Haq, B. U. et al. (1980): Late Miocene marine carbon-isotopic shift and synchroneity of some phytoplanktonic biostratigraphic events

Leg/Site/Hole: Related Expeditions:

Identifier: ID:

1980-058722

Type:

georefid

Creator: Name:

Haq, B. U.

Affiliation:

Woods Hole Oceanogr. Inst., Woods Hole, Mass., United States

Role:

author

Name:

Worsley, T. R.

Affiliation:

Univ, Ohio, United States

Role:

author

Name:

Burckle, L. H.

Affiliation:

Lamont-Doherty Geol. Obs., United States

Role:

author

Name:

Douglas, R. G.

Affiliation:

Univ. South. Calif., United States

Role:

author

Name:

Keigwin, L. D., Jr.

Affiliation:

Univ. R.I., United States

Role:

author

Name:

Opdyke, N. D.

Affiliation:

Case West. Reserve Univ., United States

Role:

author

Name:

Savin, S. M.

Affiliation:

Fla. State Univ., United States

Role:

author

Name:

Sommer, M. A., II

Affiliation:

Scripps Inst. Oceanogr., United States

Role:

author

Name:

Vincent, E.

Affiliation:

Univ. South. Calif., United States

Role:

author

Name:

Woodruff, F.

Affiliation:

Role:

author

Identification: Title:

Late Miocene marine carbon-isotopic shift and synchroneity of some phytoplanktonic biostratigraphic events

Year:

1980

Source:

Geology (Boulder)

Publisher:

Geological Society of America (GSA), Boulder, CO, United States

Volume:

Issue:

Pages:

427-431

Abstract:

Language:

English

Genre:

Serial

Rights:

URL:

Coverage:Geographic coordinates:

	North:39.0000
West:-86.0000		East: 89.0000
	South:-57.0000

Keywords:

Stratigraphy; algae; benthic taxa; biochronology; biostratigraphy; C-13/C-12; carbon; Cenozoic; Deep Sea Drilling Project; Foraminifera; geochronology; Indian Ocean; Invertebrata; isotopes; magnetostratigraphy; marine environment; microfossils; Miocene; nannofossils; Neogene; Pacific Ocean; paleomagnetism; phytoplankton; plankton; Plantae; Protista; range; ratios; stable isotopes; stratigraphy; Tertiary; thallophytes; time scales; upper Miocene; world ocean;

SEDIS - Publications

Haq, B. U. et al. (1980): Late Miocene marine carbon-isotopic shift and synchroneity of some phytoplanktonic biostratigraphic events