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dc.contributor.authorGreenop, Rosanna
dc.contributor.authorHain, Mathis P.
dc.contributor.authorSosdian, Sindia M.
dc.contributor.authorOliver, Kevin I. C.
dc.contributor.authorGoodwin, Philip
dc.contributor.authorChalk, Thomas B.
dc.contributor.authorLear, Caroline H.
dc.contributor.authorWilson, Paul A.
dc.contributor.authorFoster, Gavin L.
dc.identifier.citationGreenop , R , Hain , M P , Sosdian , S M , Oliver , K I C , Goodwin , P , Chalk , T B , Lear , C H , Wilson , P A & Foster , G L 2017 , ' A record of Neogene seawater δ 11 B reconstructed from paired δ 11 B analyses on benthic and planktic foraminifera ' , Climate of the Past , vol. 13 , no. 2 , pp. 149-170 .
dc.identifier.otherPURE: 249348278
dc.identifier.otherPURE UUID: 2f56b93a-7b6a-4d59-9e97-9024e2e5e86e
dc.identifier.otherScopus: 85014011888
dc.identifier.otherWOS: 000395328200001
dc.descriptionThe work was supported by NERC grants NE/I006176/1 (Gavin L. Foster and Caroline H. Lear), NE/H006273/1 (Gavin L. Foster), NE/I006168/1 and NE/K014137/1 and a Royal Society Research Merit Award (Paul A. Wilson), a NERC Independent Research Fellowship NE/K00901X/1 (Mathis P. Hain) and a NERC studentship (Rosanna Greenop).en
dc.description.abstractThe boron isotope composition (δ11B) of foraminiferal calcite reflects the pH and the boron isotope composition of the seawater the foraminifer grew in. For pH reconstructions, the δ11B of seawater must therefore be known, but information on this parameter is limited. Here we reconstruct Neogene seawater δ11B based on the δ11B difference between paired measurements of planktic and benthic foraminifera and an estimate of the coeval water column pH gradient from their δ13C values. Carbon cycle model simulations underscore that the ΔpH-Δδ13C relationship is relatively insensitive to ocean and carbon cycle changes, validating our approach. Our reconstructions suggest that δ11Bsw was ∼37.5‰ during the early and middle Miocene (roughly 23-12 Ma) and rapidly increased during the late Miocene (between 12 and 5 Ma) towards the modern value of 39.61 ‰. Strikingly, this pattern is similar to the evolution of the seawater isotope composition of Mg, Li and Ca, suggesting a common forcing mechanism. Based on the observed direction of change, we hypothesize that an increase in secondary mineral formation during continental weathering affected the isotope composition of riverine input to the ocean since 14 Ma.
dc.relation.ispartofClimate of the Pasten
dc.rights© Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License.en
dc.subjectGE Environmental Sciencesen
dc.subjectGC Oceanographyen
dc.subjectGlobal and Planetary Changeen
dc.titleA record of Neogene seawater δ11B reconstructed from paired δ11B analyses on benthic and planktic foraminiferaen
dc.typeJournal articleen
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews. Earth and Environmental Sciencesen
dc.contributor.institutionUniversity of St Andrews. St Andrews Isotope Geochemistryen
dc.contributor.institutionUniversity of St Andrews. School of Geography and Geosciencesen
dc.description.statusPeer revieweden

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