UB Paderborn / Katalog / Suche / in CDI

Increased Ventilation of the Northern Indian Ocean during the Last Deglaciation

Journal of the Geological Society of India, 2020-08, Vol.96 (2), p.148-150

2020

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Early- to late-Holocene contrast in productivity, OMZ intensity and calcite dissolution in the eastern Arabian Sea

Holocene (Sevenoaks), 2014-06, Vol.24 (6), p.749-755

2014

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Shell weights of foraminifera trace atmospheric CO2 from the Miocene to Pleistocene in the central Equatorial Indian Ocean

Journal of Earth System Science, 2020-12, Vol.129 (1), p.69, Article 69

2020

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Carbonate preservation during the ‘mystery interval’ in the northern Indian Ocean

GEOCHEMICAL JOURNAL, 2016/07/29, Vol.50(4), pp.357-362

2016

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Analysis of a regional change in the sign of the SAM-temperature relationship in Antarctica

Climate dynamics, 2011-01, Vol.36 (1-2), p.277-287

2011

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A century of climate variability in central Dronning Maud Land, East Antarctica, and its relation to Southern Annular Mode and El Niño-Southern Oscillation

Journal of Geophysical Research: Atmospheres, 2010-08, Vol.115 (D16), p.n/a

2010

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Relationship between weights of planktonic foraminifer shell and surface water CO3= concentration during the Holocene and Last Glacial Period

Marine geology, 2010-09, Vol.275 (1-4), p.278-282

2010

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Coupling of thermocline depth and strength of the Indian, summer monsoon during deglaciation

Journal of Earth System Science, 2019-06, Vol.128 (4), p.1-6, Article 90

2019

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Evidences of CO2 Leakage During the Last Deglaciation: The Need to Understand Deep-ocean Carbonate Chemistry of the Arabian Sea

Journal of the Geological Society of India, 2018-10, Vol.92 (4), p.404-406

2018

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Influence of climatic teleconnections on the temporal isotopic variability as recorded in a firn core from the coastal Dronning Maud Land, East Antarctica

Journal of Earth System Science, 2010-02, Vol.119 (1), p.41-49

2010

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Use of the Boron partition coefficient ‘KD' and B/Ca from planktonic foraminifera in the estimation of past seawater pCO2

GEOCHEMICAL JOURNAL, 2015/04/16, Vol.49(2), pp.229-231

2015

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Calcite dissolution along a transect in the western tropical Indian Ocean: A multiproxy approach

Geochemistry, geophysics, geosystems : G3, 2007-08, Vol.8 (8), p.Q08009-n/a

2007

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Eastern Arabian Sea CO2 outgassing during the last deglaciation and Holocene related to deep-water carbonate chemistry

Quaternary science reviews, 2023-11, Vol.319, p.108326, Article 108326

2023

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The equatorial Indian Ocean upper water-column structure influenced by cross-basinal water exchange over the last ~40000 years

Quaternary international, 2022-12, Vol.642, p.84-92

2022

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A comparison of Globigerinoides ruber calcification between upwelling and non-upwelling regions in the Arabian Sea

Journal of Earth System Science, 2013-08, Vol.122 (4), p.1153-1159

2013

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Contrasts in calcium carbonate dissolution above the lysocline in the equatorial Indian Ocean over the last ~40 ka

Marine geology, 2022-02, Vol.444, p.106717, Article 106717

2022

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Significant seasonal contrast in the Arabian Sea during deglaciation: Evidence from oxygen isotopic analyses of individual planktic foraminifera

Quaternary international, 2019-02, Vol.503, p.163-169

2019

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Evaluation of the CaCO sub(3) dissolution proxies in sediment cores from above the lysocline

Quaternary international, 2010-02, Vol.213 (1-2), p.69-73

2010

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Evaluation of the CaCO3 dissolution proxies in sediment cores from above the lysocline

Quaternary international, 2010-02, Vol.213 (1-2), p.69-73

2010

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Evaluation of the CaCO 3 dissolution proxies in sediment cores from above the lysocline

Quaternary international, 2010, Vol.213 (1), p.69-73

2010

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Does carbonate ion control planktonic foraminifera shell calcification in upwelling regions?

Current science (Bangalore), 2011-11, Vol.101 (10), p.1370-1375

2011

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Relationship between weights of planktonic foraminifer shell and surface water CO 3 = concentration during the Holocene and Last Glacial Period

Marine geology, 2010, Vol.275 (1), p.278-282

2010

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Effect of varying frontal systems on stable oxygen and carbon isotopic compositions of modern planktic foraminifera of Southern Ocean

Current science (Bangalore), 2011-03, Vol.100 (6), p.881-887

2011

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A century of climate variability in central Dronning Maud Land, East Antarctica, and its relation to Southern Annular Mode and ElNino-Southern Oscillation

Journal of geophysical research. Atmospheres, 2010-08, Vol.115 (D16)

2010

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Antarctic Climate Variability During the Past Few Centuries Based on Ice Core Records from Coastal Dronning Maud Land and Its Implications on the Recent Warming

Earth System Processes and Disaster Management, p.51-66

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Increased Ventilation of the Northern Indian Ocean during the Last Deglaciation

Early- to late-Holocene contrast in productivity, OMZ intensity and calcite dissolution in the eastern Arabian Sea

Shell weights of foraminifera trace atmospheric CO2 from the Miocene to Pleistocene in the central Equatorial Indian Ocean

Carbonate preservation during the ‘mystery interval’ in the northern Indian Ocean

Analysis of a regional change in the sign of the SAM-temperature relationship in Antarctica

A century of climate variability in central Dronning Maud Land, East Antarctica, and its relation to Southern Annular Mode and El Niño-Southern Oscillation

Relationship between weights of planktonic foraminifer shell and surface water CO3= concentration during the Holocene and Last Glacial Period

Coupling of thermocline depth and strength of the Indian, summer monsoon during deglaciation

Evidences of CO2 Leakage During the Last Deglaciation: The Need to Understand Deep-ocean Carbonate Chemistry of the Arabian Sea

Influence of climatic teleconnections on the temporal isotopic variability as recorded in a firn core from the coastal Dronning Maud Land, East Antarctica

Use of the Boron partition coefficient ‘KD' and B/Ca from planktonic foraminifera in the estimation of past seawater pCO2

Calcite dissolution along a transect in the western tropical Indian Ocean: A multiproxy approach

Eastern Arabian Sea CO2 outgassing during the last deglaciation and Holocene related to deep-water carbonate chemistry

The equatorial Indian Ocean upper water-column structure influenced by cross-basinal water exchange over the last ~40000 years

A comparison of Globigerinoides ruber calcification between upwelling and non-upwelling regions in the Arabian Sea

Contrasts in calcium carbonate dissolution above the lysocline in the equatorial Indian Ocean over the last ~40 ka

Significant seasonal contrast in the Arabian Sea during deglaciation: Evidence from oxygen isotopic analyses of individual planktic foraminifera

Evaluation of the CaCO sub(3) dissolution proxies in sediment cores from above the lysocline

Evaluation of the CaCO3 dissolution proxies in sediment cores from above the lysocline

Evaluation of the CaCO 3 dissolution proxies in sediment cores from above the lysocline

Does carbonate ion control planktonic foraminifera shell calcification in upwelling regions?

Relationship between weights of planktonic foraminifer shell and surface water CO 3 = concentration during the Holocene and Last Glacial Period

Effect of varying frontal systems on stable oxygen and carbon isotopic compositions of modern planktic foraminifera of Southern Ocean

A century of climate variability in central Dronning Maud Land, East Antarctica, and its relation to Southern Annular Mode and ElNino-Southern Oscillation

Antarctic Climate Variability During the Past Few Centuries Based on Ice Core Records from Coastal Dronning Maud Land and Its Implications on the Recent Warming

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