Eocene- Oligocene boundary: biostratigraphic recognition and gradual paleoceanographic change at DSDP Site 549 ( Goban Spur, Bay of Biscay, nannofossil chalks).

S. W. Snyder, C. Muller, Kenneth Miller

Research output: Contribution to journalArticle

18 Citations (Scopus)

Abstract

Drilling on the Goban Spur in the northern Bay of Biscay (Irish continental margin), penetrated an apparently continuous section of upper Eocene-lower Oligocene nannofossil chalks. The Eocene-Oligocene boundary as identified by nannofossils does not coincide with that recognized using planktonic foraminifers.-from Authors

Original languageEnglish (US)
Pages (from-to)112-115
Number of pages4
JournalGeology
Volume12
Issue number2
DOIs
StatePublished - Jan 1 1984
Externally publishedYes

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Eocene-Oligocene boundary
nanofossil
Deep Sea Drilling Project
planktonic foraminifera
Oligocene
continental margin
Eocene
drilling

All Science Journal Classification (ASJC) codes

  • Geology

Cite this

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Eocene- Oligocene boundary : biostratigraphic recognition and gradual paleoceanographic change at DSDP Site 549 ( Goban Spur, Bay of Biscay, nannofossil chalks). / Snyder, S. W.; Muller, C.; Miller, Kenneth.

In: Geology, Vol. 12, No. 2, 01.01.1984, p. 112-115.

Research output: Contribution to journalArticle

TY - JOUR

T1 - Eocene- Oligocene boundary

T2 - biostratigraphic recognition and gradual paleoceanographic change at DSDP Site 549 ( Goban Spur, Bay of Biscay, nannofossil chalks).

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AU - Muller, C.

AU - Miller, Kenneth

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AB - Drilling on the Goban Spur in the northern Bay of Biscay (Irish continental margin), penetrated an apparently continuous section of upper Eocene-lower Oligocene nannofossil chalks. The Eocene-Oligocene boundary as identified by nannofossils does not coincide with that recognized using planktonic foraminifers.-from Authors

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