Eocene through Pleistocene planktonic foraminifera off Peru ...

Planktonic foraminifers were studied from 213 samples collected during Leg 112 at 10 sites located on the continental shelf and slope off Peru. Because planktonic foraminifers occur discontinuously downcore, detailed biostratigraphic zonation was not defined. However, it was possible to distinguish...

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Bibliographic Details
Main Author: Ibaraki, Masako
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1990
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.745615
https://doi.pangaea.de/10.1594/PANGAEA.745615
id ftdatacite:10.1594/pangaea.745615
record_format openpolar
spelling ftdatacite:10.1594/pangaea.745615 2024-09-15T18:31:03+00:00 Eocene through Pleistocene planktonic foraminifera off Peru ... Ibaraki, Masako 1990 application/zip https://dx.doi.org/10.1594/pangaea.745615 https://doi.pangaea.de/10.1594/PANGAEA.745615 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.112.197.1990 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg112 Joides Resolution Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 1990 ftdatacite https://doi.org/10.1594/pangaea.74561510.2973/odp.proc.sr.112.197.1990 2024-08-01T10:53:02Z Planktonic foraminifers were studied from 213 samples collected during Leg 112 at 10 sites located on the continental shelf and slope off Peru. Because planktonic foraminifers occur discontinuously downcore, detailed biostratigraphic zonation was not defined. However, it was possible to distinguish early and middle Eocene, early and late Miocene, Pliocene, and Pleistocene sediments on the basis of the planktonic foraminifers. The oldest sediments of Zone P6 of early Eocene age were obtained from the basal part of Hole 688E, which was penetrated to 779.0 m below seafloor (bsf). A biosiliceous facies of the area predominates above the N6-N7 zonal interval of early Miocene age.All sites are within the present coastal upwelling area off Peru, and many of the late Pliocene and Pleistocene assemblages are similar to those that are characteristic of modern upwelling areas. The core samples differ, however, by having a predominance of cold-water elements, such as Neogloboquadrina incompta and N. pachyderma. ... : Supplement to: Ibaraki, Masako (1990): Eocene through Pleistocene planktonic foraminifers off Peru, Leg 112 - biostratigraphy and paleoceanography. In: Suess, E; von Huene, R; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 112, 239-262 ... Article in Journal/Newspaper Planktonic foraminifera DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Leg112
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Drilling/drill rig
Leg112
Joides Resolution
Ocean Drilling Program ODP
Ibaraki, Masako
Eocene through Pleistocene planktonic foraminifera off Peru ...
topic_facet Drilling/drill rig
Leg112
Joides Resolution
Ocean Drilling Program ODP
description Planktonic foraminifers were studied from 213 samples collected during Leg 112 at 10 sites located on the continental shelf and slope off Peru. Because planktonic foraminifers occur discontinuously downcore, detailed biostratigraphic zonation was not defined. However, it was possible to distinguish early and middle Eocene, early and late Miocene, Pliocene, and Pleistocene sediments on the basis of the planktonic foraminifers. The oldest sediments of Zone P6 of early Eocene age were obtained from the basal part of Hole 688E, which was penetrated to 779.0 m below seafloor (bsf). A biosiliceous facies of the area predominates above the N6-N7 zonal interval of early Miocene age.All sites are within the present coastal upwelling area off Peru, and many of the late Pliocene and Pleistocene assemblages are similar to those that are characteristic of modern upwelling areas. The core samples differ, however, by having a predominance of cold-water elements, such as Neogloboquadrina incompta and N. pachyderma. ... : Supplement to: Ibaraki, Masako (1990): Eocene through Pleistocene planktonic foraminifers off Peru, Leg 112 - biostratigraphy and paleoceanography. In: Suess, E; von Huene, R; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 112, 239-262 ...
format Article in Journal/Newspaper
author Ibaraki, Masako
author_facet Ibaraki, Masako
author_sort Ibaraki, Masako
title Eocene through Pleistocene planktonic foraminifera off Peru ...
title_short Eocene through Pleistocene planktonic foraminifera off Peru ...
title_full Eocene through Pleistocene planktonic foraminifera off Peru ...
title_fullStr Eocene through Pleistocene planktonic foraminifera off Peru ...
title_full_unstemmed Eocene through Pleistocene planktonic foraminifera off Peru ...
title_sort eocene through pleistocene planktonic foraminifera off peru ...
publisher PANGAEA
publishDate 1990
url https://dx.doi.org/10.1594/pangaea.745615
https://doi.pangaea.de/10.1594/PANGAEA.745615
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_relation https://dx.doi.org/10.2973/odp.proc.sr.112.197.1990
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.74561510.2973/odp.proc.sr.112.197.1990
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