On the public citation graph

Sea surface temperature pattern reconstructions in the Arabian Sea

0 signed · 137 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 See whether every reference in this work resolves to a known work and none has been retracted — and get a dated CiteStamped badge you can embed.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/10.1006/qres.1995.1041openalex-snapshot
Sea-Surface Temperatures and the History of Monsoon Upwelling in the Northwest Arabian Sea during the Last 500,000 Years
inferredcites →https://doi.org/10.1006/qres.1999.2083openalex-snapshot
Planktonic Foraminiferal and Alkenone Records of the Last Deglaciation from the Eastern Arabian Sea
inferredcites →https://doi.org/10.1007/978-3-642-80353-6_23openalex-snapshot
Chemical Hydrography of the South Atlantic During the Last Glacial Maximum: Cd vs. δ13C
inferredcites →https://doi.org/10.1007/978-94-009-0995-3_17openalex-snapshot
Wind-Borne Deposits in the Northwestern Indian Ocean: Record of Holocene Sediments Versus Modern Satellite Data
inferredcites →https://doi.org/10.1007/bf00211619openalex-snapshot
The southwest Indian Monsoon over the last 18 000 years
inferredcites →https://doi.org/10.1007/s003820050318openalex-snapshot
Tropical paleoclimates at the Last Glacial Maximum: comparison of Paleoclimate Modeling Intercomparison Project (PMIP) simulations and paleodata
inferredcites →https://doi.org/10.1016/0012-821x(85)90154-2openalex-snapshot
Comparison of Atlantic and Pacific paleochemical records for the last 215,000 years: changes in deep ocean circulation and chemical inventories
inferredcites →https://doi.org/10.1016/0025-3227(91)90021-uopenalex-snapshot
Clay-mineral accumulation rates in the Arabian Sea during the late Quaternary
inferredcites →https://doi.org/10.1016/0025-3227(93)90083-8openalex-snapshot
Upwelling systems: Evolution since the early miocene
inferredcites →https://doi.org/10.1016/0031-0182(86)90108-2openalex-snapshot
Variations of the monsoon regime during the upper quaternary: Evidence from carbon isotopic record of organic matter in North Indian Ocean sediment cores
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/10.1016/0033-5894(78)90064-9openalex-snapshot
Long-Term Variations of Caloric Insolation Resulting from the Earth's Orbital Elements
inferredcites →https://doi.org/10.1016/0033-5894(91)90018-zopenalex-snapshot
Atmospheric summer circulation and coastal upwelling in the Arabian Sea during the Holocene and the last glaciation
inferredcites →https://doi.org/10.1016/0277-3791(91)90033-qopenalex-snapshot
Insolation values for the climate of the last 10 million years
inferredcites →https://doi.org/10.1016/j.quascirev.2004.08.010openalex-snapshot
North Pacific and North Atlantic sea-surface temperature variability during the Holocene
inferredcites →https://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
inferredcites →https://doi.org/10.1016/s0031-0182(03)00633-3openalex-snapshot
Temperature:δ18O relationships of planktonic foraminifera collected from surface waters
inferredcites →https://doi.org/10.1016/s0079-6611(02)00039-3openalex-snapshot
The shallow overturning circulation of the Indian Ocean
inferredcites →https://doi.org/10.1016/s0277-3791(00)00145-1openalex-snapshot
Environmental processes of the ice age: land, oceans, glaciers (EPILOG)
inferredcites →https://doi.org/10.1016/s0277-3791(01)00105-6openalex-snapshot
Apparent long-term cooling of the sea surface in the northeast Atlantic and Mediterranean during the Holocene
inferredcites →https://doi.org/10.1016/s0277-3791(01)00110-xopenalex-snapshot
The oxygen isotopic composition of seawater during the Last Glacial Maximum
inferredcites →https://doi.org/10.1016/s0277-3791(97)00099-1openalex-snapshot
TROPICAL SEA-SURFACE TEMPERATURES DURING THE LAST GLACIAL PERIOD: A VIEW BASED ON ALKENONES IN INDIAN OCEAN SEDIMENTS
inferredcites →https://doi.org/10.1016/s0921-8181(00)00046-1openalex-snapshot
Processes controlling trace element geochemistry of Arabian Sea sediments during the last 25,000 years
inferredcites →https://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
inferredcites →https://doi.org/10.1016/s0967-0645(00)00022-9openalex-snapshot
Fluxes of planktic foraminifera in response to monsoonal upwelling on the Somalia Basin margin
inferredcites →https://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
inferredcites →https://doi.org/10.1017/s0033822200013904openalex-snapshot
Extended 14C Data Base and Revised CALIB 3.0 14C Age Calibration Program
inferredcites →https://doi.org/10.1029/1999jc000061openalex-snapshot
Oxygen isotope/salinity relationship in the northern Indian Ocean
inferredcites →https://doi.org/10.1029/2001pa000749openalex-snapshot
Accurate estimation of sea surface temperatures using dissolution‐corrected calibrations for Mg/Ca paleothermometry
inferredcites →https://doi.org/10.1029/2002pa000846openalex-snapshot
Calibration of Mg/Ca thermometry in planktonic foraminifera from a sediment trap time series
inferredcites →https://doi.org/10.1029/2004gl020928openalex-snapshot
Solar influence on the Indian Ocean Monsoon through dynamical processes
inferredcites →https://doi.org/10.1029/2004pa001031openalex-snapshot
A solar (irradiance) trigger for millennial‐scale abrupt changes in the southwest monsoon?
inferredcites →https://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
inferredcites →https://doi.org/10.1029/2005gc000974openalex-snapshot
Application of secondary ion mass spectrometry to the determination of Mg/Ca in rare, delicate, or altered planktonic foraminifera: Examples from the Holocene, Paleogene, and Cretaceous
inferredcites →https://doi.org/10.1029/95gl02558openalex-snapshot
A 2,200 years periodicity in the Asian Monsoon System
inferredcites →https://doi.org/10.1029/95pa00310openalex-snapshot
Glacial enrichments of authigenic Cd And U in subantarctic sediments: A climatic control on the elements' oceanic budget?
inferredcites →https://doi.org/10.1029/96gl01030openalex-snapshot
A 27,000 year record of Red Sea Outflow: Implication for timing of post‐glacial monsoon intensification
inferredcites →https://doi.org/10.1029/98pa00071openalex-snapshot
Improving past sea surface temperature estimates based on planktonic fossil faunas
inferredcites →https://doi.org/10.1029/98pa02203openalex-snapshot
Temporal variability in the northern Arabian Sea oxygen minimum zone (OMZ) during the last 225,000 years
inferredcites →https://doi.org/10.1029/gm029p0048openalex-snapshot
Variation of monsoonal upwelling: A response to changing solar radiation
inferredcites →https://doi.org/10.1029/jd093id01p00803openalex-snapshot
Sensitivity of a coupled atmosphere/mixed layer ocean model to changes in orbital forcing at 9000 years B.P.
inferredcites →https://doi.org/10.1038/20859openalex-snapshot
Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica
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/10.1038/346456a0openalex-snapshot
U-Th ages obtained by mass spectrometry in corals from Barbados: sea level during the past 130,000 years
inferredcites →https://doi.org/10.1038/353720a0openalex-snapshot
Forcing mechanisms of the Indian Ocean monsoon
inferredcites →https://doi.org/10.1038/360647a0openalex-snapshot
Sensitivity of the Indian monsoon to forcing parameters and implications for its evolution
inferredcites →https://doi.org/10.1038/364319a0openalex-snapshot
Reconstructing sea surface temperature and salinity using δ18O and alkenone records
inferredcites →https://doi.org/10.1038/364322a0openalex-snapshot
Century-scale events in monsoonal climate over the past 24,000 years
inferredcites →https://doi.org/10.1038/382241a0openalex-snapshot
Deglacial sea-level record from Tahiti corals and the timing of global meltwater discharge
inferredcites →https://doi.org/10.1038/385707a0openalex-snapshot
Interhemispheric synchrony of the last deglaciation inferred from alkenone palaeothermometry
inferredcites →https://doi.org/10.1038/nature01340openalex-snapshot
Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean
inferredcites →https://doi.org/10.1038/nature02346openalex-snapshot
Links between salinity variation in the Caribbean and North Atlantic thermohaline circulation
inferredcites →https://doi.org/10.1111/j.1469-8137.2007.02357.xopenalex-snapshot
Thermal acclimation of leaf respiration but not photosynthesis in Populus deltoides×nigra
inferredcites →https://doi.org/10.1126/science.1072881openalex-snapshot
Increase in the Asian Southwest Monsoon During the Past Four Centuries
inferredcites →https://doi.org/10.1126/science.1083130openalex-snapshot
Holocene Forcing of the Indian Monsoon Recorded in a Stalagmite from Southern Oman
inferredcites →https://doi.org/10.1126/science.1088470openalex-snapshot
Synchroneity of Tropical and High-Latitude Atlantic Temperatures over the Last Glacial Termination
inferredcites →https://doi.org/10.1126/science.289.5483.1321openalex-snapshot
Hydrological Impact of Heinrich Events in the Subtropical Northeast Atlantic
inferredcites →https://doi.org/10.1126/science.291.5501.112openalex-snapshot
Atmospheric CO 2 Concentrations over the Last Glacial Termination
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/10.1175/1520-0442(2000)013<0951:tcatlg>2.0.co;2openalex-snapshot
Tropical Cooling at the Last Glacial Maximum: An Atmosphere–Mixed Layer Ocean Model Simulation
inferredcites →https://doi.org/10.1175/1520-0442(2003)016<2472:ccsote>2.0.co;2openalex-snapshot
Coupled Climate Simulation of the Evolution of Global Monsoons in the Holocene*
inferredcites →https://doi.org/10.17617/2.2580838openalex-snapshot
An atlas based on the 'Coads' data set: The budgets of heat, buoyancy and turbulent kinetic energy at the surface of global ocean
inferredcites →https://doi.org/10.5860/choice.32-0947openalex-snapshot
Global climates since the last glacial maximum

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/10.1002/2013pa002579openalex-snapshot
Late Holocene primary productivity and sea surface temperature variations in the northeastern Arabian Sea: Implications for winter monsoon variability
inferred← citeshttps://doi.org/10.1002/2015pa002890openalex-snapshot
The climate response of the Indo‐Pacific warm pool to glacial sea level
inferred← citeshttps://doi.org/10.1002/2017pa003201openalex-snapshot
BAYSPLINE: A New Calibration for the Alkenone Paleothermometer
inferred← citeshttps://doi.org/10.1002/palo.20040openalex-snapshot
Variation in the Indian summer monsoon intensity during the Bølling‐Ållerød and Holocene
inferred← citeshttps://doi.org/10.1007/s00343-025-5062-8openalex-snapshot
Oceanographic significance of planktonic foraminiferal assemblages in the northwest Indian Ocean-Basin-Ridge system under monsoon influence
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/s12040-017-0864-5openalex-snapshot
Indian summer monsoon forcing on the deglacial polar cold reversals
inferred← citeshttps://doi.org/10.1007/s12040-022-01897-yopenalex-snapshot
Possible zonal asymmetry of the Indian summer monsoon rainfall after ~5 ka BP as revealed by palaeo-salinity in the eastern Arabian Sea
inferred← citeshttps://doi.org/10.1007/s12594-016-0399-4openalex-snapshot
A Comparison of Mg/Ca Ratios in Globigerinoides ruber (white): sensu stricto versus a Mixture of Genotypes
inferred← citeshttps://doi.org/10.1007/s43538-024-00307-9openalex-snapshot
Recent advancements in marine micropaleontological and paleoceanographic research from India
inferred← citeshttps://doi.org/10.1016/b978-0-12-822402-1.00070-3openalex-snapshot
Teleconnections between the Indian summer monsoon and climate variability: a proxy perspective
inferred← citeshttps://doi.org/10.1016/b978-0-323-99931-1.00322-6openalex-snapshot
Postglacial Indian Ocean
inferred← citeshttps://doi.org/10.1016/b978-0-444-53643-3.00301-0openalex-snapshot
PALEOCEANOGRAPHY, RECORDS | Postglacial Indian Ocean
inferred← citeshttps://doi.org/10.1016/j.csr.2021.104491openalex-snapshot
Hydrological characteristics of the Bay of Bengal water column using δ18O during the Indian summer monsoon
inferred← citeshttps://doi.org/10.1016/j.csr.2026.105664openalex-snapshot
Modern sediment sources and transport processes in the southern Arabian Sea: Evidences from geochemistry and mineralogy
inferred← citeshttps://doi.org/10.1016/j.epsl.2013.05.022openalex-snapshot
Deglaciation in the tropical Indian Ocean driven by interplay between the regional monsoon and global teleconnections
inferred← citeshttps://doi.org/10.1016/j.jseaes.2024.106121openalex-snapshot
Sediment provenance variations driven by sea level in the eastern Arabian Sea since the MIS 9 period: Evidence from geochemical proxies
inferred← citeshttps://doi.org/10.1016/j.margeo.2026.107860openalex-snapshot
Millennial-centennial climate variabilities in the western Arabian Sea during DO 12-11 reconstructed from foraminiferal proxies
inferred← citeshttps://doi.org/10.1016/j.marmicro.2010.09.006openalex-snapshot
Sea surface temperature changes during May and August in the western Arabian Sea over the last 22kyr: Implications as to shifting of the upwelling season
inferred← citeshttps://doi.org/10.1016/j.marmicro.2026.102561openalex-snapshot
Changes in pteropod assemblage driven by monsoonal variability and associated oceanographic conditions since the last Glacial Maximum in the eastern Arabian Sea
inferred← citeshttps://doi.org/10.1016/j.palaeo.2008.03.007openalex-snapshot
Surface and deep water changes in the northeast Indian Ocean during the last 60 ka inferred from carbon and oxygen isotopes of planktonic and benthic foraminifera
inferred← citeshttps://doi.org/10.1016/j.palaeo.2013.05.024openalex-snapshot
Change in the intensity of low-salinity water inflow from the Bay of Bengal into the Eastern Arabian Sea from the Last Glacial Maximum to the Holocene: Implications for monsoon variations
inferred← citeshttps://doi.org/10.1016/j.palaeo.2013.11.001openalex-snapshot
A glimpse of the Quaternary monsoon history from India and adjoining seas
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.2016.07.014openalex-snapshot
Last glacial-interglacial productivity and associated changes in the eastern Arabian Sea
inferred← citeshttps://doi.org/10.1016/j.palaeo.2017.07.026openalex-snapshot
Glacial to Holocene changes in sea surface temperature and seawater δ18O in the northern Indian Ocean
inferred← citeshttps://doi.org/10.1016/j.palaeo.2021.110326openalex-snapshot
Uncertainty in palaeosalinity estimates from foraminiferal geochemical records in the northern 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.2025.113190openalex-snapshot
Core-top constraints on the ecology and paleothermometry of planktic foraminifera in the Indian Ocean
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.quaint.2016.07.012openalex-snapshot
Revisiting reconstructed Indian monsoon rainfall variations during the last ∼25 ka from planktonic foraminiferal δ18O from the Eastern Arabian Sea
inferred← citeshttps://doi.org/10.1016/j.quaint.2016.08.030openalex-snapshot
Investigating the dynamical behavior of the Intertropical Convergence Zone since the last glacial maximum based on terrestrial and marine sedimentary records
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.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.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.2016.11.028openalex-snapshot
Qualitative assessment of PMIP3 rainfall simulations across the eastern African monsoon domains during the mid-Holocene and the Last Glacial Maximum
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/10.1017/qua.2020.118openalex-snapshot
Causes and climatic influence of centennial-scale denitrification variability in the southeastern Arabian Sea since the last glacial period
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/10.1029/2017gc007286openalex-snapshot
Variations in Denitrification and Ventilation Within the Arabian Sea Oxygen Minimum Zone During the Holocene
inferred← citeshttps://doi.org/10.1029/2019pa003576openalex-snapshot
Global Core Top Calibration of δ18O in Planktic Foraminifera to Sea Surface Temperature
inferred← citeshttps://doi.org/10.1029/2019pa003744openalex-snapshot
Bayesian Calibration of the Mg/Ca Paleothermometer in Planktic Foraminifera
inferred← citeshttps://doi.org/10.1029/2019pa003811openalex-snapshot
Enhanced Poleward Flux of Atmospheric Moisture to the Weddell Sea Region (ODP Site 690) During the Paleocene‐Eocene Thermal Maximum
inferred← citeshttps://doi.org/10.1029/2021pa004255openalex-snapshot
Applicability of the Long Chain Diol Index (LDI) as a Sea Surface Temperature Proxy in the Arabian Sea
inferred← citeshttps://doi.org/10.1029/2022pa004570openalex-snapshot
Enhanced CO2 Degassing From the Tropical Indian Ocean During Cold Climatic Events of the Last Glacial Cycle
inferred← citeshttps://doi.org/10.1029/2023pa004632openalex-snapshot
Reconstructing the Oxygen Depth Profile in the Arabian Sea During the Last Glacial Period
inferred← citeshttps://doi.org/10.1029/2026gl124170openalex-snapshot
A Multi‐Basin Calibration of Magnetofossils as a Quantitative Proxy for Bottom Water Oxygenation
inferred← citeshttps://doi.org/10.1038/ngeo2603openalex-snapshot
Deglacial Indian monsoon failure and North Atlantic stadials linked by Indian Ocean surface cooling
inferred← citeshttps://doi.org/10.1038/s41598-022-07774-4openalex-snapshot
Abrupt upwelling and CO2 outgassing episodes in the north-eastern Arabian Sea since mid-Holocene
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/10.1111/j.1755-6724.2012.00746.xopenalex-snapshot
Linkage between Seasonal Insolation Gradient in the Tropical Northern Hemisphere and the Sea Surface Salinity of the Equatorial Indian Ocean during the Last Glacial Period
inferred← citeshttps://doi.org/10.1126/sciadv.aat9658openalex-snapshot
Glacial changes in tropical climate amplified by the Indian Ocean
inferred← citeshttps://doi.org/10.1130/g32608.1openalex-snapshot
Impact of Indus River discharge on productivity and preservation of organic carbon in the Arabian Sea over the twentieth century
inferred← citeshttps://doi.org/10.1186/s40645-020-00349-9openalex-snapshot
Reconstruction of monsoon evolution in southernmost Sumatra over the past 35 kyr and its response to northern hemisphere climate changes
inferred← citeshttps://doi.org/10.1371/journal.pone.0222299openalex-snapshot
Controls on planktonic foraminifera apparent calcification depths for the northern equatorial Indian Ocean
inferred← citeshttps://doi.org/10.1575/1912/5136openalex-snapshot
The centennial and millennial variability of the IndoPacific Warm Pool and the Indonesian Throughflow
inferred← citeshttps://doi.org/10.1594/pangaea.834986openalex-snapshot
(Table 2) Age determination of sediment core TN047-6-GGC
inferred← citeshttps://doi.org/10.1594/pangaea.834987openalex-snapshot
(Table 3) Mg/Ca ratios of Globigerinoides ruber from Arabian Sea sediments
inferred← citeshttps://doi.org/10.1594/pangaea.834988openalex-snapshot
(Table 4) Seawater oxygen isotopes and salinity in the Arabian Sea
inferred← citeshttps://doi.org/10.1594/pangaea.945401openalex-snapshot
Oxygen isotopic ratio of Globigerinoides ruber (white variety) in the surface sediments of the northern Indian Ocean
inferred← citeshttps://doi.org/10.2343/geochemj.2.0371openalex-snapshot
Migration history of an ariid Indian catfish reconstructed by otolith Sr/Ca and δ18O micro-analysis
inferred← citeshttps://doi.org/10.3390/oceans7010019openalex-snapshot
Reorganization of the Arabian Sea Oxygen Minimum Zone in Response to Monsoon Fluctuations During Dansgaard–Oeschger Events 12–11
inferred← citeshttps://doi.org/10.5194/cp-13-491-2017openalex-snapshot
Decadal resolution record of Oman upwelling indicates solar forcing of the Indian summer monsoon (9–6 ka)
inferred← citeshttps://doi.org/10.5194/cp-14-1331-2018openalex-snapshot
Variations of the Somali upwelling since 18.5 ka BP and its relationship with southwest monsoon rainfall
inferred← citeshttps://doi.org/10.5194/cp-15-73-2019openalex-snapshot
Indian winter and summer monsoon strength over the 4.2 ka BP event in foraminifer isotope records from the Indus River delta in the Arabian Sea
inferred← citeshttps://doi.org/10.5194/cp-17-1243-2021openalex-snapshot
The remote response of the South Asian Monsoon to reduced dust emissions and Sahara greening during the middle Holocene
inferred← citeshttps://doi.org/10.5194/cp-21-279-2025openalex-snapshot
Spatial and temporal variability in sea surface temperatures and monsoon dynamics in the northwestern Arabian Sea during the last 43 kyr
inferred← citeshttps://doi.org/10.5194/cpd-10-3661-2014openalex-snapshot
Oxygen isotopic analyses of individual planktic foraminifera species: implications for seasonality in the western Arabian Sea
inferred← citeshttps://doi.org/10.70675/16c3f866z07caz49a5zb382z2d6b2ebeb7a0openalex-snapshot
Climate variability over the tropical Indian Ocean since the Last Glacial Maximum and its impact on primary productivity : insights from model-data comparisons
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.