Stable carbon and oxygen isotope record of planktonic foraminifera of ODP Hole 115-709C, supplement to: Shackleton, Nicholas J; Hall, Michael A (1990): Pliocene oxygen isotope stratigraphy of Hole 709C. In: Duncan, RA; Backmann, J; Peterson, LC; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 115, 529-538
A closely spaced (5-cm interval) oxygen isotope stratigraphy of planktonic foraminifers from Hole 709C was completed for most of the Pliocene and lowermost Pleistocene (around 4.6-1.4 Ma). This will contribute data to the future testing of the Matthews and Poore model of 1980, in which it was assume...
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ftdatacite:10.1594/pangaea.755884 2023-05-15T18:00:51+02:00 Stable carbon and oxygen isotope record of planktonic foraminifera of ODP Hole 115-709C, supplement to: Shackleton, Nicholas J; Hall, Michael A (1990): Pliocene oxygen isotope stratigraphy of Hole 709C. In: Duncan, RA; Backmann, J; Peterson, LC; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 115, 529-538 Shackleton, Nicholas J Hall, Michael A 1990 application/zip https://dx.doi.org/10.1594/pangaea.755884 https://doi.pangaea.de/10.1594/PANGAEA.755884 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://dx.doi.org/10.2973/odp.proc.sr.115.174.1990 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 CC-BY Drilling/drill rig Leg115 Joides Resolution Ocean Drilling Program ODP Supplementary Collection of Datasets Collection article 1990 ftdatacite https://doi.org/10.1594/pangaea.755884 https://doi.org/10.2973/odp.proc.sr.115.174.1990 2022-02-08T16:24:46Z A closely spaced (5-cm interval) oxygen isotope stratigraphy of planktonic foraminifers from Hole 709C was completed for most of the Pliocene and lowermost Pleistocene (around 4.6-1.4 Ma). This will contribute data to the future testing of the Matthews and Poore model of 1980, in which it was assumed that low-latitude sea-surface temperature has remained virtually constant as global climate evolved.Spectral analyses of the record by means of biostratigraphic time controls show a distinct peak at a period near 40 ka that is probably associated with the orbital obliquity cycle. Visual inspection of the record shows that intervals containing distinct 40-ka cycles are present in both lower and upper parts of the Pliocene even though a regular cycle cannot be followed throughout the entire 4-m.y. investigated. Article in Journal/Newspaper Planktonic foraminifera DataCite Metadata Store (German National Library of Science and Technology) Shackleton |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Drilling/drill rig Leg115 Joides Resolution Ocean Drilling Program ODP |
spellingShingle |
Drilling/drill rig Leg115 Joides Resolution Ocean Drilling Program ODP Shackleton, Nicholas J Hall, Michael A Stable carbon and oxygen isotope record of planktonic foraminifera of ODP Hole 115-709C, supplement to: Shackleton, Nicholas J; Hall, Michael A (1990): Pliocene oxygen isotope stratigraphy of Hole 709C. In: Duncan, RA; Backmann, J; Peterson, LC; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 115, 529-538 |
topic_facet |
Drilling/drill rig Leg115 Joides Resolution Ocean Drilling Program ODP |
description |
A closely spaced (5-cm interval) oxygen isotope stratigraphy of planktonic foraminifers from Hole 709C was completed for most of the Pliocene and lowermost Pleistocene (around 4.6-1.4 Ma). This will contribute data to the future testing of the Matthews and Poore model of 1980, in which it was assumed that low-latitude sea-surface temperature has remained virtually constant as global climate evolved.Spectral analyses of the record by means of biostratigraphic time controls show a distinct peak at a period near 40 ka that is probably associated with the orbital obliquity cycle. Visual inspection of the record shows that intervals containing distinct 40-ka cycles are present in both lower and upper parts of the Pliocene even though a regular cycle cannot be followed throughout the entire 4-m.y. investigated. |
format |
Article in Journal/Newspaper |
author |
Shackleton, Nicholas J Hall, Michael A |
author_facet |
Shackleton, Nicholas J Hall, Michael A |
author_sort |
Shackleton, Nicholas J |
title |
Stable carbon and oxygen isotope record of planktonic foraminifera of ODP Hole 115-709C, supplement to: Shackleton, Nicholas J; Hall, Michael A (1990): Pliocene oxygen isotope stratigraphy of Hole 709C. In: Duncan, RA; Backmann, J; Peterson, LC; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 115, 529-538 |
title_short |
Stable carbon and oxygen isotope record of planktonic foraminifera of ODP Hole 115-709C, supplement to: Shackleton, Nicholas J; Hall, Michael A (1990): Pliocene oxygen isotope stratigraphy of Hole 709C. In: Duncan, RA; Backmann, J; Peterson, LC; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 115, 529-538 |
title_full |
Stable carbon and oxygen isotope record of planktonic foraminifera of ODP Hole 115-709C, supplement to: Shackleton, Nicholas J; Hall, Michael A (1990): Pliocene oxygen isotope stratigraphy of Hole 709C. In: Duncan, RA; Backmann, J; Peterson, LC; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 115, 529-538 |
title_fullStr |
Stable carbon and oxygen isotope record of planktonic foraminifera of ODP Hole 115-709C, supplement to: Shackleton, Nicholas J; Hall, Michael A (1990): Pliocene oxygen isotope stratigraphy of Hole 709C. In: Duncan, RA; Backmann, J; Peterson, LC; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 115, 529-538 |
title_full_unstemmed |
Stable carbon and oxygen isotope record of planktonic foraminifera of ODP Hole 115-709C, supplement to: Shackleton, Nicholas J; Hall, Michael A (1990): Pliocene oxygen isotope stratigraphy of Hole 709C. In: Duncan, RA; Backmann, J; Peterson, LC; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 115, 529-538 |
title_sort |
stable carbon and oxygen isotope record of planktonic foraminifera of odp hole 115-709c, supplement to: shackleton, nicholas j; hall, michael a (1990): pliocene oxygen isotope stratigraphy of hole 709c. in: duncan, ra; backmann, j; peterson, lc; et al. (eds.), proceedings of the ocean drilling program, scientific results, college station, tx (ocean drilling program), 115, 529-538 |
publisher |
PANGAEA - Data Publisher for Earth & Environmental Science |
publishDate |
1990 |
url |
https://dx.doi.org/10.1594/pangaea.755884 https://doi.pangaea.de/10.1594/PANGAEA.755884 |
geographic |
Shackleton |
geographic_facet |
Shackleton |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_relation |
https://dx.doi.org/10.2973/odp.proc.sr.115.174.1990 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/pangaea.755884 https://doi.org/10.2973/odp.proc.sr.115.174.1990 |
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1766170121445834752 |