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Millennial Variability in Intermediate Ocean Circulation and Indian Monsoonal Weathering Inputs During the Last Deglaciation and Holocene

https://doi.org/10.1029/2022gl100003

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What this work says

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

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Weakening and strengthening of the Indian monsoon during Heinrich events and Dansgaard-Oeschger oscillations

inferredcites →https://doi.org/10.1002/2014pa002707openalex-snapshot

Interhemispheric controls on deep ocean circulation and carbon chemistry during the last two glacial cycles

inferredcites →https://doi.org/10.1002/2015gl064015openalex-snapshot

Abrupt changes in Indian summer monsoon strength during 33,800 to 5500 years B.P.

inferredcites →https://doi.org/10.1007/978-3-642-80353-6_11openalex-snapshot

Antarctic Intermediate Water in the South Atlantic

inferredcites →https://doi.org/10.1016/0012-821x(88)90153-7openalex-snapshot

Origin of Deccan Trap lavas: evidence from combined trace element and Sr-, Nd- and Pb-isotope studies

inferredcites →https://doi.org/10.1016/b0-08-043751-6/06179-xopenalex-snapshot

Long-lived Isotopic Tracers in Oceanography, Paleoceanography, and Ice-sheet Dynamics

inferredcites →https://doi.org/10.1016/j.chemgeo.2019.01.007openalex-snapshot

Neodymium concentration and isotopic composition distributions in the southwestern Indian Ocean and the Indian sector of the Southern Ocean

inferredcites →https://doi.org/10.1016/j.earscirev.2020.103216openalex-snapshot

New insights on Chinese cave δ18O records and their paleoclimatic significance

inferredcites →https://doi.org/10.1016/j.epsl.2010.08.025openalex-snapshot

The release of 14C-depleted carbon from the deep ocean during the last deglaciation: Evidence from the Arabian Sea

inferredcites →https://doi.org/10.1016/j.epsl.2011.06.019openalex-snapshot

New Arabian Sea records help decipher orbital timing of Indo-Asian monsoon

inferredcites →https://doi.org/10.1016/j.epsl.2012.06.009openalex-snapshot

A boundary exchange influence on deglacial neodymium isotope records from the deep western Indian Ocean

inferredcites →https://doi.org/10.1016/j.epsl.2013.01.038openalex-snapshot

Increasing chemical weathering in the Himalayan system since the Last Glacial Maximum

inferredcites →https://doi.org/10.1016/j.epsl.2015.05.014openalex-snapshot

Quaternary climate modulation of Pb isotopes in the deep Indian Ocean linked to the Himalayan chemical weathering

inferredcites →https://doi.org/10.1016/j.epsl.2016.09.027openalex-snapshot

Neodymium isotopic evidence for linked changes in Southeast Atlantic and Southwest Pacific circulation over the last 200 kyr

inferredcites →https://doi.org/10.1016/j.epsl.2017.08.013openalex-snapshot

Post-glacial climate forcing of surface processes in the Ganges–Brahmaputra river basin and implications for carbon sequestration

inferredcites →https://doi.org/10.1016/j.epsl.2017.09.022openalex-snapshot

Seasonal variations in dissolved neodymium isotope composition in the Bay of Bengal

inferredcites →https://doi.org/10.1016/j.epsl.2018.08.006openalex-snapshot

Antarctic Intermediate Water penetration into the Northern Indian Ocean during the last deglaciation

inferredcites →https://doi.org/10.1016/j.gca.2014.09.006openalex-snapshot

Impact of water mass mixing and dust deposition on Nd concentration and ε Nd of the Arabian Sea water column

inferredcites →https://doi.org/10.1016/j.gca.2018.10.018openalex-snapshot

The resilience and sensitivity of Northeast Atlantic deep water εNd to overprinting by detrital fluxes over the past 30,000 years

inferredcites →https://doi.org/10.1016/j.gca.2021.11.021openalex-snapshot

Widespread lithogenic control of marine authigenic neodymium isotope records? Implications for paleoceanographic reconstructions

inferredcites →https://doi.org/10.1016/j.quascirev.2010.05.003openalex-snapshot

Northern Hemisphere climate control of the Bengali rivers discharge during the past 4 Ma

inferredcites →https://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

inferredcites →https://doi.org/10.1016/j.quascirev.2013.12.027openalex-snapshot

Neodymium associated with foraminiferal carbonate as a recorder of seawater isotopic signatures

inferredcites →https://doi.org/10.1016/j.quascirev.2014.08.010openalex-snapshot

Evolution of the Indian Summer Monsoon and terrestrial vegetation in the Bengal region during the past 18 ka

inferredcites →https://doi.org/10.1016/s0012-821x(00)00011-xopenalex-snapshot

Glacial–interglacial variations in the neodymium isotope composition of seawater in the Bay of Bengal recorded by planktonic foraminifera

inferredcites →https://doi.org/10.1016/s0012-821x(01)00317-xopenalex-snapshot

Erosion of Deccan Traps determined by river geochemistry: impact on the global climate and the 87Sr/86Sr ratio of seawater

inferredcites →https://doi.org/10.1016/s0012-821x(02)00822-1openalex-snapshot

Tracing the distribution of erosion in the Brahmaputra watershed from isotopic compositions of stream sediments

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/10.1029/2011gc003802openalex-snapshot

Temporal variations in 87Sr/86Sr and ɛNd in sediments of the southeastern Arabian Sea: Impact of monsoon and surface water circulation

inferredcites →https://doi.org/10.1029/2018gc007860openalex-snapshot

A 16‐kyr Record of Ocean Circulation and Monsoon Intensification From the Central Bay of Bengal

inferredcites →https://doi.org/10.1029/97jc00880openalex-snapshot

Oxygen 18/16 variability in Greenland snow and ice with 10−3‐ to 105‐year time resolution

inferredcites →https://doi.org/10.1038/nature02494openalex-snapshot

Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes

inferredcites →https://doi.org/10.1038/nature05365openalex-snapshot

Negligible glacial–interglacial variation in continental chemical weathering rates

inferredcites →https://doi.org/10.1038/nature07828openalex-snapshot

Variable Quaternary chemical weathering fluxes and imbalances in marine geochemical budgets

inferredcites →https://doi.org/10.1038/nature09044openalex-snapshot

Long-term stability of global erosion rates and weathering during late-Cenozoic cooling

inferredcites →https://doi.org/10.1038/nature12376openalex-snapshot

Onset of deglacial warming in West Antarctica driven by local orbital forcing

inferredcites →https://doi.org/10.1038/nature18591openalex-snapshot

The Asian monsoon over the past 640,000 years and ice age terminations

inferredcites →https://doi.org/10.1038/nature22995openalex-snapshot

West Antarctic Ice Sheet retreat driven by Holocene warm water incursions

inferredcites →https://doi.org/10.1038/ngeo2452openalex-snapshot

Stable runoff and weathering fluxes into the oceans over Quaternary climate cycles

inferredcites →https://doi.org/10.1038/ngeo2603openalex-snapshot

Deglacial Indian monsoon failure and North Atlantic stadials linked by Indian Ocean surface cooling

inferredcites →https://doi.org/10.1038/ngeo987openalex-snapshot

Southern Ocean source of 14C-depleted carbon in the North Pacific Ocean during the last deglaciation

inferredcites →https://doi.org/10.1038/s41467-019-13707-zopenalex-snapshot

Glacial–interglacial Nd isotope variability of North Atlantic Deep Water modulated by North American ice sheet

inferredcites →https://doi.org/10.1038/s41561-019-0319-5openalex-snapshot

Role of Asian summer monsoon subsystems in the inter-hemispheric progression of deglaciation

inferredcites →https://doi.org/10.1038/s41561-020-0585-2openalex-snapshot

Steady erosion rates in the Himalayas through late Cenozoic climatic changes

inferredcites →https://doi.org/10.1038/srep24374openalex-snapshot

Indian monsoon variability on millennial-orbital timescales

inferredcites →https://doi.org/10.1038/srep44310openalex-snapshot

Increased chemical weathering during the deglacial to mid-Holocene summer monsoon intensification

inferredcites →https://doi.org/10.1051/0004-6361:20041335openalex-snapshot

A long-term numerical solution for the insolation quantities of the Earth

inferredcites →https://doi.org/10.1098/rsta.2015.0293openalex-snapshot

Neodymium in the oceans: a global database, a regional comparison and implications for palaeoceanographic research

inferredcites →https://doi.org/10.1126/science.1138679openalex-snapshot

Marine Radiocarbon Evidence for the Mechanism of Deglacial Atmospheric CO 2 Rise

inferredcites →https://doi.org/10.1126/science.1167441openalex-snapshot

Wind-Driven Upwelling in the Southern Ocean and the Deglacial Rise in Atmospheric CO 2

inferredcites →https://doi.org/10.1130/0091-7613(2001)029<0023:herith>2.0.co;2openalex-snapshot

Higher erosion rates in the Himalaya: Geochemical constraints on riverine fluxes

inferredcites →https://doi.org/10.1130/0091-7613(2001)029<0063:maaocc>2.0.co;2openalex-snapshot

Modulation and amplification of climatic changes in the Northern Hemisphere by the Indian summer monsoon during the past 80 k.y

inferredcites →https://doi.org/10.3390/quat1030029openalex-snapshot

The Indian Summer Monsoon from a Speleothem δ18O Perspective—A Review

inferredcites →https://doi.org/10.3390/quat2010007openalex-snapshot

SISAL: Bringing Added Value to Speleothem Research

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/10.1016/b978-0-323-99712-6.00023-4openalex-snapshot

Introduction to the Holocene glacial landscapes

inferred← citeshttps://doi.org/10.1016/j.chemgeo.2024.121954openalex-snapshot

Roles of changes in land weathering intensity in the Nd cycle of the South China Sea during the past 30 kyr as inferred from neodymium isotopic composition in foraminifera

inferred← citeshttps://doi.org/10.1016/j.chemgeo.2025.122652openalex-snapshot

Clay Li isotopes reveal contrasting responses of chemical weathering intensity to hydroclimate changes in South Asia

inferred← citeshttps://doi.org/10.1016/j.chemgeo.2025.122807openalex-snapshot

Study of the sources and dispersion of sediments on the Sunda Shelf based on the investigation of rare earth element concentrations and Nd isotope compositions

inferred← citeshttps://doi.org/10.1016/j.chemgeo.2025.123107openalex-snapshot

New isotopic constraints on the role of continental weathering in the neodymium cycle of the Nordic Seas over the last 22,000 years

inferred← citeshttps://doi.org/10.1016/j.epsl.2024.118902openalex-snapshot

Impact of riverine sediment mineralogy on seawater Nd isotope compositions in the northeastern part of the Indian Ocean during the last two glacial cycles

inferred← citeshttps://doi.org/10.1016/j.gca.2025.12.003openalex-snapshot

Neodymium isotopes in marginal seawater trace continental weathering inputs

inferred← citeshttps://doi.org/10.1016/j.gloplacha.2025.105048openalex-snapshot

Late Pliocene millennial-scale climate variability response of the South Asian summer monsoon to low-latitude insolation and Antarctic ice sheet forcing

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.margeo.2025.107632openalex-snapshot

Sea level changes and the Indian Summer Monsoon influence on chemical weathering and sediment deposition on the Ninetyeast Ridge over the past 21 ka

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.2024.112710openalex-snapshot

Impact of continental weathering on deep northwestern Pacific εNd over the past 16,000 years

inferred← citeshttps://doi.org/10.1016/j.palaeo.2025.113430openalex-snapshot

Orbital-scale sea level and millennial-scale climatic event controls on terrestrial input in the northern Ninetyeast Ridge over the past 40 kyr

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.quascirev.2023.108109openalex-snapshot

Unraveling the climate control on debris-free glacier evolution in the Everest region (Nepal, central Himalaya) during the Holocene

inferred← citeshttps://doi.org/10.1016/j.quascirev.2024.108723openalex-snapshot

Millennial to orbital scale Indian summer monsoon evolution inferred from grain size end-members in Tengchongbeihai wetland, southwestern China

inferred← citeshttps://doi.org/10.1016/j.quascirev.2024.108994openalex-snapshot

Comparing the evolution of debris-free and debris-covered glaciers during the end of the Lateglacial and the Holocene in Dudh Koshi basin, Everest region, Nepal

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.2025.109659openalex-snapshot

The first application of RI-OH lipid biomarkers to reconstruct the upper water column thermal structure. An example from the tropical Indian Ocean (Bay of Bengal) during the past 24 kyr

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/10.1029/2024gl114500openalex-snapshot

Tectonics Modulated Long‐Term Weathering Inputs From the East Asian Continent and Tropical Island Arc to the South China Sea Since the Late Oligocene

inferred← citeshttps://doi.org/10.1029/2024pa004857openalex-snapshot

Magnetic Response to the Source‐To‐Sink Environmental Changes in the Bay of Bengal Since ∼60 ka

inferred← citeshttps://doi.org/10.1029/2024pa005025openalex-snapshot

Lithium Isotope Reveals Tight Links Between Chemical Weathering Intensity and Indian Summer Monsoon in South Asia

inferred← citeshttps://doi.org/10.1029/2025gc012711openalex-snapshot

Nd Isotope Response to Precipitation Variability in the Western Tropical Pacific Over the Last 30 kyr

inferred← citeshttps://doi.org/10.1029/2025pa005310openalex-snapshot

Tracking the Millennial Scale Variability of Deep Water Circulation and Lithogenic Influence in the Arabian Sea Over the Past 41 ka Through Nd Isotope

inferred← citeshttps://doi.org/10.1029/2026gl124113openalex-snapshot

Different Orbital Controls on Detrital Magnetic Components in the Ninety‐East Ridge Since the Late Pleistocene

inferred← citeshttps://doi.org/10.1029/2026jc024726openalex-snapshot

Tracking Water Masses and Lithogenic Inputs Along the GEOTRACES GI10 Transect in the Arabian Sea With Dissolved Neodymium Concentration and Isotopes

inferred← citeshttps://doi.org/10.1088/1748-9326/ad5bf4openalex-snapshot

Wind-driven sediment exchange between the Indian marginal seas over the last 18 000 years

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/10.1130/b38602.1openalex-snapshot

The phase lag between Indian Summer Monsoon and Northern Hemisphere summer insolation driven by ice volume and greenhouse gas

inferred← citeshttps://doi.org/10.1175/jcli-d-23-0667.1openalex-snapshot

Indian Ocean Intermediate Water Masses and Their Simulations by CMIP6 Models

inferred← citeshttps://doi.org/10.70675/022999a2z9a7cz4153z801dz2b911548f8beopenalex-snapshot

Past changes in weathering of the peri-Himalayan rivers and ocean circulations in the South China Sea and the Bay of Bengal : new constraints from the εNd proxy

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