Sr, C and O isotope ratios of Neogene sediments from DSDP Hole 38-341, Voring Plateau ...
The Neogene sediments from DSDP site 341 on the Voring Plateau, Norwegian Sea, contain a thin glauconitic pellet-bearing subunit, which separates underlying pelagic clays from overlying glacial-marine sediments. Oxygen isotope measurements of benthic foraminifera show a delta18O shift of + 1 per mil...
Main Authors: | , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
PANGAEA
1986
|
Subjects: | |
Online Access: | https://dx.doi.org/10.1594/pangaea.714252 https://doi.pangaea.de/10.1594/PANGAEA.714252 |
id |
ftdatacite:10.1594/pangaea.714252 |
---|---|
record_format |
openpolar |
spelling |
ftdatacite:10.1594/pangaea.714252 2024-09-15T18:26:49+00:00 Sr, C and O isotope ratios of Neogene sediments from DSDP Hole 38-341, Voring Plateau ... Smalley, P Craig Nordaa, A Raheim, A 1986 application/zip https://dx.doi.org/10.1594/pangaea.714252 https://doi.pangaea.de/10.1594/PANGAEA.714252 en eng PANGAEA https://dx.doi.org/10.1016/0012-821x(86)90004-x Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg38 Glomar Challenger Deep Sea Drilling Project DSDP article Collection Supplementary Publication Series of Datasets 1986 ftdatacite https://doi.org/10.1594/pangaea.71425210.1016/0012-821x(86)90004-x 2024-08-01T10:55:41Z The Neogene sediments from DSDP site 341 on the Voring Plateau, Norwegian Sea, contain a thin glauconitic pellet-bearing subunit, which separates underlying pelagic clays from overlying glacial-marine sediments. Oxygen isotope measurements of benthic foraminifera show a delta18O shift of + 1 per mil during deposition of this subunit, probably a combined effect of a drop in bottom water temperature and a rise in seawater delta18O. The chronology of this sedimentological and O isotope transition is, however, poorly constrained by fossil evidence.Rb-Sr dating of glauconitic pellets indicates that the lower part of the glauconitic subunit was deposited 11.6 +/- 0.2 Ma ago. Further geochronological evidence, derived from the Sr and C isotopic compositions of foraminifera compared with known seawater-time variations, indicates that the lower pelagic clays are early to middle Miocene, deposited at a mean rate of ~15 m/Ma. The glauconitic subunit contains part of the middle Miocene and probably all of the late ... : Supplement to: Smalley, P Craig; Nordaa, A; Raheim, A (1986): Geochronology and paleothermometry of Neogene sediments from the Voring Plateau using Sr, C and O isotopes. Earth and Planetary Science Letters, 78(4), 368-378 ... Article in Journal/Newspaper Norwegian Sea DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Drilling/drill rig Leg38 Glomar Challenger Deep Sea Drilling Project DSDP |
spellingShingle |
Drilling/drill rig Leg38 Glomar Challenger Deep Sea Drilling Project DSDP Smalley, P Craig Nordaa, A Raheim, A Sr, C and O isotope ratios of Neogene sediments from DSDP Hole 38-341, Voring Plateau ... |
topic_facet |
Drilling/drill rig Leg38 Glomar Challenger Deep Sea Drilling Project DSDP |
description |
The Neogene sediments from DSDP site 341 on the Voring Plateau, Norwegian Sea, contain a thin glauconitic pellet-bearing subunit, which separates underlying pelagic clays from overlying glacial-marine sediments. Oxygen isotope measurements of benthic foraminifera show a delta18O shift of + 1 per mil during deposition of this subunit, probably a combined effect of a drop in bottom water temperature and a rise in seawater delta18O. The chronology of this sedimentological and O isotope transition is, however, poorly constrained by fossil evidence.Rb-Sr dating of glauconitic pellets indicates that the lower part of the glauconitic subunit was deposited 11.6 +/- 0.2 Ma ago. Further geochronological evidence, derived from the Sr and C isotopic compositions of foraminifera compared with known seawater-time variations, indicates that the lower pelagic clays are early to middle Miocene, deposited at a mean rate of ~15 m/Ma. The glauconitic subunit contains part of the middle Miocene and probably all of the late ... : Supplement to: Smalley, P Craig; Nordaa, A; Raheim, A (1986): Geochronology and paleothermometry of Neogene sediments from the Voring Plateau using Sr, C and O isotopes. Earth and Planetary Science Letters, 78(4), 368-378 ... |
format |
Article in Journal/Newspaper |
author |
Smalley, P Craig Nordaa, A Raheim, A |
author_facet |
Smalley, P Craig Nordaa, A Raheim, A |
author_sort |
Smalley, P Craig |
title |
Sr, C and O isotope ratios of Neogene sediments from DSDP Hole 38-341, Voring Plateau ... |
title_short |
Sr, C and O isotope ratios of Neogene sediments from DSDP Hole 38-341, Voring Plateau ... |
title_full |
Sr, C and O isotope ratios of Neogene sediments from DSDP Hole 38-341, Voring Plateau ... |
title_fullStr |
Sr, C and O isotope ratios of Neogene sediments from DSDP Hole 38-341, Voring Plateau ... |
title_full_unstemmed |
Sr, C and O isotope ratios of Neogene sediments from DSDP Hole 38-341, Voring Plateau ... |
title_sort |
sr, c and o isotope ratios of neogene sediments from dsdp hole 38-341, voring plateau ... |
publisher |
PANGAEA |
publishDate |
1986 |
url |
https://dx.doi.org/10.1594/pangaea.714252 https://doi.pangaea.de/10.1594/PANGAEA.714252 |
genre |
Norwegian Sea |
genre_facet |
Norwegian Sea |
op_relation |
https://dx.doi.org/10.1016/0012-821x(86)90004-x |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.71425210.1016/0012-821x(86)90004-x |
_version_ |
1810467454025990144 |