Pb concentrations, Pb isotopic composition, and amount of metalliferous components in pelagic sediments from the Pacific Ocean
The amount of lead annually transferred from oceanic crust to metalliferous sediments was estimated in order to test the hypothesis that a non-magmatic flux of lead causes the Pb surplus in the continental crust. A Pb surplus has been inferred from global crust-mantle lead mass balances derived from...
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Format: | Dataset |
Language: | English |
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PANGAEA
1994
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.712126 https://doi.org/10.1594/PANGAEA.712126 |
id |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.712126 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
16-161A 16-162 19-183 34-319 35-323 5-37 5-39 85-574C 8-74 8-75 91-596 92-597 9-77B Antarctic Ocean/PLAIN Components indeterminata Deep Sea Drilling Project Distance relative DRILL Drilling/drill rig DSDP DSDP/ODP/IODP sample designation Elevation of event Event label Glomar Challenger Latitude of event Lead Lead-206/Lead-204 ratio Lead-207/Lead-204 ratio Lead-208/Lead-204 ratio Leg16 Leg19 Leg34 Leg35 Leg5 Leg8 Leg85 Leg9 Leg91 Leg92 Longitude of event Mass spectrometer Finnigan MAT 251 North Pacific/CONT RISE North Pacific/HILL North Pacific/PLAIN North Pacific/TROUGH Sample code/label South Pacific South Pacific/BASIN South Pacific/CONT RISE |
spellingShingle |
16-161A 16-162 19-183 34-319 35-323 5-37 5-39 85-574C 8-74 8-75 91-596 92-597 9-77B Antarctic Ocean/PLAIN Components indeterminata Deep Sea Drilling Project Distance relative DRILL Drilling/drill rig DSDP DSDP/ODP/IODP sample designation Elevation of event Event label Glomar Challenger Latitude of event Lead Lead-206/Lead-204 ratio Lead-207/Lead-204 ratio Lead-208/Lead-204 ratio Leg16 Leg19 Leg34 Leg35 Leg5 Leg8 Leg85 Leg9 Leg91 Leg92 Longitude of event Mass spectrometer Finnigan MAT 251 North Pacific/CONT RISE North Pacific/HILL North Pacific/PLAIN North Pacific/TROUGH Sample code/label South Pacific South Pacific/BASIN South Pacific/CONT RISE Peucker-Ehrenbrink, Bernhard Hofmann, Albrecht W Hart, Stanley R Pb concentrations, Pb isotopic composition, and amount of metalliferous components in pelagic sediments from the Pacific Ocean |
topic_facet |
16-161A 16-162 19-183 34-319 35-323 5-37 5-39 85-574C 8-74 8-75 91-596 92-597 9-77B Antarctic Ocean/PLAIN Components indeterminata Deep Sea Drilling Project Distance relative DRILL Drilling/drill rig DSDP DSDP/ODP/IODP sample designation Elevation of event Event label Glomar Challenger Latitude of event Lead Lead-206/Lead-204 ratio Lead-207/Lead-204 ratio Lead-208/Lead-204 ratio Leg16 Leg19 Leg34 Leg35 Leg5 Leg8 Leg85 Leg9 Leg91 Leg92 Longitude of event Mass spectrometer Finnigan MAT 251 North Pacific/CONT RISE North Pacific/HILL North Pacific/PLAIN North Pacific/TROUGH Sample code/label South Pacific South Pacific/BASIN South Pacific/CONT RISE |
description |
The amount of lead annually transferred from oceanic crust to metalliferous sediments was estimated in order to test the hypothesis that a non-magmatic flux of lead causes the Pb surplus in the continental crust. A Pb surplus has been inferred from global crust-mantle lead mass balances derived from lead concentration correlations with other trace elements and from lead isotope systematics in oceanic basalts. DSDP/ODP data on the amount of metalliferous sediments in the Pacific Ocean and along a South Atlantic traverse are used to calculate the mean worldwide thickness of 3 (+/-1) m for purely metalliferous sediment componens. Lead isotope ratios of 39 metalliferous sediments from the Pacific define mixing lines between continent-derived (seawater) and mantle-derived (basaltic) lead, with the most metal-rich sediments usually having the most mantle-like Pb isotope composition. We used this isotope correlation and the Pb content of the 39 metalliferous sediments to derive an estimate of 130 (+/-70) µg/g for the concentration of mantle-derived lead in the purely metalliferous end-member. Mass balance calculations show that at least 12 (+/-8)% of the lead, annually transferred from upper mantle to oceanic crust at the ocean ridges, is leached out by hydrothermal processes and re-deposited in marine sediments. If all of the metalliferous lead is ultimately transferred to the continental crust during subduction, the annual flux of this lead from mantle to continental crust is 2.6 (+/-2.0) * 10**6 kg. Assuming this transfer rate to be proportional to the rate of oceanic plate production, one can fit the lead transfer to models of plate production rate variations through time. Integrating over 4 Ga, hydrothermal lead transfer to the continental crust accounts for a significant portion of the Pb surplus in the continental crust. It therefore appears to be one of the main reasons for the anomalous behavior of lead in the global crust-mantle system. |
format |
Dataset |
author |
Peucker-Ehrenbrink, Bernhard Hofmann, Albrecht W Hart, Stanley R |
author_facet |
Peucker-Ehrenbrink, Bernhard Hofmann, Albrecht W Hart, Stanley R |
author_sort |
Peucker-Ehrenbrink, Bernhard |
title |
Pb concentrations, Pb isotopic composition, and amount of metalliferous components in pelagic sediments from the Pacific Ocean |
title_short |
Pb concentrations, Pb isotopic composition, and amount of metalliferous components in pelagic sediments from the Pacific Ocean |
title_full |
Pb concentrations, Pb isotopic composition, and amount of metalliferous components in pelagic sediments from the Pacific Ocean |
title_fullStr |
Pb concentrations, Pb isotopic composition, and amount of metalliferous components in pelagic sediments from the Pacific Ocean |
title_full_unstemmed |
Pb concentrations, Pb isotopic composition, and amount of metalliferous components in pelagic sediments from the Pacific Ocean |
title_sort |
pb concentrations, pb isotopic composition, and amount of metalliferous components in pelagic sediments from the pacific ocean |
publisher |
PANGAEA |
publishDate |
1994 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.712126 https://doi.org/10.1594/PANGAEA.712126 |
op_coverage |
MEDIAN LATITUDE: 1.421215 * MEDIAN LONGITUDE: -134.873808 * SOUTH-BOUND LATITUDE: -63.680700 * WEST-BOUND LONGITUDE: -165.654500 * NORTH-BOUND LATITUDE: 52.571700 * EAST-BOUND LONGITUDE: -97.994800 * DATE/TIME START: 1969-05-10T00:00:00 * DATE/TIME END: 1983-03-02T00:00:00 * MINIMUM ELEVATION: -5701.0 m * MAXIMUM ELEVATION: -4166.0 m |
long_lat |
ENVELOPE(-165.654500,-97.994800,52.571700,-63.680700) |
geographic |
Antarctic Antarctic Ocean Pacific |
geographic_facet |
Antarctic Antarctic Ocean Pacific |
genre |
Antarc* Antarctic Antarctic Ocean |
genre_facet |
Antarc* Antarctic Antarctic Ocean |
op_source |
Supplement to: Peucker-Ehrenbrink, Bernhard; Hofmann, Albrecht W; Hart, Stanley R (1994): Hydrothermal lead transfer from mantle to continental crust: the role of metalliferous sediments. Earth and Planetary Science Letters, 125(1-4), 129-142, https://doi.org/10.1016/0012-821X(94)90211-9 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.712126 https://doi.org/10.1594/PANGAEA.712126 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.712126 https://doi.org/10.1016/0012-821X(94)90211-9 |
_version_ |
1766019374024491008 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.712126 2023-05-15T13:31:38+02:00 Pb concentrations, Pb isotopic composition, and amount of metalliferous components in pelagic sediments from the Pacific Ocean Peucker-Ehrenbrink, Bernhard Hofmann, Albrecht W Hart, Stanley R MEDIAN LATITUDE: 1.421215 * MEDIAN LONGITUDE: -134.873808 * SOUTH-BOUND LATITUDE: -63.680700 * WEST-BOUND LONGITUDE: -165.654500 * NORTH-BOUND LATITUDE: 52.571700 * EAST-BOUND LONGITUDE: -97.994800 * DATE/TIME START: 1969-05-10T00:00:00 * DATE/TIME END: 1983-03-02T00:00:00 * MINIMUM ELEVATION: -5701.0 m * MAXIMUM ELEVATION: -4166.0 m 1994-02-03 text/tab-separated-values, 312 data points https://doi.pangaea.de/10.1594/PANGAEA.712126 https://doi.org/10.1594/PANGAEA.712126 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.712126 https://doi.org/10.1594/PANGAEA.712126 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Peucker-Ehrenbrink, Bernhard; Hofmann, Albrecht W; Hart, Stanley R (1994): Hydrothermal lead transfer from mantle to continental crust: the role of metalliferous sediments. Earth and Planetary Science Letters, 125(1-4), 129-142, https://doi.org/10.1016/0012-821X(94)90211-9 16-161A 16-162 19-183 34-319 35-323 5-37 5-39 85-574C 8-74 8-75 91-596 92-597 9-77B Antarctic Ocean/PLAIN Components indeterminata Deep Sea Drilling Project Distance relative DRILL Drilling/drill rig DSDP DSDP/ODP/IODP sample designation Elevation of event Event label Glomar Challenger Latitude of event Lead Lead-206/Lead-204 ratio Lead-207/Lead-204 ratio Lead-208/Lead-204 ratio Leg16 Leg19 Leg34 Leg35 Leg5 Leg8 Leg85 Leg9 Leg91 Leg92 Longitude of event Mass spectrometer Finnigan MAT 251 North Pacific/CONT RISE North Pacific/HILL North Pacific/PLAIN North Pacific/TROUGH Sample code/label South Pacific South Pacific/BASIN South Pacific/CONT RISE Dataset 1994 ftpangaea https://doi.org/10.1594/PANGAEA.712126 https://doi.org/10.1016/0012-821X(94)90211-9 2023-01-20T08:47:12Z The amount of lead annually transferred from oceanic crust to metalliferous sediments was estimated in order to test the hypothesis that a non-magmatic flux of lead causes the Pb surplus in the continental crust. A Pb surplus has been inferred from global crust-mantle lead mass balances derived from lead concentration correlations with other trace elements and from lead isotope systematics in oceanic basalts. DSDP/ODP data on the amount of metalliferous sediments in the Pacific Ocean and along a South Atlantic traverse are used to calculate the mean worldwide thickness of 3 (+/-1) m for purely metalliferous sediment componens. Lead isotope ratios of 39 metalliferous sediments from the Pacific define mixing lines between continent-derived (seawater) and mantle-derived (basaltic) lead, with the most metal-rich sediments usually having the most mantle-like Pb isotope composition. We used this isotope correlation and the Pb content of the 39 metalliferous sediments to derive an estimate of 130 (+/-70) µg/g for the concentration of mantle-derived lead in the purely metalliferous end-member. Mass balance calculations show that at least 12 (+/-8)% of the lead, annually transferred from upper mantle to oceanic crust at the ocean ridges, is leached out by hydrothermal processes and re-deposited in marine sediments. If all of the metalliferous lead is ultimately transferred to the continental crust during subduction, the annual flux of this lead from mantle to continental crust is 2.6 (+/-2.0) * 10**6 kg. Assuming this transfer rate to be proportional to the rate of oceanic plate production, one can fit the lead transfer to models of plate production rate variations through time. Integrating over 4 Ga, hydrothermal lead transfer to the continental crust accounts for a significant portion of the Pb surplus in the continental crust. It therefore appears to be one of the main reasons for the anomalous behavior of lead in the global crust-mantle system. Dataset Antarc* Antarctic Antarctic Ocean PANGAEA - Data Publisher for Earth & Environmental Science Antarctic Antarctic Ocean Pacific ENVELOPE(-165.654500,-97.994800,52.571700,-63.680700) |