about
Global climate evolution during the last deglaciationGlobal climate change.The Atlantic Meridional Overturning Circulation and Abrupt Climate Change.A warm thermal enclave in the late Pleistocene of the south-eastern United States.Atlantic meridional overturning circulation during the Last Glacial Maximum.El Niño-like pattern in ice age tropical Pacific sea surface temperature.Dynamic carbonate sedimentation on the Northern Line Islands Ridge, Palmyra BasinGlacial-interglacial changes in central tropical Pacific surface seawater property gradientsConstraints on the salinity–oxygen isotope relationship in the central tropical Pacific OceanCalibration of the carbon isotope composition (δ13 C) of benthic foraminiferaNorth Atlantic intermediate depth variability during the Younger Dryas: Evidence from benthic foraminiferal Mg/Ca and the GFDL R30 Coupled Climate ModelTiming of Deglacial AMOC Variability From a High-Resolution Seawater Cadmium ReconstructionMuted change in Atlantic overturning circulation over some glacial-aged Heinrich eventsWestern Pacific thermocline structure and the Pacific marine Intertropical Convergence Zone during the Last Glacial MaximumTemporal variation in the interhemispheric14C offsetSurface currents in the western North Atlantic during the Last Glacial MaximumOxygen isotopic composition ofGloborotalia truncatulinoidesas a proxy for intermediate depth densitySynchronous and proportional deglacial changes in Atlantic meridional overturning and northeast Brazilian precipitationEffect of lower sea level on geostrophic transport through the Florida Straits during the Last Glacial MaximumAntarctic density stratification and the strength of the circumpolar current during the Last Glacial MaximumCorroborating ecological depth preferences of planktonic foraminifera in the tropical Atlantic with the stable oxygen isotope ratios of core top specimensMid-Holocene El Niño–Southern Oscillation (ENSO) attenuation revealed by individual foraminifera in eastern tropical Pacific sedimentsSimilar glacial and Holocene Southern Ocean hydrographyWhat caused the atmosphere's CO2content to rise during the last 8000 years?Late glacial diatom accumulation at 9°S in the Indian Ocean
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description
researcher, ORCID id # 0000-0002-9353-1972
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wetenschapper
@nl
name
Jean Lynch-Stieglitz
@ast
Jean Lynch-Stieglitz
@en
Jean Lynch-Stieglitz
@es
Jean Lynch-Stieglitz
@nl
type
label
Jean Lynch-Stieglitz
@ast
Jean Lynch-Stieglitz
@en
Jean Lynch-Stieglitz
@es
Jean Lynch-Stieglitz
@nl
prefLabel
Jean Lynch-Stieglitz
@ast
Jean Lynch-Stieglitz
@en
Jean Lynch-Stieglitz
@es
Jean Lynch-Stieglitz
@nl
P1053
J-2277-2018
P1153
6603963528
P21
P31
P496
0000-0002-9353-1972