The effect of ocean alkalinity and carbon transfer on deep-sea carbonate ion concentration during the past five glacial cycles

Joanna Kerr, Rosalind Rickaby, Jimin Yu, Henry Elderfield, Aleksey Yu Sadekov

Research output: Contribution to journalArticle

13 Citations (Scopus)

Abstract

Glacial–interglacial deep Indo-Pacific carbonate ion concentration ([CO32−]) changes were mainly driven by two mechanisms that operated on different timescales: 1) a long-term increase during glaciation caused by a carbonate deposition reduction on shelves (i.e., the coral reef hypothesis), and 2) transient carbonate compensation responses to deep ocean carbon storage changes. To investigate these mechanisms, we have used benthic foraminiferal B/Ca to reconstruct deep-water [CO32−] in cores from the deep Indian and Equatorial Pacific Oceans during the past five glacial cycles. Based on our reconstructions, we suggest that the shelf-to-basin shift of carbonate deposition raised deep-water [CO32−], on average, by 7.3 ± 0.5 (SE) μmol/kg during glaciations. Oceanic carbon reorganisations during major climatic transitions caused deep-water [CO32−] deviations away from the long-term trend, and carbonate compensation processes subsequently acted to restore the ocean carbonate system to new steady state conditions. Deep-water [CO32−] showed similar patterns to sediment carbonate content (%CaCO3) records on glacial–interglacial timescales, suggesting that past seafloor %CaCO3 variations were dominated by deep-water carbonate preservation changes at our studied sites.

Original languageEnglish
Pages (from-to)42-53
Number of pages12
JournalEarth and Planetary Science Letters
Volume471
DOIs
Publication statusPublished - 1 Aug 2017

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alkalinity
Carbonates
Alkalinity
ion concentration
deep sea
carbonates
oceans
Carbon
Ions
deep water
carbonate
cycles
ion
carbon
ocean
Water
glaciation
shelves
timescale
carbonate system

Cite this

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title = "The effect of ocean alkalinity and carbon transfer on deep-sea carbonate ion concentration during the past five glacial cycles",
abstract = "Glacial–interglacial deep Indo-Pacific carbonate ion concentration ([CO32−]) changes were mainly driven by two mechanisms that operated on different timescales: 1) a long-term increase during glaciation caused by a carbonate deposition reduction on shelves (i.e., the coral reef hypothesis), and 2) transient carbonate compensation responses to deep ocean carbon storage changes. To investigate these mechanisms, we have used benthic foraminiferal B/Ca to reconstruct deep-water [CO32−] in cores from the deep Indian and Equatorial Pacific Oceans during the past five glacial cycles. Based on our reconstructions, we suggest that the shelf-to-basin shift of carbonate deposition raised deep-water [CO32−], on average, by 7.3 ± 0.5 (SE) μmol/kg during glaciations. Oceanic carbon reorganisations during major climatic transitions caused deep-water [CO32−] deviations away from the long-term trend, and carbonate compensation processes subsequently acted to restore the ocean carbonate system to new steady state conditions. Deep-water [CO32−] showed similar patterns to sediment carbonate content ({\%}CaCO3) records on glacial–interglacial timescales, suggesting that past seafloor {\%}CaCO3 variations were dominated by deep-water carbonate preservation changes at our studied sites.",
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The effect of ocean alkalinity and carbon transfer on deep-sea carbonate ion concentration during the past five glacial cycles. / Kerr, Joanna; Rickaby, Rosalind; Yu, Jimin; Elderfield, Henry; Sadekov, Aleksey Yu.

In: Earth and Planetary Science Letters, Vol. 471, 01.08.2017, p. 42-53.

Research output: Contribution to journalArticle

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