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Seasonal origin of the thermal maxima at the Holocene and the last interglacial

Nature (London), 2021-01, Vol.589 (7843), p.548-553

2021

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Reply to: Concerns of assuming linearity in the reconstruction of thermal maxima

Nature (London), 2022-07, Vol.607 (7920), p.E15-E18

2022

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Reply to: Non-trivial role of internal climate feedback on interglacial temperature evolution

Nature (London), 2021-12, Vol.600 (7887), p.E4-E6

2021

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Potential and pitfalls of XRF-CS analysis of ion-exchange resins in environmental studies

Scientific reports, 2021-10, Vol.11 (1), p.20941-11, Article 20941

2021

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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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Evolution of productivity and monsoonal dynamics in the eastern Arabian Sea during the past 68ka using dinoflagellate cyst records

Palaeogeography, palaeoclimatology, palaeoecology, 2015-10, Vol.435, p.193-202

2015

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70 kyr record of denitrification and oxygenation changes in the eastern Arabian Sea

GEOCHEMICAL JOURNAL, 2017/07/21, Vol.51(4), pp.329-336

2017

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Multifunctional Ag2CO3 microrods as SERS-active substrate for the detection and degradation of Rhodamine B dye

Spectrochimica acta. Part A, Molecular and biomolecular spectroscopy, 2021-12, Vol.263, p.120176, Article 120176

2021

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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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Sea surface temperature changes during May and August in the western Arabian Sea over the last 22kyr: Implications as to shifting of the upwelling season

Marine micropaleontology, 2011-01, Vol.78 (1-2), p.25-29

2011

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Remote forcing of winter cooling in the Arabian Sea: Implications for the NE monsoon

Palaeogeography, palaeoclimatology, palaeoecology, 2022-01, Vol.586, p.110755, Article 110755

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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Concerns of assuming linearity in the reconstruction of thermal maxima/Reply

Nature (London), 2022-07, Vol.607 (7920), p.E12-E18

2022

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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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Sea surface temperature changes during May and August in the western Arabian Sea over the last 22 kyr: Implications as to shifting of the upwelling season

Marine micropaleontology, 2011, Vol.78 (1), p.25-29

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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Seasonal origin of the thermal maxima at the Holocene and the last interglacial

Reply to: Concerns of assuming linearity in the reconstruction of thermal maxima

Reply to: Non-trivial role of internal climate feedback on interglacial temperature evolution

Potential and pitfalls of XRF-CS analysis of ion-exchange resins in environmental studies

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

Evolution of productivity and monsoonal dynamics in the eastern Arabian Sea during the past 68ka using dinoflagellate cyst records

70 kyr record of denitrification and oxygenation changes in the eastern Arabian Sea

Multifunctional Ag2CO3 microrods as SERS-active substrate for the detection and degradation of Rhodamine B dye

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

Sea surface temperature changes during May and August in the western Arabian Sea over the last 22kyr: Implications as to shifting of the upwelling season

Remote forcing of winter cooling in the Arabian Sea: Implications for the NE monsoon

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

Concerns of assuming linearity in the reconstruction of thermal maxima/Reply

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

Sea surface temperature changes during May and August in the western Arabian Sea over the last 22 kyr: Implications as to shifting of the upwelling season

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

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