A synthesis of marine sediment core delta C data over the last 150 000 years
A synthesis of marine sediment core delta C data over the last 150 000 years
The isotopic composition of carbon, ?13C, in seawater is used in reconstructions of ocean circulation, marine productivity, air-sea gas exchange, and biosphere carbon storage. Here, a synthesis of ?13C measurements taken from foraminifera in marine sediment cores over the last 150 000 years is presented. The dataset comprises previously published and unpublished data from benthic and planktonic records throughout the global ocean. Data are placed on a common ?18O age scale suitable for examining orbital timescale variability but not millennial events, which are removed by a 10 ka filter. Error estimates account for the resolution and scatter of the original data, and uncertainty in the relationship between ?13C of calcite and of dissolved inorganic carbon (DIC) in seawater. This will assist comparison with ?13C of DIC output from models, which can be further improved using model outputs such as temperature, DIC concentration, and alkalinity to improve estimates of fractionation during calcite formation.
645-673
Oliver, K.I.C.
588b11c6-4d0c-4c59-94e2-255688474987
Hoogakker, B.A.A.
38e5c382-9641-487e-910d-402786d3d1c2
Crowhurst, S.
25f9eba3-9453-4d00-bd1e-1df6384b1876
Henderson, G.M.
1a310365-c407-4667-a617-b8473505a536
Rickaby, R.E.M.
bbc52831-4b8d-499e-9546-fb68fedb4604
Edwards, N.R.
e41b719b-784e-4748-acc4-6ccbc4643c7d
Elderfield, H.
fe3fae5f-0b4b-4741-a100-3aaa75568f06
2010
Oliver, K.I.C.
588b11c6-4d0c-4c59-94e2-255688474987
Hoogakker, B.A.A.
38e5c382-9641-487e-910d-402786d3d1c2
Crowhurst, S.
25f9eba3-9453-4d00-bd1e-1df6384b1876
Henderson, G.M.
1a310365-c407-4667-a617-b8473505a536
Rickaby, R.E.M.
bbc52831-4b8d-499e-9546-fb68fedb4604
Edwards, N.R.
e41b719b-784e-4748-acc4-6ccbc4643c7d
Elderfield, H.
fe3fae5f-0b4b-4741-a100-3aaa75568f06
Oliver, K.I.C., Hoogakker, B.A.A., Crowhurst, S., Henderson, G.M., Rickaby, R.E.M., Edwards, N.R. and Elderfield, H.
(2010)
A synthesis of marine sediment core delta C data over the last 150 000 years.
Climate of the Past, 6 (5), .
(doi:10.5194/cp-6-645-2010).
Abstract
The isotopic composition of carbon, ?13C, in seawater is used in reconstructions of ocean circulation, marine productivity, air-sea gas exchange, and biosphere carbon storage. Here, a synthesis of ?13C measurements taken from foraminifera in marine sediment cores over the last 150 000 years is presented. The dataset comprises previously published and unpublished data from benthic and planktonic records throughout the global ocean. Data are placed on a common ?18O age scale suitable for examining orbital timescale variability but not millennial events, which are removed by a 10 ka filter. Error estimates account for the resolution and scatter of the original data, and uncertainty in the relationship between ?13C of calcite and of dissolved inorganic carbon (DIC) in seawater. This will assist comparison with ?13C of DIC output from models, which can be further improved using model outputs such as temperature, DIC concentration, and alkalinity to improve estimates of fractionation during calcite formation.
This record has no associated files available for download.
More information
Published date: 2010
Organisations:
Ocean and Earth Science
Identifiers
Local EPrints ID: 169451
URI: http://eprints.soton.ac.uk/id/eprint/169451
ISSN: 1814-9332
PURE UUID: c4b93e47-fec1-4e17-a897-ef2985f6ce1b
Catalogue record
Date deposited: 15 Dec 2010 11:43
Last modified: 14 Mar 2024 02:20
Export record
Altmetrics
Contributors
Author:
B.A.A. Hoogakker
Author:
S. Crowhurst
Author:
G.M. Henderson
Author:
R.E.M. Rickaby
Author:
N.R. Edwards
Author:
H. Elderfield
Download statistics
Downloads from ePrints over the past year. Other digital versions may also be available to download e.g. from the publisher's website.
View more statistics