafting events and Hudson Strait Heinrich(-like) Events during the late Pliocene and Pleistocene: a review
inferred← citeshttps://doi.org/10.1016/j.quascirev.2022.107403openalex-snapshot
Indian Summer Monsoon variability 140–70 thousand years ago based on multi-proxy records from the Bay of Bengal
inferred← citeshttps://doi.org/10.1016/j.quascirev.2022.107761openalex-snapshot
A strong influence of the mid-Pleistocene transition on the monsoon and associated productivity in the Indian Ocean
inferred← citeshttps://doi.org/10.1016/j.quascirev.2023.108326openalex-snapshot
Eastern Arabian Sea CO2 outgassing during the last deglaciation and Holocene related to deep-water carbonate chemistry
inferred← citeshttps://doi.org/10.1016/j.quascirev.2024.109115openalex-snapshot
Substantial invasion of Antarctic Intermediate Water into the Arabian Sea during Younger Dryas and Heinrich Stadials
inferred← citeshttps://doi.org/10.1016/j.quascirev.2025.109198openalex-snapshot
Distinct response of Arabian sea upwelling and Indian summer monsoon rainfall on the millennial timescale
inferred← citeshttps://doi.org/10.1016/j.revpalbo.2006.10.005openalex-snapshot
Vegetation history and palaeoclimate of the past 30 kyr in Pakistan as inferred from the palynology of continental margin sediments off the Indus Delta
inferred← citeshttps://doi.org/10.1016/j.rsma.2021.101776openalex-snapshot
Paleoproductivity shifts since the last 130 ka off Lakshadweep, Southeastern Arabian Sea
inferred← citeshttps://doi.org/10.1016/j.yqres.2010.02.002openalex-snapshot
Climatology of the Eastern Arabian Sea during the last glacial Cycle reconstructed from paired measurement of foraminiferal δ18O and Mg/Ca
inferred← citeshttps://doi.org/10.1016/j.yqres.2011.07.001openalex-snapshot
The monsoon imprint during the ‘atypical’ MIS 13 as seen through north and equatorial Indian Ocean records
inferred← citeshttps://doi.org/10.1016/s0012-821x(04)00109-8openalex-snapshot
Variations in productivity and eolian fluxes in the northeastern Arabian Sea during the past 110 ka
inferred← citeshttps://doi.org/10.1016/s0012-821x(99)00232-0openalex-snapshot
Variations of oxygen-minimum and primary productivity recorded in sediments of the Arabian Sea
inferred← citeshttps://doi.org/10.1016/s0016-7037(01)00554-3openalex-snapshot
Early diagenesis of organic matter from sediments of the eastern subtropical Atlantic: evidence from stable nitrogen and carbon isotopes
inferred← citeshttps://doi.org/10.1016/s0016-7037(01)00817-1openalex-snapshot
Burial of redox-sensitive metals and organic matter in the equatorial Indian Ocean linked to precession
inferred← citeshttps://doi.org/10.1016/s0016-7037(02)00865-7openalex-snapshot
The influence of oxic degradation on the sedimentary biomarker record II. Evidence from Arabian Sea sediments
inferred← citeshttps://doi.org/10.1016/s0025-3227(00)00086-4openalex-snapshot
Controls on terrigenous sediment supply to the Arabian Sea during the late Quaternary: the Indus Fan
inferred← citeshttps://doi.org/10.1016/s0025-3227(00)00087-6openalex-snapshot
Controls on terrigenous sediment supply to the Arabian Sea during the late Quaternary: the Makran continental slope
inferred← citeshttps://doi.org/10.1016/s0025-3227(00)00119-5openalex-snapshot
On the formation of laminated sediments on the continental margin off Pakistan: the effects of sediment provenance and sediment redistribution
inferred← citeshttps://doi.org/10.1016/s0025-3227(02)00183-4openalex-snapshot
Sedimentary pyrite formation in the Arabian Sea
inferred← citeshttps://doi.org/10.1016/s0025-3227(02)00184-6openalex-snapshot
Synchroneity of oxygen minimum zone intensity on the Oman and Pakistan Margins at sub-Milankovitch time scales
inferred← citeshttps://doi.org/10.1016/s0025-3227(02)00268-2openalex-snapshot
Reconstruction of late Quaternary monsoon oscillations based on clay mineral proxies using sediment cores from the western margin of India
inferred← citeshttps://doi.org/10.1016/s0025-3227(03)00207-xopenalex-snapshot
A 350,000 year summer-monsoon multi-proxy stack from the Owen Ridge, Northern Arabian Sea
inferred← citeshttps://doi.org/10.1016/s0025-3227(03)00208-1openalex-snapshot
Biomass burning and oceanic primary production estimates in the Sulu Sea area over the last 380 kyr and the East Asian monsoon dynamics
inferred← citeshttps://doi.org/10.1016/s0025-3227(03)00214-7openalex-snapshot
Investigating the history of East Asian monsoon and climate during the last glacial–interglacial period (0–140 000 years): mineralogy and geochemistry of ODP Sites 1143 and 1144, South China Sea
inferred← citeshttps://doi.org/10.1016/s0031-0182(00)00074-2openalex-snapshot
Benthic foraminifera as proxies of organic matter flux and bottom water oxygenation? A case history from the northern Arabian Sea
inferred← citeshttps://doi.org/10.1016/s0031-0182(00)00156-5openalex-snapshot
Glacial to Holocene fluctuations in hydrography and productivity along the southwestern continental margin of India
inferred← citeshttps://doi.org/10.1016/s0031-0182(00)00241-8openalex-snapshot
Monsoonal variability in the northeastern Arabian Sea during the past 5000years: geochemical evidence from laminated sediments
inferred← citeshttps://doi.org/10.1016/s0031-0182(02)00599-0openalex-snapshot
Late Pleistocene–Holocene planktonic assemblages in three box-cores from the Mediterranean Ridge area (west–southwest of Crete): palaeoecological and palaeoceanographic reconstruction of sapropel S1 interval
inferred← citeshttps://doi.org/10.1016/s0031-0182(03)00385-7openalex-snapshot
Late-Quaternary biogenic productivity and organic carbon deposition in the eastern Arabian Sea
inferred← citeshttps://doi.org/10.1016/s0031-0182(03)00386-9openalex-snapshot
Primary production in the Arabian Sea during the last 135 000 years
inferred← citeshttps://doi.org/10.1016/s0031-0182(03)00387-0openalex-snapshot
Orbital insolation forcing of the Indian Monsoon – a motor for global climate changes?
inferred← citeshttps://doi.org/10.1016/s0031-0182(03)00472-3openalex-snapshot
Late Tortonian–early Messinian stepwise disruption of the Mediterranean–Atlantic connections: constraints from benthic foraminiferal and geochemical data
inferred← citeshttps://doi.org/10.1016/s0031-0182(99)00042-5openalex-snapshot
Multiple monsoon-controlled breakdown of oxygen-minimum conditions during the past 30,000 years documented in laminated sediments off Pakistan
inferred← citeshttps://doi.org/10.1016/s0277-3791(01)00139-1openalex-snapshot
Global distribution of centennial-scale records for Marine Isotope Stage (MIS) 3: a database
inferred← citeshttps://doi.org/10.1016/s0277-3791(99)00064-5openalex-snapshot
The low-latitude monsoon climate during Dansgaard–Oeschger cycles and Heinrich Events
inferred← citeshttps://doi.org/10.1016/s0304-4203(01)00037-8openalex-snapshot
Phosphorus regeneration vs. burial in sediments of the Arabian Sea
inferred← citeshttps://doi.org/10.1016/s0377-8398(00)00043-8openalex-snapshot
The influence of the NE winter monsoon on productivity changes in the Gulf of Aden, NW Arabian Sea, during the last 530ka as recorded by foraminifera
inferred← citeshttps://doi.org/10.1016/s0377-8398(03)00050-1openalex-snapshot
Late Quaternary Protoperidinium cysts as indicators of paleoproductivity in the northern Arabian Sea
inferred← citeshttps://doi.org/10.1016/s0422-9894(06)73012-4openalex-snapshot
Chapter 12 Precession and ENSO-Like Variability in the Equatorial Indo-Pacific Ocean
inferred← citeshttps://doi.org/10.1016/s0921-8181(02)00117-0openalex-snapshot
Oxygen availability effects on early diagenetic calcite dissolution in the Arabian Sea as inferred from calcareous dinoflagellate cysts
inferred← citeshttps://doi.org/10.1016/s0967-0645(00)00142-9openalex-snapshot
Mesozooplankton biomass, composition and distribution in the Arabian Sea during the Fall Intermonsoon: implications of oxygen gradients
inferred← citeshttps://doi.org/10.1017/s0016756819000098openalex-snapshot
Monsoon-induced changes in surface hydrography of the eastern Arabian Sea during the early Pleistocene
inferred← citeshttps://doi.org/10.1029/054spopenalex-snapshot
Methane Hydrates in Quaternary Climate Change: The Clathrate Gun Hypothesis
inferred← citeshttps://doi.org/10.1029/1999pa000422openalex-snapshot
Glacial‐interglacial variability in denitrification in the World's Oceans: Causes and consequences
inferred← citeshttps://doi.org/10.1029/1999pa000433openalex-snapshot
Late Quaternary insolation forcing on total organic carbon and C37 alkenone variations in the Arabian Sea
inferred← citeshttps://doi.org/10.1029/1999pa900035openalex-snapshot
Climatically linked oscillations in Arabian Sea denitrification over the past 1 m.y.: Implications for the marine N cycle
inferred← citeshttps://doi.org/10.1029/1999pa900042openalex-snapshot
Environmental control on Mediterranean salinity and δ18O
inferred← citeshttps://doi.org/10.1029/2000gb001337openalex-snapshot
Millennial‐scale oscillation of denitrification intensity in the Arabian Sea during the Late Quaternary and its potential influence on atmospheric N 2 O and global climate
inferred← citeshttps://doi.org/10.1029/2000pa000558openalex-snapshot
Nitrogen isotope evidence for water mass denitrification during the Early Toarcian (Jurassic) oceanic anoxic event
inferred← citeshttps://doi.org/10.1029/2000pa000592openalex-snapshot
Multidecadal variations in the Early Holocene outflow of Red Sea water into the Arabian Sea
inferred← citeshttps://doi.org/10.1029/2000pa000608openalex-snapshot
South Asian monsoon climate change and radiocarbon in the Arabian Sea during early and middle Holocene
inferred← citeshttps://doi.org/10.1029/2000pa000616openalex-snapshot
Sedimentary phosphorus record from the Oman margin: New evidence of high productivity during glacial periods
inferred← citeshttps://doi.org/10.1029/2000pa000621openalex-snapshot
Oxygen minimum zone controlled Mn redistribution in Arabian Sea sediments during the late Quaternary
inferred← citeshttps://doi.org/10.1029/2003pa000900openalex-snapshot
Hyperstratification following glacial overturning events in the northern Arabian Sea
inferred← citeshttps://doi.org/10.1029/2004pa001017openalex-snapshot
Comment on “Sedimentary phosphorus record from the Oman margin: New evidence of high productivity during glacial periods” by F. Tamburini et al.
inferred← citeshttps://doi.org/10.1029/2004pa001031openalex-snapshot
A solar (irradiance) trigger for millennial‐scale abrupt changes in the southwest monsoon?
inferred← citeshttps://doi.org/10.1029/2004pa001044openalex-snapshot
Oxygenation changes in the deep western Arabian Sea during the last 190,000 years: Productivity versus deepwater circulation
inferred← citeshttps://doi.org/10.1029/2004pa001078openalex-snapshot
Seasonal sea surface temperature contrast between the Holocene and last glacial period in the western Arabian Sea (Ocean Drilling Project Site 723A): Modulated by monsoon upwelling
inferred← citeshttps://doi.org/10.1029/2005gc001095openalex-snapshot
Is there a persistent control of monsoon winds by precipitation during the late Holocene?
inferred← citeshttps://doi.org/10.1029/2005pa001161openalex-snapshot
Tropical Pacific climate response to obliquity forcing in the Pleistocene
inferred← citeshttps://doi.org/10.1029/2005pa001162openalex-snapshot
Sea surface temperature pattern reconstructions in the Arabian Sea
inferred← citeshttps://doi.org/10.1029/2006gb002718openalex-snapshot
Potential impact of changes in river nutrient supply on global ocean biogeochemistry
inferred← citeshttps://doi.org/10.1029/2006gb002852openalex-snapshot
Evidence of ventilation changes in the Arabian Sea during the late Quaternary: Implication for denitrification and nitrous oxide emission
inferred← citeshttps://doi.org/10.1029/2006pa001284openalex-snapshot
Multispecies stable isotopes of benthic foraminifers reveal past changes of organic matter decomposition and deepwater oxygenation in the Arabian Sea
inferred← citeshttps://doi.org/10.1029/2006pa001292openalex-snapshot
Sea surface temperatures of the western Arabian Sea during the last deglaciation
inferred← citeshttps://doi.org/10.1029/2006pa001355openalex-snapshot
Nitrate reduction, sulfate reduction, and sedimentary iron isotope evolution during the Cenomanian‐Turonian oceanic anoxic event
inferred← citeshttps://doi.org/10.1029/2006pa001384openalex-snapshot
Large fluctuations of dissolved oxygen in the Indian and Pacific oceans during Dansgaard‐Oeschger oscillations caused by variations of North Atlantic Deep Water subduction
inferred← citeshttps://doi.org/10.1029/2007gc001932openalex-snapshot
Bromine counts from XRF scanning as an estimate of the marine organic carbon content of sediment cores
inferred← citeshttps://doi.org/10.1029/2007pa001502openalex-snapshot
A 28‐ka history of sea surface temperature, primary productivity and planktonic community variability in the western Arabian Sea
inferred← citeshttps://doi.org/10.1029/2007pa001546openalex-snapshot
Benthic foraminiferal faunal and isotopic changes as recorded in Holocene sediments of the northwest Indian Ocean
inferred← citeshttps://doi.org/10.1029/2008pa001638openalex-snapshot
Southern Hemisphere forcing of Pliocene δ18O and the evolution of Indo‐Asian monsoons
inferred← citeshttps://doi.org/10.1029/2008pa001687openalex-snapshot
Evaporation-precipitation changes in the eastern Arabian Sea for the last 68 ka: Implications on monsoon variability
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