(Q105255641)

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Foraminiferal faunal estimates of paleotemperature: Circumventing the No-analog problem yields cool Ice Age tropics

scientific article published in June 1999

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Foraminiferal faunal estimates of paleotemperature: Circumventing the No-analog problem yields cool Ice Age tropics (English)

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1 reference

Ann E. Morey

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Steven W. Hostetler

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Steven W. Hostetler

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Alan C. Mix

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1

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Nicklas G. Pisias

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3

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publication date

June 1999

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published in

Paleoceanography

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volume

14

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issue

3

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page(s)

350-359

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The role of ocean-atmosphere interactions in tropical cooling during the last glacial maximum

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Pleistocene climates and chronology in deep-sea sediments

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7 January 2021

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Vertical distribution and isotopic fractionation of living planktonic foraminifera from the Panama Basin

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Simulation of modern and glacial climates with a coupled global model of intermediate complexity

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Tropical temperature variations since 20,000 years ago: modulating interhemispheric climate change

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Foraminiferal magnesium inGloberiginoides sacculiferas a paleotemperature proxy

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The agulhas current during the late pleistocene: analysis of modern faunal analogs

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New Transfer Function for Estimating Past Sea-Surface Conditions from Sea-Bed Distribution of Planktonic Foraminiferal Assemblages in the North Atlantic

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Enhanced ventilation of the North Atlantic subtropical gyre thermocline during the last glaciation

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Cooling of Tropical Brazil (5°C) During the Last Glacial Maximum

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Late glacial stage and holocene tropical ice core records from huascaran, peru

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7 January 2021

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Improving past sea surface temperature estimates based on planktonic fossil faunas

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7 January 2021

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Simulated influence of carbon dioxide, orbital forcing and ice sheets on the climate of the Last Glacial Maximum

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10.1029/1999PA900012

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(Q105255641)

Foraminiferal faunal estimates of paleotemperature: Circumventing the No-analog problem yields cool Ice Age tropics

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