Cenozoic silicoflagellates and ebridians from ODP Leg 113 ...

Silicoflagellates are present at ODP 113 Sites 689, 690, 693, 695, 696, and 697. These are generally Neogene in age except for Oligocene and Eocene silicoflagellates and ebridians at Sites 689, 690, and 693, and Lower Cretaceous (Albian) silicoflagellates at Site 693 (the latter are described in McC...

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Main Authors: McCartney, Kevin, Wise, Sherwood W
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1990
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.753479
https://doi.pangaea.de/10.1594/PANGAEA.753479
id ftdatacite:10.1594/pangaea.753479
record_format openpolar
spelling ftdatacite:10.1594/pangaea.753479 2024-09-15T17:47:16+00:00 Cenozoic silicoflagellates and ebridians from ODP Leg 113 ... McCartney, Kevin Wise, Sherwood W 1990 application/zip https://dx.doi.org/10.1594/pangaea.753479 https://doi.pangaea.de/10.1594/PANGAEA.753479 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.113.142.1990 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg113 Joides Resolution Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 1990 ftdatacite https://doi.org/10.1594/pangaea.75347910.2973/odp.proc.sr.113.142.1990 2024-08-01T10:54:44Z Silicoflagellates are present at ODP 113 Sites 689, 690, 693, 695, 696, and 697. These are generally Neogene in age except for Oligocene and Eocene silicoflagellates and ebridians at Sites 689, 690, and 693, and Lower Cretaceous (Albian) silicoflagellates at Site 693 (the latter are described in McCartney, et al., this volume). The uppermost Miocenelowermost Pliocene of most sites contains an interesting assemblage of Distephanus speculum speculum that lack apical rings (the "pseudofibula plexus"). These co-occur with the youngest ice-rafted sediments deposited during the late Miocene-early Pliocene West Antarctic glaciations and are discussed in detail to show the variability within this group. We believe that these variations resulted from environmental stress, the precise nature of which is still undetermined. The "pseudofibulid" condition has developed at several different times during the Cenozoic within the Distephanus speculum lineage to produce such ecophenotypes. One new form from the "pseudofibula ... : Supplement to: McCartney, Kevin; Wise, Sherwood W (1990): Cenozoic silicoflagellates and ebridians from ODP Leg 113: biostratigraphy and notes on morphologic variability. In: Barker, PF; Kennett, JP; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 113, 729-760 ... Article in Journal/Newspaper Antarc* Antarctic DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Leg113
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Drilling/drill rig
Leg113
Joides Resolution
Ocean Drilling Program ODP
McCartney, Kevin
Wise, Sherwood W
Cenozoic silicoflagellates and ebridians from ODP Leg 113 ...
topic_facet Drilling/drill rig
Leg113
Joides Resolution
Ocean Drilling Program ODP
description Silicoflagellates are present at ODP 113 Sites 689, 690, 693, 695, 696, and 697. These are generally Neogene in age except for Oligocene and Eocene silicoflagellates and ebridians at Sites 689, 690, and 693, and Lower Cretaceous (Albian) silicoflagellates at Site 693 (the latter are described in McCartney, et al., this volume). The uppermost Miocenelowermost Pliocene of most sites contains an interesting assemblage of Distephanus speculum speculum that lack apical rings (the "pseudofibula plexus"). These co-occur with the youngest ice-rafted sediments deposited during the late Miocene-early Pliocene West Antarctic glaciations and are discussed in detail to show the variability within this group. We believe that these variations resulted from environmental stress, the precise nature of which is still undetermined. The "pseudofibulid" condition has developed at several different times during the Cenozoic within the Distephanus speculum lineage to produce such ecophenotypes. One new form from the "pseudofibula ... : Supplement to: McCartney, Kevin; Wise, Sherwood W (1990): Cenozoic silicoflagellates and ebridians from ODP Leg 113: biostratigraphy and notes on morphologic variability. In: Barker, PF; Kennett, JP; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 113, 729-760 ...
format Article in Journal/Newspaper
author McCartney, Kevin
Wise, Sherwood W
author_facet McCartney, Kevin
Wise, Sherwood W
author_sort McCartney, Kevin
title Cenozoic silicoflagellates and ebridians from ODP Leg 113 ...
title_short Cenozoic silicoflagellates and ebridians from ODP Leg 113 ...
title_full Cenozoic silicoflagellates and ebridians from ODP Leg 113 ...
title_fullStr Cenozoic silicoflagellates and ebridians from ODP Leg 113 ...
title_full_unstemmed Cenozoic silicoflagellates and ebridians from ODP Leg 113 ...
title_sort cenozoic silicoflagellates and ebridians from odp leg 113 ...
publisher PANGAEA
publishDate 1990
url https://dx.doi.org/10.1594/pangaea.753479
https://doi.pangaea.de/10.1594/PANGAEA.753479
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_relation https://dx.doi.org/10.2973/odp.proc.sr.113.142.1990
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.75347910.2973/odp.proc.sr.113.142.1990
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