ODP Leg 198: New evidence for rapid climate change in the Cretaceous and Paleogene from the Shatsky Rise, Northwest Pacific Ocean

Timothy Bralower, Isabella Premoli Silva, Mitchell J. Malone

Research output: Contribution to journalArticle

1 Citation (Scopus)

Abstract

Shatsky Rise is a medium-sized, large igneous province in the Pacific Ocean that serves as a pedestal for an impressive 140-million-year package of pelagic sediment. The primary objectives of Ocean Drilling Program (ODP) Leg 198 were to use cores obtained from these sediments to understand long-term transitions into and out of the warm Cretaceous and early Paleogene climate "greenhouse", as well as transient but critical events that involved major changes in oceanic environments, geochemical cycling, and marine biotas.

Original languageEnglish (US)
Pages (from-to)13-17
Number of pages5
JournalJOIDES Journal
Volume28
Issue number2
StatePublished - Sep 1 2002

Fingerprint

Ocean Drilling Program
Climate change
Paleogene
Drilling
Sediments
Cretaceous
large igneous province
climate change
Greenhouses
ocean
sediment
biota
climate
Biota

All Science Journal Classification (ASJC) codes

  • Oceanography
  • Geology

Cite this

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ODP Leg 198 : New evidence for rapid climate change in the Cretaceous and Paleogene from the Shatsky Rise, Northwest Pacific Ocean. / Bralower, Timothy; Silva, Isabella Premoli; Malone, Mitchell J.

In: JOIDES Journal, Vol. 28, No. 2, 01.09.2002, p. 13-17.

Research output: Contribution to journalArticle

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