The chromium isotope system as a tracer of ocean and atmosphere redox / (Record no. 27160)

000 -LEADER
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006 - FIXED-LENGTH DATA ELEMENTS--ADDITIONAL MATERIAL CHARACTERISTICS--GENERAL INFORMATION
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007 - PHYSICAL DESCRIPTION FIXED FIELD--GENERAL INFORMATION
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008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION
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020 ## - INTERNATIONAL STANDARD BOOK NUMBER
International Standard Book Number 9781108870443 (ebook)
Qualifying information (R) Online Resouce
040 ## - CATALOGING SOURCE
Original cataloging agency UkCbUP
Language of cataloging eng
Description conventions rda
082 04 - DEWEY DECIMAL CLASSIFICATION NUMBER
Classification number 546.532
Edition number 23
100 1# - MAIN ENTRY--PERSONAL NAME
Personal name Bauer, Kohen W.,
245 14 - TITLE STATEMENT
Title The chromium isotope system as a tracer of ocean and atmosphere redox /
260 ## - PUBLICATION, DISTRIBUTION, ETC. (IMPRINT)
Place of publication, distribution, etc London
Name of publisher, distributor, etc Cambridge University Press
Date of publication, distribution, etc 2021
300 ## - PHYSICAL DESCRIPTION
Extent 1 online resource (26 pages) :
Other physical details digital, PDF file(s).
490 1# - SERIES STATEMENT
Series statement Cambridge elements. Elements in geochemical tracers in Earth system science,
500 ## - GENERAL NOTE
General note Title from publisher's bibliographic system (viewed on 05 Feb 2021).
520 ## - SUMMARY, ETC.
Summary, etc The stable chromium (Cr) isotope system has emerged over the past decade as a new tool to track changes in the amount of oxygen in earth's ocean-atmosphere system. Much of the initial foundation for using Cr isotopes (δ53Cr) as a paleoredox proxy has required recent revision. However, the basic idea behind using Cr isotopes as redox tracers is straightforward-the largest isotope fractionations are redox-dependent and occur during partial reduction of Cr(VI). As such, Cr isotopic signatures can provide novel insights into Cr redox cycling in both marine and terrestrial settings. Critically, the Cr isotope system-unlike many other trace metal proxies-can respond to short-term redox perturbations (e.g., on timescales characteristic of Pleistocene glacial-interglacial cycles). The Cr isotope system can also be used to probe the earth's long-term atmospheric oxygenation, pointing towards low but likely dynamic oxygen levels for the majority of Earth's history.
650 #0 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name as entry element Chromium
General subdivision Isotopes.
Topical term or geographic name as entry element Oxidation-reduction reaction.
Topical term or geographic name as entry element Environmental geochemistry.
700 1# - ADDED ENTRY--PERSONAL NAME
Personal name Planavsky, Noah J.,
Relator term author.
Personal name Reinhard, Christopher T.,
Relator term author.
Personal name Cole, Devon B.,
Relator term author.
776 08 - ADDITIONAL PHYSICAL FORM ENTRY
Display text Print version:
International Standard Book Number 9781108792578
830 #0 - SERIES ADDED ENTRY--UNIFORM TITLE
Uniform title Cambridge elements.
Name of part/section of a work Elements in geochemical tracers in Earth system science,
856 40 - ELECTRONIC LOCATION AND ACCESS
Uniform Resource Identifier <a href="https://doi.org/10.1017/9781108870443">https://doi.org/10.1017/9781108870443</a>
942 ## - ADDED ENTRY ELEMENTS (KOHA)
Source of classification or shelving scheme
Item type E-Book

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