On the public citation graph

A 300 KYR Record of Upwelling Off Oman during the Late Quaternary: Evidence of the Asian Southwest Monsoon

0 signed · 250 inferred · view as graph

Inferred edges come from two machine sources: sweeps of open repository metadata (mostly SSRN and Zenodo), and a bulk OpenAlex citation snapshot. Every row below is labelled with the one it came from. Neither is a complete citation index — absence here is not evidence of absence.

Is this your work? Sign in with ORCID and put your name on the claims that are yours.

Claim with ORCID

Reference health. See whether every reference in this work resolves to a known work and none has been retracted — and get a dated CiteStamped badge you can embed.

See reference health

What this work says

Outgoing claims: the papers this work cites, builds on, or argues with.

inferredcites →https://doi.org/10.1016/0012-8252(72)90038-4openalex-snapshot

Late Cenozoic Glacial Ages

inferredcites →https://doi.org/10.1016/0016-7037(89)90123-3openalex-snapshot

The role of ocean-atmosphere reorganizations in glacial cycles

inferredcites →https://doi.org/10.1016/0031-0182(92)90216-ropenalex-snapshot

On the nature of the ice cap on the Tibetan Plateau during the late Quaternary

inferredcites →https://doi.org/10.1016/0198-0149(84)90032-3openalex-snapshot

Some aspects of the physical oceanography of the Indian Ocean

inferredcites →https://doi.org/10.1016/0377-8398(84)90022-7openalex-snapshot

Planktonic foraminifera of the northern Indian Ocean: Distribution and preservation in surface sediments

inferredcites →https://doi.org/10.1016/0921-8181(92)90004-topenalex-snapshot

On the nature of the ice cap on the Tibetan Plateau during the late Quaternary

inferredcites →https://doi.org/10.1029/90pa02497openalex-snapshot

A high‐resolution Late Quaternary upwelling record from the anoxic Cariaco Basin, Venezuela

inferredcites →https://doi.org/10.1029/91jc02225openalex-snapshot

Interannual variability in phytoplankton blooms observed in the northwestern Arabian Sea during the southwest monsoon

inferredcites →https://doi.org/10.1029/92jc01428openalex-snapshot

The structure of the southwest monsoon winds over the Arabian Sea during the late Quaternary: Observations, simulations, and marine geologic evidence

inferredcites →https://doi.org/10.1029/92pa01267openalex-snapshot

Southwest Monsoon Circulation and Environments of Recent Planktonic Foraminifera in the Northwestern Arabian Sea

inferredcites →https://doi.org/10.1029/gm029p0048openalex-snapshot

Variation of monsoonal upwelling: A response to changing solar radiation

inferredcites →https://doi.org/10.1029/jc082i027p03889openalex-snapshot

Simulation of the tropical climate of an ice age

inferredcites →https://doi.org/10.1029/jd092id07p08411openalex-snapshot

Monsoon variability over the past 150,000 years

inferredcites →https://doi.org/10.1029/jd093id07p08283openalex-snapshot

Climate simulations for 9000 years before present: Seasonal variations and effect of the Laurentide ice sheet

inferredcites →https://doi.org/10.1029/pa005i002p00109openalex-snapshot

Late Pleistocene variability of Arabian Sea summer monsoon winds and continental aridity: Eolian records from the lithogenic component of deep‐sea sediments

inferredcites →https://doi.org/10.1038/295494a0openalex-snapshot

Glacial to interglacial contrasts in the northern Indian Ocean

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/10.1038/317130a0openalex-snapshot

Milankovitch forcing of fluctuations in the level of tropical lakes from 18 to 0 kyr BP

inferredcites →https://doi.org/10.1038/323526a0openalex-snapshot

Coherent response of Arabian Sea upwelling and pollen transport to late Quaternary monsoonal winds

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.1992.064.01.08openalex-snapshot

Physical upwelling processes, upper ocean environment and the sediment record of the southwest monsoon

inferredcites →https://doi.org/10.1175/1520-0469(1982)039<1177:tsotaa>2.0.co;2openalex-snapshot

The Sensitivity of the African-Asian Monsoonal Climate to Orbital Parameter Changes for 9000 Years B.P. in a Low-Resolution General Circulation Model

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

inferredcites →https://doi.org/10.1175/1520-0469(1989)046<0661:teoesc>2.0.co;2openalex-snapshot

The Effect of Eurasian Snow Cover on Regional and Global Climate Variations

inferredcites →https://doi.org/10.2307/1485406openalex-snapshot

Ecology of Planktonic Foraminifera and Biogeographic Patterns of Life and Fossil Assemblages in the Indian Ocean

inferredcites →https://doi.org/10.2307/2286100openalex-snapshot

Spectral Analysis and its Applications.

inferredcites →https://doi.org/10.2973/odp.proc.sr.117.168.1991openalex-snapshot

Oxygen and Carbon Isotope Stratigraphy at Site 723, Oman Margin

inferredcites →https://doi.org/10.2973/odp.proc.sr.118.1991openalex-snapshot

Proceedings of the Ocean Drilling Program, 118 Scientific Results

What points at this work

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

inferred← citeshttps://doi.org/10.2139/ssrn.4705842openalex-extracted

Asian Winter Monsoon Controlling Productivity Variations in North Arabian Sea During the Holocene

inferred← citeshttps://doi.org/10.1002/2013pa002603openalex-snapshot

Red Sea circulation during marine isotope stage 5e

inferred← citeshttps://doi.org/10.1002/2015jc010982openalex-snapshot

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

inferred← citeshttps://doi.org/10.1002/jqs.1369openalex-snapshot

Indian summer monsoon during the last two millennia

inferred← citeshttps://doi.org/10.1002/lom3.10637openalex-snapshot

Size normalizing planktonic Foraminifera abundance in the water column

inferred← citeshttps://doi.org/10.1006/qres.1995.1041openalex-snapshot

Sea-Surface Temperatures and the History of Monsoon Upwelling in the Northwest Arabian Sea during the Last 500,000 Years

inferred← citeshttps://doi.org/10.1006/qres.1998.1958openalex-snapshot

Comparison of Late Pleistocene and Modern Glacier Extents in Central Nepal Based on Digital Elevation Data and Satellite Imagery

inferred← citeshttps://doi.org/10.1006/qres.1999.2083openalex-snapshot

Planktonic Foraminiferal and Alkenone Records of the Last Deglaciation from the Eastern Arabian Sea

inferred← citeshttps://doi.org/10.1006/qres.2001.2231openalex-snapshot

Late Quaternary Upwelling Intensity and East Asian Monsoon Forcing in the South China Sea

inferred← citeshttps://doi.org/10.1007/978-1-4615-4197-4_15openalex-snapshot

Primary Production Response to Orbitally Induced Variations of the Southern Oscillation in the Equatorial Indian Ocean

inferred← citeshttps://doi.org/10.1007/978-3-030-15989-4_14openalex-snapshot

Evolution and Development of the Indian Monsoon

inferred← citeshttps://doi.org/10.1007/978-3-319-73597-9_1openalex-snapshot

Introduction

inferred← citeshttps://doi.org/10.1007/978-3-642-28845-6_8openalex-snapshot

High Resolution Southwest Monsoon Reconstruction for the Past ~2,800 Years: Wind Versus Precipitation

inferred← citeshttps://doi.org/10.1007/978-3-642-58646-0_12openalex-snapshot

Organic Carbon and Carbonate as Paleoproductivity Proxies: Examples from High and Low Productivity Areas of the Tropical Atlantic

inferred← citeshttps://doi.org/10.1007/978-3-642-79268-7_2openalex-snapshot

Fluctuations of the Indian Monsoon Regime During the Last 170,000 Years: Evidence from Sea Surface Temperature, Salinity and Organic Carbon Records

inferred← citeshttps://doi.org/10.1007/978-3-642-80353-6_27openalex-snapshot

Late Quaternary Surface Temperatures and Productivity in the East-Equatorial South Atlantic: Response to Changes in Trade/Monsoon Wind Forcing and Surface Water Advection

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/bf00211619openalex-snapshot

The southwest Indian Monsoon over the last 18 000 years

inferred← citeshttps://doi.org/10.1007/s00367-018-0538-6openalex-snapshot

Variability of terrigenous input to the Bay of Bengal for the last ~80 kyr: Implications on the Indian monsoon variability

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/s00367-022-00733-yopenalex-snapshot

Surface hydrographic variations in the western Arabian Sea through the last 172 kyr

inferred← citeshttps://doi.org/10.1007/s11434-009-0540-5openalex-snapshot

Effect of precession on the Asian summer monsoon evolution: A systematic review

inferred← citeshttps://doi.org/10.1007/s11629-007-0091-7openalex-snapshot

Critical approach to methods of glacier reconstruction in high Asia and discussion of the probability of a Qinghai-Xizang (Tibetan) inland ice

inferred← citeshttps://doi.org/10.1007/s12038-009-0066-7openalex-snapshot

Deep-sea palaeoceanography of the Maldives Islands (ODP Hole 716A), equatorial Indian Ocean during MIS 12-6

inferred← citeshttps://doi.org/10.1007/s12040-011-0011-7openalex-snapshot

Late Quaternary changes in surface productivity and oxygen minimum zone (OMZ) in the northwestern Arabian Sea: Micropaleontologic and sedimentary record at ODP site 728A

inferred← citeshttps://doi.org/10.1007/s12040-021-01659-2openalex-snapshot

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/s12517-021-08652-5openalex-snapshot

Calcareous peloids in the north-western Arabian Sea: implications of late Quaternary marine sedimentation and paleoclimate

inferred← citeshttps://doi.org/10.1007/s12517-023-11728-zopenalex-snapshot

Dense mineral distribution in the northwestern Arabian Sea: insights into sediment provenance and paleoclimate

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/s12594-011-0014-7openalex-snapshot

Relationship between Abundance and Morphology of Benthic Foraminifera Epistominella exigua: Paleoclimatic Implications

inferred← citeshttps://doi.org/10.1007/s12594-023-2482-yopenalex-snapshot

Paleoclimatic Influence on the Evolution of the Late Quaternary Clastic Sediments, Northwestern Arabian Sea

inferred← citeshttps://doi.org/10.1016/0377-8398(95)00014-3openalex-snapshot

Do benthic foraminifer records represent a productivity index in oxygen minimum zone areas? An evaluation from the Oman Margin, Arabian Sea

inferred← citeshttps://doi.org/10.1016/0377-8398(95)00070-4openalex-snapshot

Fertility tracers and monsoon forcing at an equatorial site of the Somali Basin (Northwest Indian Ocean)

inferred← citeshttps://doi.org/10.1016/b0-08-043751-6/06118-1openalex-snapshot

The Biological Pump in the Past

inferred← citeshttps://doi.org/10.1016/b978-0-08-095975-7.00618-5openalex-snapshot

The Biological Pump in the Past

inferred← citeshttps://doi.org/10.1016/j.apgeochem.2021.105088openalex-snapshot

Texture, mineralogy and geochemistry of late Quaternary sediments of the Mahi River basin, western India: Implications to climate and tectonics

inferred← citeshttps://doi.org/10.1016/j.dsr2.2005.05.003openalex-snapshot

Carbonate and carbon fluctuations in the Eastern Arabian Sea over 140ka: Implications on productivity changes?

inferred← citeshttps://doi.org/10.1016/j.dsr2.2025.105518openalex-snapshot

A large glacial-interglacial shift in carbon burial in the northeast Indian Ocean during the Late Quaternary

inferred← citeshttps://doi.org/10.1016/j.epsl.2004.06.008openalex-snapshot

Understanding the Red Sea response to sea level

inferred← citeshttps://doi.org/10.1016/j.epsl.2007.05.004openalex-snapshot

A high-resolution, absolute-dated deglacial speleothem record of Indian Ocean climate from Socotra Island, Yemen

inferred← citeshttps://doi.org/10.1016/j.epsl.2008.09.022openalex-snapshot

A 90 kyr upwelling record from the northwestern Indian Ocean using a novel long-chain diol index

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.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.gloplacha.2003.09.002openalex-snapshot

Isotopic evidences of past upwelling intensity in the Arabian Sea

inferred← citeshttps://doi.org/10.1016/j.gloplacha.2009.12.008openalex-snapshot

Controlling weathering and erosion intensity on the southern slope of the Central Himalaya by the Indian summer monsoon during the last glacial

inferred← citeshttps://doi.org/10.1016/j.gloplacha.2015.03.004openalex-snapshot

The middle Holocene climatic records from Arabia: Reassessing lacustrine environments, shift of ITCZ in Arabian Sea, and impacts of the southwest Indian and African monsoons

inferred← citeshttps://doi.org/10.1016/j.gloplacha.2017.09.006openalex-snapshot

Offshore expansion of the Brazilian coastal upwelling zones during Marine Isotope Stage 5

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.2025.104734openalex-snapshot

Changes in surface conditions and associated hypoxia since the late Marine Isotope Stage 3, eastern Arabian Sea

inferred← citeshttps://doi.org/10.1016/j.gr.2024.06.008openalex-snapshot

C, N, Hg isotopes and elemental chemostratigraphy across the Ordovician–Silurian transition in the Argentine Precordillera: Implications for the link between volcanism and extinctions

inferred← citeshttps://doi.org/10.1016/j.gsf.2022.101432openalex-snapshot

Paleo-glacial reconstruction of the Thajwas glacier in the Kashmir Himalaya using 10Be cosmogenic radionuclide dating

inferred← citeshttps://doi.org/10.1016/j.jop.2017.08.005openalex-snapshot

Distributional patterns of anemophilous tree pollen indicating the pathways of Indian monsoon through Qinghai–Tibetan Plateau

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.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.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.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.marmicro.2004.01.005openalex-snapshot

Atypical δ13C signature in Globigerina bulloides at the ODP site 723A (Arabian Sea): implications of environmental changes caused by upwelling

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.2014.01.004openalex-snapshot

Boron/calcium ratios in Globigerinoides ruber from the Arabian Sea: Implications for controls on boron incorporation

inferred← citeshttps://doi.org/10.1016/j.marmicro.2017.10.006openalex-snapshot

Genetic diversity and ecology of the planktonic foraminifers Globigerina bulloides , Turborotalita quinqueloba and Neogloboquadrina pachyderma off the Oman margin during the late SW Monsoon

inferred← citeshttps://doi.org/10.1016/j.palaeo.2005.04.007openalex-snapshot

Monitoring the variations of the Socotra upwelling system during the last 250 kyr: A biogenic and geochemical approach

inferred← citeshttps://doi.org/10.1016/j.palaeo.2006.05.015openalex-snapshot

Calcretes from a Late Quaternary interfluve in the Ganga Plains, India: Carbonate types and isotopic systems in a monsoonal setting

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.2010.01.013openalex-snapshot

The variation of the southwest monsoon from the high resolution pollen record in Heqing Basin, Yunnan Province, China for the last 2.78Ma

inferred← citeshttps://doi.org/10.1016/j.palaeo.2014.07.006openalex-snapshot

Monsoonal dynamics and evolution of the primary productivity in the eastern Arabian Sea over the past 30ka

inferred← citeshttps://doi.org/10.1016/j.palaeo.2015.08.006openalex-snapshot

Evolution of the South Asian monsoon wind system since the late Middle Miocene

inferred← citeshttps://doi.org/10.1016/j.palaeo.2017.11.051openalex-snapshot

Variation in monsoonal rainfall sources (Arabian Sea and Bay of Bengal) during the late Quaternary: Implications for regional vegetation and fluvial systems

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.2022.110865openalex-snapshot

A ~ 30 kyr sub-centennial to millennial Indian summer monsoon variability record from the southern Andaman Sea, northeastern Indian Ocean

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.2025.113460openalex-snapshot

Inter-hemispheric climate linkages and monsoonal controls on the Arabian Sea surface temperatures

inferred← citeshttps://doi.org/10.1016/j.pnsc.2007.09.004openalex-snapshot

Late Neogene radiolarian absence event in the southern South China Sea and its paleoceanographic implication

inferred← citeshttps://doi.org/10.1016/j.quaint.2006.02.012openalex-snapshot

Review of the timing and extent of glaciers during the last glacial cycle in the bordering mountains of Tibet and in East Asia

inferred← citeshttps://doi.org/10.1016/j.quaint.2006.10.031openalex-snapshot

Stable isotopic composition of pedogenic carbonates from the eastern margin of the Thar Desert, Rajasthan, India

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.2014.12.014openalex-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.2015.05.068openalex-snapshot

Potential influence of temperature changes in the Southern Hemisphere on the evolution of the Asian summer monsoon during the last glacial period

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.2020.09.053openalex-snapshot

Hydro-climatic variability during last five thousand years and its impact on human colonization and cultural transition in Ladakh sector, India

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.2021.04.015openalex-snapshot

Strong solar influence on multi-decadal periodic productivity changes in the central-western Bay of Bengal

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.2025.109713openalex-snapshot

Last 15 ka record of water column changes associated with Indian summer monsoon variability from the northeastern Bay of Bengal

inferred← citeshttps://doi.org/10.1016/j.quaint.2025.109894openalex-snapshot

Late Quaternary productivity and hydrographic variability in the upper water column of the Agulhas Return Current region as inferred from planktic foraminifera

inferred← citeshttps://doi.org/10.1016/j.quaint.2025.110106openalex-snapshot

Foraminiferal and geochemical evidence of the late Quaternary monsoon and oceanographic shifts in the southern Bay of Bengal

inferred← citeshttps://doi.org/10.1016/j.quaint.2026.110156openalex-snapshot

Calcareous non-skeletal grains from northwestern Arabian Sea: insights into late Quaternary paleoclimate

inferred← citeshttps://doi.org/10.1016/j.quascirev.2003.06.021openalex-snapshot

Palaeo-climate reconstruction from stable isotope variations in speleothems: a review

inferred← citeshttps://doi.org/10.1016/j.quascirev.2004.07.020openalex-snapshot

Sea-surface temperatures around the Australian margin and Indian Ocean during the Last Glacial Maximum

inferred← citeshttps://doi.org/10.1016/j.quascirev.2004.08.009openalex-snapshot

Synchronous Holocene sea surface temperature and rainfall variations in the Asian monsoon system

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.2011.10.004openalex-snapshot

Variations of Indian monsoon precipitation during the last 32kyr reflected in the surface hydrography of the Western Bay of Bengal

inferred← citeshttps://doi.org/10.1016/j.quascirev.2013.12.006openalex-snapshot

Modelling stable water isotopes in monsoon precipitation during the previous interglacial

inferred← citeshttps://doi.org/10.1016/j.quascirev.2015.02.002openalex-snapshot

A ∼50 ka record of monsoonal variability in the Darjeeling foothill region, eastern Himalayas

inferred← citeshttps://doi.org/10.1016/j.quascirev.2017.07.017openalex-snapshot

Rapid and punctuated Late Holocene recession of Siling Co, central Tibet

inferred← citeshttps://doi.org/10.1016/j.quascirev.2018.05.021openalex-snapshot

Relative influence of precession and obliquity in the early Holocene: Topographic modulation of subtropical seasonality during the Asian summer monsoon

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.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.quascirev.2025.109328openalex-snapshot

Mineral dust as a forcing factor behind primary productivity in the northwestern Arabian Sea since the Last Glacial Maximum

inferred← citeshttps://doi.org/10.1016/j.quascirev.2026.110205openalex-snapshot

Multiproxy evidence for reduced productivity and enhanced carbonate preservation during MIS 2 in the Bay of Bengal

inferred← citeshttps://doi.org/10.1016/j.rsma.2018.09.011openalex-snapshot

Temporal phytoplankton diversity patterns and community structure in a monsoonal region, Oman Seawater (Iranian parts)

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.2009.03.007openalex-snapshot

Spatial patterns of Holocene glacier advance and retreat in Central Asia

inferred← citeshttps://doi.org/10.1016/j.yqres.2009.07.003openalex-snapshot

Ecological variations in diatom assemblages in the Paleo-Kathmandu Lake linked with global and Indian monsoon climate changes for the last 600,000 years

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/s0012-821x(04)00095-0openalex-snapshot

Stepwise Holocene aridification in NE Africa deduced from dust-borne radiogenic isotope records

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(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)00215-9openalex-snapshot

Development of east Asian summer monsoon environments in the late Miocene: radiolarian evidence from Site 1143 of ODP Leg 184

inferred← citeshttps://doi.org/10.1016/s0025-3227(98)00163-7openalex-snapshot

Pelagic productivity changes in the equatorial area of the northwest Indian Ocean during the last 400,000 years

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(03)00267-0openalex-snapshot

Productivity fluctuations in the southeastern Arabian Sea during the last 140 ka

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)00389-4openalex-snapshot

500 000-Year records of carbonate, organic carbon, and foraminiferal sea-surface temperature from the southeastern South China Sea (near Palawan Island)

inferred← citeshttps://doi.org/10.1016/s0033-5894(03)00086-3openalex-snapshot

Changing moisture sources over the last 330,000 years in Northern Oman from fluid-inclusion evidence in speleothems

inferred← citeshttps://doi.org/10.1016/s0277-3791(01)00133-0openalex-snapshot

Event stratigraphy, paleoenvironment and chronology of SE Arabian deserts

inferred← citeshttps://doi.org/10.1016/s0277-3791(96)00049-2openalex-snapshot

Mechanisms forcing abrupt fluctuations of the indian ocean summer monsoon during the last deglaciation

inferred← citeshttps://doi.org/10.1016/s0377-8398(00)00042-6openalex-snapshot

Aplanktonic zones in the Red 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(98)00015-2openalex-snapshot

Benthic foraminiferal response to variations in surface water productivity and oxygenation in the northern Arabian Sea

inferred← citeshttps://doi.org/10.1016/s0377-8398(98)00026-7openalex-snapshot

A size analysis of planktic foraminifera from the 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)00120-0openalex-snapshot

The effect of upwelling on the distribution and stable isotope composition of Globigerina bulloides and Globigerinoides ruber (planktic foraminifera) in modern surface waters of the NW Arabian Sea

inferred← citeshttps://doi.org/10.1016/s0967-0645(97)00008-8openalex-snapshot

Sea surface temperature and productivity records for the past 240 kyr in the Arabian Sea

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/10.1029/1999pa000433openalex-snapshot

Late Quaternary insolation forcing on total organic carbon and C37 alkenone variations in the Arabian Sea

inferred← citeshttps://doi.org/10.1029/2001gl013315openalex-snapshot

Earth's eccentricity cycles and Indian Summer Monsoon variability over the past 2 million years: Evidence from deep‐sea benthic foraminifer

inferred← citeshttps://doi.org/10.1029/2002gc000348openalex-snapshot

Decadal‐centennial scale monsoon variations in the Arabian Sea during the Early Holocene

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/10.1029/2005gl022685openalex-snapshot

Solar influence on the Indian summer monsoon during the Holocene

inferred← citeshttps://doi.org/10.1029/2006pa001292openalex-snapshot

Sea surface temperatures of the western Arabian Sea during the last deglaciation

inferred← citeshttps://doi.org/10.1029/2007pa001431openalex-snapshot

Red Sea during the Last Glacial Maximum: Implications for sea level reconstruction

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/10.1029/2007pa001564openalex-snapshot

Coupled sea surface temperature–seawater δ18O reconstructions in the Arabian Sea at the millennial scale for the last 35 ka

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

inferred← citeshttps://doi.org/10.1029/2009gl042225openalex-snapshot

Mid‐Brunhes strengthening of the Indian Ocean Dipole caused increased equatorial East African and decreased Australasian rainfall

inferred← citeshttps://doi.org/10.1029/2009pa001923openalex-snapshot

Productivity collapses in the Arabian Sea during glacial cold phases

inferred← citeshttps://doi.org/10.1029/2021pa004278openalex-snapshot

Evidence of a South Asian Proto‐Monsoon During the Oligocene‐Miocene Transition

inferred← citeshttps://doi.org/10.1029/2022pa004453openalex-snapshot

Variations of Primary Productivity in the Northwestern Arabian Sea During the Last 23,000 Years and Their Paleoclimatological Implications

inferred← citeshttps://doi.org/10.1029/2022pa004530openalex-snapshot

Hydroclimate Variability in the Equatorial Western Indian Ocean for the Last 250,000 Years

inferred← citeshttps://doi.org/10.1029/2023pa004813openalex-snapshot

Decoupling Warming and Monsoon Precipitation Over the Last 3110 Years in Northwestern Yunnan Province, Southwestern China

inferred← citeshttps://doi.org/10.1029/94pa00443openalex-snapshot

Milankovitch band forcing of sub‐Milankovitch climate variability during the Pleistocene

inferred← citeshttps://doi.org/10.1029/94pa01648openalex-snapshot

Glacial conditions in the Red Sea

inferred← citeshttps://doi.org/10.1029/94pa02514openalex-snapshot

Impact of productivity events on the benthic foraminiferal fauna in the Arabian Sea over the last 150,000 years

inferred← citeshttps://doi.org/10.1029/94pa02682openalex-snapshot

Monsoon upwelling effects on test size of some planktonic foraminiferal species from the Oman Margin, Arabian Sea

inferred← citeshttps://doi.org/10.1029/95gl02558openalex-snapshot

A 2,200 years periodicity in the Asian Monsoon System

inferred← citeshttps://doi.org/10.1029/95pa00420openalex-snapshot

Paleohydrographic changes in the Somali Basin (5°N upwelling and equatorial areas) during the last 160 Kyr, based on correspondence analysis of foraminiferal and radiolarian assemblages

inferred← citeshttps://doi.org/10.1029/95pa03198openalex-snapshot

A High‐resolution record of Late Quaternary upwelling along the Oman Margin, Arabian Sea based on planktonic foraminifera

inferred← citeshttps://doi.org/10.1029/95rg01035openalex-snapshot

Paleoclimatology and climate system dynamics

inferred← citeshttps://doi.org/10.1029/97pa00213openalex-snapshot

Role of orbital forcing in east Asian monsoon climates during the last 350 kyr: Evidence from terrestrial and marine climate proxies from core RC14‐99

inferred← citeshttps://doi.org/10.1029/97pa02892openalex-snapshot

A 400 kyr record of combustion oxygen demand in the western equatorial Pacific: Evidence for a precessionally forced climate response

inferred← citeshttps://doi.org/10.1029/98pa02203openalex-snapshot

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

inferred← citeshttps://doi.org/10.1029/gm070p0447openalex-snapshot

Evolution and Variability of the Indian Ocean Summer Monsoon: Evidence from the Western Arabian Sea Drilling Program

inferred← citeshttps://doi.org/10.1038/373506a0openalex-snapshot

Climate-related variations in denitrification in the Arabian Sea from sediment 15N/14N ratios

inferred← citeshttps://doi.org/10.1038/nature01340openalex-snapshot

Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean

inferred← citeshttps://doi.org/10.1063/1.5008698openalex-snapshot

Study of spectro-temporal variation in paleo-climatic marine proxy records using wavelet transformations

inferred← citeshttps://doi.org/10.1088/2515-7620/ae165fopenalex-snapshot

A persistent change in south Asian monsoon seasonality during the last 580 kyr

inferred← citeshttps://doi.org/10.1093/oxfordhb/9780197607770.013.36openalex-snapshot

The Archaeology of the Iberian Atlantic Façade

inferred← citeshttps://doi.org/10.1109/isacv.2015.7106195openalex-snapshot

Detection of Moroccan coastal upwelling in SST images using the Expectation-Maximization

inferred← citeshttps://doi.org/10.1111/j.1365-3091.2004.00678.xopenalex-snapshot

Eustatic and climatic controls on the development of the Wahiba Sand Sea, Sultanate of Oman

inferred← citeshttps://doi.org/10.1111/j.1502-3885.2009.00118.xopenalex-snapshot

Late Quaternary glaciation in the Tianshan and implications for palaeoclimatic change: a review

inferred← citeshttps://doi.org/10.1111/j.1755-6724.2011.00498.xopenalex-snapshot

Paired Measurements of Foraminiferal δ18O and Mg/Ca Ratios of Indian Monsoons Reconstructed from Holocene to Last Glacial Record

inferred← citeshttps://doi.org/10.1126/science.1072881openalex-snapshot

Increase in the Asian Southwest Monsoon During the Past Four Centuries

inferred← citeshttps://doi.org/10.1126/science.274.5289.943openalex-snapshot

Nonstationary Phase of the Plio-Pleistocene Asian Monsoon

inferred← citeshttps://doi.org/10.1130/0091-7613(2001)029<0623:sefofc>2.0.co;2openalex-snapshot

Speleothem evidence from Oman for continental pluvial events during interglacial periods

inferred← citeshttps://doi.org/10.1130/b25554.1openalex-snapshot

Late Pleistocene eolian history of the Liwa region, Arabian Peninsula

inferred← citeshttps://doi.org/10.1144/gsjgs.155.2.0353openalex-snapshot

The role of the Indian summer monsoon and the mid-latitude westerlies in Himalayan glaciation: review and speculative discussion

inferred← citeshttps://doi.org/10.1144/gsl.sp.1996.116.01.16openalex-snapshot

Laminated sediments from the oxygen-minimum zone of the northeastern Arabian Sea

inferred← citeshttps://doi.org/10.1144/gsl.sp.2002.195.01.16openalex-snapshot

Quaternary climatic changes over Southern Arabia and the Thar Desert, India

inferred← citeshttps://doi.org/10.1144/gsl.sp.2002.195.01.18openalex-snapshot

Centennial-millennial-scale monsoon variations off Somalia over the last 35 ka

inferred← citeshttps://doi.org/10.1144/gsl.sp.2002.195.01.26openalex-snapshot

The seasonal and vertical distribution of living planktic foraminifera in the NW Arabian Sea

inferred← citeshttps://doi.org/10.1144/gsl.sp.2005.247.01.04openalex-snapshot

Response of tropical African and East Atlantic climates to orbital forcing over the last 1.7 Ma

inferred← citeshttps://doi.org/10.1144/sp342.11openalex-snapshot

Evolution of the Indian summer monsoon: synthesis of continental records

inferred← citeshttps://doi.org/10.1155/2012/574851openalex-snapshot

The Impact of the Geologic History and Paleoclimate on the Diversification of East African Cichlids

inferred← citeshttps://doi.org/10.1155/2014/621479openalex-snapshot

The Interdependency of the Morphological Variations of the Planktonic Foraminiferal SpeciesGlobigerina bulloidesin Surface Sediments on the Environmental Parameters of the Southwestern Indian Ocean

inferred← citeshttps://doi.org/10.1177/05529360251407471openalex-snapshot

History of monsoon-induced upwelling and associated productivity based on planktic foraminiferal assemblage since the Last Glacial Maximum in the eastern Arabian Sea

inferred← citeshttps://doi.org/10.1177/0959683617744267openalex-snapshot

Timing of the Indian Summer Monsoon onset during the early Holocene: Evidence from a sediment core at Linggo Co, central Tibetan Plateau

inferred← citeshttps://doi.org/10.1186/2193-1801-2-282openalex-snapshot

Distribution patterns of toxic metals in the marine oyster Saccostrea cucullata from the Arabian Sea in Oman: spatial, temporal, and size variations

inferred← citeshttps://doi.org/10.1186/s40645-022-00489-0openalex-snapshot

The response of the hydrological cycle to temperature changes in recent and distant climatic history

inferred← citeshttps://doi.org/10.1201/9780203748978-3openalex-snapshot

Sensitivity of Subtropical African and Asian Climate to Prescribed Boundary Condition Changes: Model Implications for the Plio-Pleistocene Evolution of Low-Latitude Climate

inferred← citeshttps://doi.org/10.13000/jfmse.2026.6.38.3.648openalex-snapshot

Evaluation of Wake and Upwelling Regions of Artificial Reef Sets Composed of Cube-type Reefs

inferred← citeshttps://doi.org/10.1360/csb2009-54-20-3097openalex-snapshot

岁差对亚洲夏季风气候变化影响研究进展

inferred← citeshttps://doi.org/10.15344/2456-351x/2017/142openalex-snapshot

Preliminary Study of Global Warming Mitigation by Grazing OTEC

inferred← citeshttps://doi.org/10.1594/pangaea.51874openalex-snapshot

Susceptibility raw data from ODP Hole 117-723B in the Arabian Sea

inferred← citeshttps://doi.org/10.1594/pangaea.52590openalex-snapshot

(Table 1) Age model of ODP Site 117-723 in the Arabian Sea

inferred← citeshttps://doi.org/10.17491/jgsi/2006/680306openalex-snapshot

Millennial Scale Variations in Productivity and OMZ Intensity in the Eastern Arabian Sea

inferred← citeshttps://doi.org/10.17491/jgsi/2025/174117openalex-snapshot

A Late Quaternary Foraminiferal Record of Deep-Water Ventilation Changes below OMZ in the Northwest Arabian Sea

inferred← citeshttps://doi.org/10.18520/cs/v119/i2/282-290openalex-snapshot

Evolution and Dynamics of the Denitrification in the Arabian Sea on Millennial to Million-Year Timescale

inferred← citeshttps://doi.org/10.2113/gsjfr.40.3.220openalex-snapshot

DECIPHERING THE MODERN CALCIFICATION DEPTH OF GLOBIGERINA BULLOIDES IN THE SOUTHWESTERN INDIAN OCEAN FROM ITS OXYGEN ISOTOPIC COMPOSITION

inferred← citeshttps://doi.org/10.2139/ssrn.6105798openalex-snapshot

Sensitivity of Sedimentation Processes to Climate Variability in the Western Indian Ocean over the Last 100 kyr

inferred← citeshttps://doi.org/10.2151/jmsj.85.1openalex-snapshot

A Coupled Model Study of Glacial Asian Monsoon Variability and Indian Ocean Dipole

inferred← citeshttps://doi.org/10.21608/ejabf.2018.8183openalex-snapshot

State of Seasonal Environmental Factors of the Hadhramout Coast, Gulf of Aden, Yemen

inferred← citeshttps://doi.org/10.22541/au.171036278.84062706/v1openalex-snapshot

Size normalizing planktonic Foraminifera abundance in the water column

inferred← citeshttps://doi.org/10.2312/polarforschung.71.1-2.1openalex-snapshot

The Tibetan Ice Sheet, Its Impact on the Palaeomonsoon and Relation to the Earth´s Orbital Variations

inferred← citeshttps://doi.org/10.3233/jcc-160021openalex-snapshot

Significance of Globigerina Bulloides D’orbigny: A Foraminiferal Proxy for Palaeomonsoon and Past Upwelling Records

inferred← citeshttps://doi.org/10.3354/cr020001openalex-snapshot

A relief-specific model of the ice age on the basis of uplift-controlled glacier areas in Tibet and the corresponding albedo increase as well as their positive climatological feedback by means of the global radiation geometry

showing the first 200 of 222

Editorial review for independent work. ICSAC — the Institute for Complexity Science and Advanced Computing — runs a structured editorial panel for researchers publishing outside journals, and publishes on CiteStamp rails. Submission is free and goes through ORCID: icsacinstitute.org/submit.