Neogene palynology of Deep Sea Drilling Site 603 on the lower continental rise, northwestern Atlantic

W. A. Van Der Kaars

doi:10.2973/dsdp.proc.93.124.1987

Neogene palynology of Deep Sea Drilling Site 603 on the lower continental rise, northwestern Atlantic

W. A. Van Der Kaars

Earth and Climate

Research output: Chapter in Book / Report / Conference proceeding › Chapter › Academic › peer-review

Abstract

The analysis of 104 core-catcher samples from Site 603 resulted in a continuous palynological record from the middle Miocene to early Pleistocene. Two palynological zones could be established (Zone 2, below 380 m: high Pinus, Quercus, and Carya values; Zone 1, above 380 m; high Pinus, and Sphagnum values). The marine pollen record was found to reflect the history of the vegetation of the eastern United States, the flora from Zone 2 indicating a warmer climate than that from Zone 1, which depicts a climatic cooling trend. The onset of Western Boundary Undercurrent deposition had no noticeable effect on the pollen distribution in the marine sediment. -Author

Original language	English
Title of host publication	Initial reports DSDP
Subtitle of host publication	Volume XCIII, Norfolk, Virginia to Norfolk, Virginia Part 2
Chapter	24
Pages	783-788
Number of pages	6
Volume	2
DOIs	https://doi.org/10.2973/dsdp.proc.93.124.1987
Publication status	Published - 1987

Publication series

Name	Initial reports DSDP
Volume	93

Bibliographical note

Copyright:
Copyright 2017 Elsevier B.V., All rights reserved.

Access to Document

10.2973/dsdp.proc.93.124.1987

Persistent URL (handle)

Persistent link

Cite this

@inbook{e8ee0d9fd6394d1fb45186cd5c6dd1b5,

title = "Neogene palynology of Deep Sea Drilling Site 603 on the lower continental rise, northwestern Atlantic",

abstract = "The analysis of 104 core-catcher samples from Site 603 resulted in a continuous palynological record from the middle Miocene to early Pleistocene. Two palynological zones could be established (Zone 2, below 380 m: high Pinus, Quercus, and Carya values; Zone 1, above 380 m; high Pinus, and Sphagnum values). The marine pollen record was found to reflect the history of the vegetation of the eastern United States, the flora from Zone 2 indicating a warmer climate than that from Zone 1, which depicts a climatic cooling trend. The onset of Western Boundary Undercurrent deposition had no noticeable effect on the pollen distribution in the marine sediment. -Author",

author = "\{Van Der Kaars\}, \{W. A.\}",

year = "1987",

doi = "10.2973/dsdp.proc.93.124.1987",

language = "English",

volume = "2",

series = "Initial reports DSDP",

pages = "783--788",

booktitle = "Initial reports DSDP",

}

Neogene palynology of Deep Sea Drilling Site 603 on the lower continental rise, northwestern Atlantic. / Van Der Kaars, W. A.
Initial reports DSDP: Volume XCIII, Norfolk, Virginia to Norfolk, Virginia Part 2. Vol. 2 1987. p. 783-788 (Initial reports DSDP; Vol. 93).

Research output: Chapter in Book / Report / Conference proceeding › Chapter › Academic › peer-review

TY - CHAP

T1 - Neogene palynology of Deep Sea Drilling Site 603 on the lower continental rise, northwestern Atlantic

AU - Van Der Kaars, W. A.

PY - 1987

Y1 - 1987

N2 - The analysis of 104 core-catcher samples from Site 603 resulted in a continuous palynological record from the middle Miocene to early Pleistocene. Two palynological zones could be established (Zone 2, below 380 m: high Pinus, Quercus, and Carya values; Zone 1, above 380 m; high Pinus, and Sphagnum values). The marine pollen record was found to reflect the history of the vegetation of the eastern United States, the flora from Zone 2 indicating a warmer climate than that from Zone 1, which depicts a climatic cooling trend. The onset of Western Boundary Undercurrent deposition had no noticeable effect on the pollen distribution in the marine sediment. -Author

AB - The analysis of 104 core-catcher samples from Site 603 resulted in a continuous palynological record from the middle Miocene to early Pleistocene. Two palynological zones could be established (Zone 2, below 380 m: high Pinus, Quercus, and Carya values; Zone 1, above 380 m; high Pinus, and Sphagnum values). The marine pollen record was found to reflect the history of the vegetation of the eastern United States, the flora from Zone 2 indicating a warmer climate than that from Zone 1, which depicts a climatic cooling trend. The onset of Western Boundary Undercurrent deposition had no noticeable effect on the pollen distribution in the marine sediment. -Author

UR - https://www.scopus.com/pages/publications/0023518041

UR - https://www.scopus.com/pages/publications/0023518041#tab=citedBy

UR - http://www.deepseadrilling.org/i_reports.htm

U2 - 10.2973/dsdp.proc.93.124.1987

DO - 10.2973/dsdp.proc.93.124.1987

M3 - Chapter

AN - SCOPUS:0023518041

VL - 2

T3 - Initial reports DSDP

SP - 783

EP - 788

BT - Initial reports DSDP

ER -

Neogene palynology of Deep Sea Drilling Site 603 on the lower continental rise, northwestern Atlantic

Abstract

Publication series

Bibliographical note

Access to Document

Persistent URL (handle)

Other files and links

Fingerprint

Cite this