Timing and nature of the deepening of the Tasmanian Gateway

Author:

Stickley Catherine E.1,Brinkhuis Henk2,Schellenberg Stephen A.3,Sluijs Appy2,Röhl Ursula4,Fuller Michael5,Grauert Marianne6,Huber Matthew7,Warnaar Jeroen2,Williams Graham L.8

Affiliation:

1. School of Earth, Ocean and Planetary Sciences; Cardiff University; Cardiff UK

2. Laboratory of Palaeobotany and Palynology; Utrecht University; Utrecht Netherlands

3. Department of Geological Sciences; San Diego State University; San Diego California USA

4. Research Center for Ocean Margins, Department of Geosciences; Bremen University; Bremen Germany

5. Hawaii Institute of Geophysics and Planetology; University of Hawaii at Manoa; Honolulu Hawaii USA

6. Department of Geography; University of Copenhagen; Copenhagen Denmark

7. Earth and Atmospheric Science; Purdue University; West Lafayette Indiana USA

8. Geological Survey of Canada (Atlantic); Bedford Institute of Oceanography; Dartmouth Nova Scotia Canada

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Reference83 articles.

1. Laser diffraction size analysis

2. Mechanisms of climate warming at the end of the Paleocene;Bains;Science,1999

3. 14. Middle Eocene through Early Miocene Diatom Floral Turnover

4. Diatom biostratigraphy: Kerguelen Plateau and Prydz Bay regions of the Southern Ocean;Baldauf;Proc. Ocean Drill. Program Sci. Results,1991

5. Scotia Sea regional tectonic evolution: Implications for mantle flow and palaeocirculation;Barker;Earth Sci. Rev.,2001

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