Neogene planktonic foraminifera of ODP Leg 101 holes ...

Leg 101 of the Ocean Drilling Program recovered a large volume of Neogene sediments from sites in the Straits of Florida, Little Bahama Bank, and Exuma Sound. In varying amounts, shallow-water, platform-derived carbonate debris is nearly ubiquitous. Reworked planktonic foraminifers are common, espec...

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Bibliographic Details
Main Author: Melillo, Allan J
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1988
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.743447
https://doi.pangaea.de/10.1594/PANGAEA.743447
id ftdatacite:10.1594/pangaea.743447
record_format openpolar
spelling ftdatacite:10.1594/pangaea.743447 2023-05-15T18:00:53+02:00 Neogene planktonic foraminifera of ODP Leg 101 holes ... Melillo, Allan J 1988 application/zip https://dx.doi.org/10.1594/pangaea.743447 https://doi.pangaea.de/10.1594/PANGAEA.743447 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.101.128.1988 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg101 Joides Resolution Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 1988 ftdatacite https://doi.org/10.1594/pangaea.74344710.2973/odp.proc.sr.101.128.1988 2023-04-03T13:12:12Z Leg 101 of the Ocean Drilling Program recovered a large volume of Neogene sediments from sites in the Straits of Florida, Little Bahama Bank, and Exuma Sound. In varying amounts, shallow-water, platform-derived carbonate debris is nearly ubiquitous. Reworked planktonic foraminifers are common, especially in the Pliocene-Pleistocene.At Site 626 in the Straits of Florida, a sequence of Holocene to upper Oligocene sediments was recovered. The greatest Neogene hiatus at this site spans the latest Miocene through Pliocene. Below this, several minor hiatuses are present in a generally conformable sequence.From the Little Bahama Bank transect (Sites 627, 628, and 630), a nearly complete composite Neogene section was sampled. At Site 627, a major unconformity separates lowermost Miocene sediments from middle to upper Eocene sediments. A second major unconformity occurs at Site 628. Here, middle Miocene sediments lie above uppermost Oligocene deposits.Sites 632, 633, and 631 in Exuma Sound all bottomed in a thick, ... : Supplement to: Melillo, Allan J (1988): Neogene planktonic foraminifer biostratigraphy, ODP Leg 101, Bahamas. In: Austin, JA Jr.; Schlager, W; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 101, 3-45 ... Article in Journal/Newspaper Planktonic foraminifera DataCite Metadata Store (German National Library of Science and Technology) Austin
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Leg101
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Drilling/drill rig
Leg101
Joides Resolution
Ocean Drilling Program ODP
Melillo, Allan J
Neogene planktonic foraminifera of ODP Leg 101 holes ...
topic_facet Drilling/drill rig
Leg101
Joides Resolution
Ocean Drilling Program ODP
description Leg 101 of the Ocean Drilling Program recovered a large volume of Neogene sediments from sites in the Straits of Florida, Little Bahama Bank, and Exuma Sound. In varying amounts, shallow-water, platform-derived carbonate debris is nearly ubiquitous. Reworked planktonic foraminifers are common, especially in the Pliocene-Pleistocene.At Site 626 in the Straits of Florida, a sequence of Holocene to upper Oligocene sediments was recovered. The greatest Neogene hiatus at this site spans the latest Miocene through Pliocene. Below this, several minor hiatuses are present in a generally conformable sequence.From the Little Bahama Bank transect (Sites 627, 628, and 630), a nearly complete composite Neogene section was sampled. At Site 627, a major unconformity separates lowermost Miocene sediments from middle to upper Eocene sediments. A second major unconformity occurs at Site 628. Here, middle Miocene sediments lie above uppermost Oligocene deposits.Sites 632, 633, and 631 in Exuma Sound all bottomed in a thick, ... : Supplement to: Melillo, Allan J (1988): Neogene planktonic foraminifer biostratigraphy, ODP Leg 101, Bahamas. In: Austin, JA Jr.; Schlager, W; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 101, 3-45 ...
format Article in Journal/Newspaper
author Melillo, Allan J
author_facet Melillo, Allan J
author_sort Melillo, Allan J
title Neogene planktonic foraminifera of ODP Leg 101 holes ...
title_short Neogene planktonic foraminifera of ODP Leg 101 holes ...
title_full Neogene planktonic foraminifera of ODP Leg 101 holes ...
title_fullStr Neogene planktonic foraminifera of ODP Leg 101 holes ...
title_full_unstemmed Neogene planktonic foraminifera of ODP Leg 101 holes ...
title_sort neogene planktonic foraminifera of odp leg 101 holes ...
publisher PANGAEA
publishDate 1988
url https://dx.doi.org/10.1594/pangaea.743447
https://doi.pangaea.de/10.1594/PANGAEA.743447
geographic Austin
geographic_facet Austin
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_relation https://dx.doi.org/10.2973/odp.proc.sr.101.128.1988
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.74344710.2973/odp.proc.sr.101.128.1988
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