Pike, J. et al. (2004): Late Quaternary biosiliceous laminated marine sediments from Antarctica; seasonality during a period of rapid climate change

Leg/Site/Hole: Related Expeditions:

ODP 178
ODP 178 1098

Identifier: ID:

2007-074674

Type:

georefid

Creator: Name:

Pike, J.

Affiliation:

Cardiff University, School of Earth, Ocean and Planetary Sciences, Cardiff, United Kingdom

Role:

author

Name:

Stickley, Cathy E.

Affiliation:

Colgate University, United States

Role:

author

Name:

Maddison, E. J.

Affiliation:

Montclair State University, United States

Role:

author

Name:

Leventer, A.

Affiliation:

Hamilton College, United States

Role:

author

Name:

Brachfeld, S.

Affiliation:

Stanford University, United States

Role:

author

Name:

Domack, E. W.

Affiliation:

Middlebury College, United States

Role:

author

Name:

Dunbar, R. B.

Affiliation:

Role:

author

Name:

Manley, P. L.

Affiliation:

Role:

author

Name:

McClennen, C.

Affiliation:

Role:

author

Identification: Title:

Late Quaternary biosiliceous laminated marine sediments from Antarctica; seasonality during a period of rapid climate change

Year:

2004

Source:

In: Anonymous, AGU 2004 fall meeting

Publisher:

American Geophysical Union, Washington, DC, United States

Volume:

Issue:

47, Suppl.

Pages:

Abstract:

Language:

English

Genre:

Rights:

URL:

Coverage:Geographic coordinates:

	North:-64.5143
West:-64.1228		East: -64.1228
	South:-64.5143

Keywords:

Quaternary geology; algae; Antarctic ice sheet; Antarctic Peninsula; Antarctica; bioclastic sedimentation; biostratigraphy; Cenozoic; climate change; continental margin; cores; diatoms; dynamics; laminations; Leg 178; marine sediments; microfossils; Ocean Drilling Program; ODP Site 1098; paleo-oceanography; paleoclimatology; Palmer Deep; planar bedding structures; Plantae; Quaternary; sedimentary structures; sedimentation; sediments; siliceous composition; Southern Ocean; thickness; upper Quaternary; varves;

SEDIS - Publications

Pike, J. et al. (2004): Late Quaternary biosiliceous laminated marine sediments from Antarctica; seasonality during a period of rapid climate change