(Table 1) Geochemical analysis on sediment core CRP-3

Sediments and rocks recovered in CRP-3 coring operations contain minute amounts of organic matter (average 0.3% TOC). TOC contents and C:N ratios are zoned systematically: those rocks encountered at depths greater than 330 meters below sea floor (mbsf) contain less organic matter and have higher TOC...

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Bibliographic Details
Main Author: Kettler, Richard M
Format: Dataset
Language:English
Published: PANGAEA 2001
Subjects:
Cape Roberts Project
Carbon
organic
total
standard deviation
Core wireline system
CRP
CRP-3
CWS
Depth
bottom/max
sediment/rock
top/min
Element analyser CHNS-O
Carlo Erba EA1108
Nitrogen
Ross Sea
Sampling/drilling from ice
Sulfur
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.62127
https://doi.org/10.1594/PANGAEA.62127
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.62127
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.62127 2024-09-15T18:32:31+00:00 (Table 1) Geochemical analysis on sediment core CRP-3 Kettler, Richard M LATITUDE: -77.006000 * LONGITUDE: 163.719000 * DATE/TIME START: 1999-10-09T00:00:00 * DATE/TIME END: 1999-11-19T00:00:00 * MINIMUM DEPTH, sediment/rock: 8.140 m * MAXIMUM DEPTH, sediment/rock: 781.690 m 2001 text/tab-separated-values, 638 data points https://doi.pangaea.de/10.1594/PANGAEA.62127 https://doi.org/10.1594/PANGAEA.62127 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.62127 https://doi.org/10.1594/PANGAEA.62127 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Kettler, Richard M (2001): Results of whole-rock organic geochemical analyses of the CRP-3 drillcore, Victoria Land Basin, Antarctica. Terra Antartica, 8(3), 303-308, hdl:10013/epic.28241.d001 Cape Roberts Project Carbon organic total standard deviation Core wireline system CRP CRP-3 CWS Depth bottom/max sediment/rock top/min Element analyser CHNS-O Carlo Erba EA1108 Nitrogen Ross Sea Sampling/drilling from ice Sulfur dataset 2001 ftpangaea https://doi.org/10.1594/PANGAEA.62127 2024-08-27T23:49:29Z Sediments and rocks recovered in CRP-3 coring operations contain minute amounts of organic matter (average 0.3% TOC). TOC contents and C:N ratios are zoned systematically: those rocks encountered at depths greater than 330 meters below sea floor (mbsf) contain less organic matter and have higher TOC:N ratios (after correcting for inorganic N) than do shallower rocks. The only two samples that have TOC values greater than 1% also contain abundant granule to silt-sized particles of coal. The total sulphur contents of these rocks is very low and indicates either that only small amounts of deposited organic matter were labile, or that no source of reactive iron was present during diagenesis. Dataset Ross Sea PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(163.719000,163.719000,-77.006000,-77.006000)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Cape Roberts Project
Carbon
organic
total
standard deviation
Core wireline system
CRP
CRP-3
CWS
Depth
bottom/max
sediment/rock
top/min
Element analyser CHNS-O
Carlo Erba EA1108
Nitrogen
Ross Sea
Sampling/drilling from ice
Sulfur
spellingShingle Cape Roberts Project
Carbon
organic
total
standard deviation
Core wireline system
CRP
CRP-3
CWS
Depth
bottom/max
sediment/rock
top/min
Element analyser CHNS-O
Carlo Erba EA1108
Nitrogen
Ross Sea
Sampling/drilling from ice
Sulfur
Kettler, Richard M
(Table 1) Geochemical analysis on sediment core CRP-3
topic_facet Cape Roberts Project
Carbon
organic
total
standard deviation
Core wireline system
CRP
CRP-3
CWS
Depth
bottom/max
sediment/rock
top/min
Element analyser CHNS-O
Carlo Erba EA1108
Nitrogen
Ross Sea
Sampling/drilling from ice
Sulfur
description Sediments and rocks recovered in CRP-3 coring operations contain minute amounts of organic matter (average 0.3% TOC). TOC contents and C:N ratios are zoned systematically: those rocks encountered at depths greater than 330 meters below sea floor (mbsf) contain less organic matter and have higher TOC:N ratios (after correcting for inorganic N) than do shallower rocks. The only two samples that have TOC values greater than 1% also contain abundant granule to silt-sized particles of coal. The total sulphur contents of these rocks is very low and indicates either that only small amounts of deposited organic matter were labile, or that no source of reactive iron was present during diagenesis.
format Dataset
author Kettler, Richard M
author_facet Kettler, Richard M
author_sort Kettler, Richard M
title (Table 1) Geochemical analysis on sediment core CRP-3
title_short (Table 1) Geochemical analysis on sediment core CRP-3
title_full (Table 1) Geochemical analysis on sediment core CRP-3
title_fullStr (Table 1) Geochemical analysis on sediment core CRP-3
title_full_unstemmed (Table 1) Geochemical analysis on sediment core CRP-3
title_sort (table 1) geochemical analysis on sediment core crp-3
publisher PANGAEA
publishDate 2001
url https://doi.pangaea.de/10.1594/PANGAEA.62127
https://doi.org/10.1594/PANGAEA.62127
op_coverage LATITUDE: -77.006000 * LONGITUDE: 163.719000 * DATE/TIME START: 1999-10-09T00:00:00 * DATE/TIME END: 1999-11-19T00:00:00 * MINIMUM DEPTH, sediment/rock: 8.140 m * MAXIMUM DEPTH, sediment/rock: 781.690 m
long_lat ENVELOPE(163.719000,163.719000,-77.006000,-77.006000)
genre Ross Sea
genre_facet Ross Sea
op_source Supplement to: Kettler, Richard M (2001): Results of whole-rock organic geochemical analyses of the CRP-3 drillcore, Victoria Land Basin, Antarctica. Terra Antartica, 8(3), 303-308, hdl:10013/epic.28241.d001
op_relation https://doi.pangaea.de/10.1594/PANGAEA.62127
https://doi.org/10.1594/PANGAEA.62127
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1594/PANGAEA.62127
_version_ 1810474259855704064

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