Quaternary through early Eocene benthic foraminifera off Peru

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Autor principal: Resig, Johanna M
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 1990
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_version_ 1867168555844239360
author Resig, Johanna M
author_facet Resig, Johanna M
collection Datos científicos de ciencias marinas y ambientales
contents Stratigraphic assemblages of Quaternary through early Eocene benthic foraminifers were recovered among 10 Peru margin drill sites. Various hiatuses and intervals barren in foraminifers characterize the sections, but numerous samples contain abundant, well-preserved benthic foraminifers. Bathymetry of the extant species and California-based estimates of the paleobathymetry of the extinct species permit recognition of Quaternary sea-level fluctuations between shelf and upper bathyal depths that produced vertical migrations of oxygenated and low-oxygen habitats at the six shallow sites. Assemblages from lower-slope sites at about 9° and 11°S indicate a general subsidence of the continental margin from shelf or upper bathyal depths in Eocene time to the present lower bathyal depths. Data from 11°S suggest a major part of this subsidence occurred in late Oligocene to early Miocene time. Downslope-transported shelf specimens, particularly the small biserial species, Bolivina costata and B. vaughani, are major contributors to these lower bathyal assemblages from the middle Miocene through Quaternary time.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_745662
institution PANGAEA
language en
publishDate 1990
publisher PANGAEA
record_format pangaea
spellingShingle Quaternary through early Eocene benthic foraminifera off Peru
Resig, Johanna M
112-679D; 112-680B; 112-681A; 112-682A; 112-683A; 112-683B; 112-684A; 112-685A; 112-686A; 112-687A; 112-688A; 112-688E; DRILL; Drilling/drill rig; Joides Resolution; Leg112; Ocean Drilling Program; ODP; South Pacific Ocean
Stratigraphic assemblages of Quaternary through early Eocene benthic foraminifers were recovered among 10 Peru margin drill sites. Various hiatuses and intervals barren in foraminifers characterize the sections, but numerous samples contain abundant, well-preserved benthic foraminifers. Bathymetry of the extant species and California-based estimates of the paleobathymetry of the extinct species permit recognition of Quaternary sea-level fluctuations between shelf and upper bathyal depths that produced vertical migrations of oxygenated and low-oxygen habitats at the six shallow sites. Assemblages from lower-slope sites at about 9° and 11°S indicate a general subsidence of the continental margin from shelf or upper bathyal depths in Eocene time to the present lower bathyal depths. Data from 11°S suggest a major part of this subsidence occurred in late Oligocene to early Miocene time. Downslope-transported shelf specimens, particularly the small biserial species, Bolivina costata and B. vaughani, are major contributors to these lower bathyal assemblages from the middle Miocene through Quaternary time.
title Quaternary through early Eocene benthic foraminifera off Peru
topic 112-679D; 112-680B; 112-681A; 112-682A; 112-683A; 112-683B; 112-684A; 112-685A; 112-686A; 112-687A; 112-688A; 112-688E; DRILL; Drilling/drill rig; Joides Resolution; Leg112; Ocean Drilling Program; ODP; South Pacific Ocean
url https://doi.org/10.1594/PANGAEA.745662