Characterising the intermediate depth waters of the Pacific Ocean using δ 13 C and other geochemical tracers

Evidence from geochemical tracers (salinity, oxygen, silicate, nutrients, alkalinity, dissolved inorganic carbon (DIC), carbon isotopes (δ13CDIC) and radiocarbon (Δ14C)) collected during the Pacific Ocean World Ocean Circulation Experiment (WOCE) voyage

Bibliographic Details
Published in:Deep Sea Research Part I: Oceanographic Research Papers
Main Authors: Bostock, Helen, Opdyke, Bradley, Williams, Michael J.M.
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier
Subjects:
Keywords: Antarctic intermediate waters
Benthic foraminifera
Carbon isotopes
Conservative tracers
Deep Water
Diatom production
Dissolved inorganic carbon
Eastern equatorial Pacific
Equatorial Pacific
Four-core
Geochemical properties
Geochemical proxies
d13C
d14C
AAIW
Equatorial intermediate waters
Geochemical tracers
Intermediate depth waters
NPIW
Pacific Ocean
Antarctic
Pacific
Antarc*
Online Access:http://hdl.handle.net/1885/35209
https://doi.org/10.1016/j.dsr.2010.04.005
https://openresearch-repository.anu.edu.au/bitstream/1885/35209/5/Bostock_et_al_2010.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/35209/7/01_Bostock_Characterising_the_2010.pdf.jpg
Description
Summary:Evidence from geochemical tracers (salinity, oxygen, silicate, nutrients, alkalinity, dissolved inorganic carbon (DIC), carbon isotopes (δ13CDIC) and radiocarbon (Δ14C)) collected during the Pacific Ocean World Ocean Circulation Experiment (WOCE) voyage

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