Southwest Pacific deep water carbonate chemistry linked to high southern latitude climate and atmospheric CO2 during the Last Glacial Termination

Katherine A Allen, Elisabeth L. Sikes, Thomas P. Guilderson, Yair Rosenthal, Robert F. Anderson
Published 2015

Abstract

A greater amount of CO2 was stored in the deep sea during glacial periods, likely via greater efficiency of the biologic pump and increased uptake by a more alkaline ocean. Reconstructing past variations in seawater carbonate ion concentration (a major component of alkalinity) enables quantification of the relative roles of different oceanic CO2 storage… (More)

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Cited By

Links between eastern equatorial Pacific stratification and atmospheric CO2 rise during the last deglaciation

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Synchronous centennial abrupt events in the ocean and atmosphere during the last deglaciation.

Tianyu Chen, Laura F Robinson, +4 authors Hong Chin Ng
Science
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Southwest Pacific deep water carbonate chemistry linked to high southern latitude climate and atmospheric CO2 during the Last Glacial Termination

Abstract

Topics

7 Figures and Tables

Cited By

Links between eastern equatorial Pacific stratification and atmospheric CO2 rise during the last deglaciation

Synchronous centennial abrupt events in the ocean and atmosphere during the last deglaciation.

References

Centennial-scale changes in the global carbon cycle during the last deglaciation.

Neodymium isotopic composition of intermediate and deep waters in the glacial southwest Pacific

Reviewing the circulation and mixing of Antarctic Intermediate Water in the South Pacific using evidence from geochemical tracers and Argo float trajectories

Glacial-interglacial changes in water mass structure and flow in the SW Pacific Ocean

A global ocean carbon climatology: Results from Global Data Analysis Project (GLODAP)

Palynology, vegetation and climate of the Waikato Lowlands, North Island, New Zealand, since ~18,000 years ago

Boron isotope evidence for oceanic carbon dioxide leakage during the last deglaciation.

Distinct roles of the Southern Ocean and North Atlantic in the deglacial atmospheric radiocarbon decline

Closure of the global overturning circulation through the Indian, Pacific, and Southern Oceans: schematics and transports

Responses of the deep ocean carbonate system to carbon reorganization during the Last GlacialeInterglacial cycle

Slides referencing similar topics

Southwest Pacific deep water carbonate chemistry linked to high southern latitude climate and atmospheric CO2 during the Last Glacial Termination

Abstract

Topics

7 Figures and Tables

Cited By

Links between eastern equatorial Pacific stratification and atmospheric CO2 rise during the last deglaciation

Synchronous centennial abrupt events in the ocean and atmosphere during the last deglaciation.

References

Centennial-scale changes in the global carbon cycle during the last deglaciation.

Neodymium isotopic composition of intermediate and deep waters in the glacial southwest Pacific

Reviewing the circulation and mixing of Antarctic Intermediate Water in the South Pacific using evidence from geochemical tracers and Argo float trajectories

Glacial-interglacial changes in water mass structure and flow in the SW Pacific Ocean

A global ocean carbon climatology: Results from Global Data Analysis Project (GLODAP)

Palynology, vegetation and climate of the Waikato Lowlands, North Island, New Zealand, since ~18,000 years ago

Boron isotope evidence for oceanic carbon dioxide leakage during the last deglaciation.

Distinct roles of the Southern Ocean and North Atlantic in the deglacial atmospheric radiocarbon decline

Closure of the global overturning circulation through the Indian, Pacific, and Southern Oceans: schematics and transports

Responses of the deep ocean carbonate system to carbon reorganization during the Last GlacialeInterglacial cycle

Similar Papers

Slides referencing similar topics