about
Biogeochemical significance of pelagic ecosystem function: an end-Cretaceous case study.Boron isotope evidence for oceanic carbon dioxide leakage during the last deglaciation.Boron isotopes and B/Ca in benthic foraminifera: Proxies for the deep ocean carbonate systemStructural limitations in deriving accurate U-series ages from calcitic cold-water corals contrast with robust coral radiocarbon and Mg/Ca systematicsDistribution and ecology of planktic foraminifera in the North Pacific: Implications for paleo-reconstructionsReconstructing Ocean pH with Boron Isotopes in ForaminiferaCalibration of the boron isotope proxy in the planktonic foraminifera Globigerinoides ruber for use in palaeo-CO2 reconstructionInterlaboratory comparison of boron isotope analyses of boric acid, seawater and marine CaCO3 by MC-ICPMS and NTIMSResponses of the deep ocean carbonate system to carbon reorganization during the Last Glacial–interglacial cycleThe evolution of pCO2, ice volume and climate during the middle MioceneRapid ocean acidification and protracted Earth system recovery followed the end-Cretaceous Chicxulub impact
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P50
description
onderzoeker
@nl
researcher
@en
հետազոտող
@hy
name
James W.B. Rae
@ast
James W.B. Rae
@en
James W.B. Rae
@es
James W.B. Rae
@nl
type
label
James W.B. Rae
@ast
James W.B. Rae
@en
James W.B. Rae
@es
James W.B. Rae
@nl
prefLabel
James W.B. Rae
@ast
James W.B. Rae
@en
James W.B. Rae
@es
James W.B. Rae
@nl
P108
P1053
R-3812-2017
P106
P1153
36454830900
P21
P31
P3829
P496
0000-0003-3904-2526