Warmer or cooler late Holocene marine palaeoenvironments?: interpreting southeast Australian and Brazilian sea-level changes using fixed biological indicators and their δ18O composition-Reference-Cited by-同舟云学术

Warmer or cooler late Holocene marine palaeoenvironments?: interpreting southeast Australian and Brazilian sea-level changes using fixed biological indicators and their δ18O composition

Published:2001-04 Issue:3-4 Volume:168 Page:249-272
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Baker R.G.V,Haworth R.J,Flood P.G

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference37 articles.

1. The Brazilian sea-level curves: a critical review with emphasis on the curves from the Paranagua and Cananeia regions;Angulo;Marine Geology,1997

2. Relative sea-level changes in the last 5500years in southern Brazil (Laguna-Imbituba region, Santa Catarina State) based on vermetid 14C ages;Angulo;Marine Geology,1999

3. Further evidence from relic shellcrust sequences for a late Holocene higher sea-level for eastern Australia;Baker;Marine Geology,1997

4. Smooth or oscillating late Holocene sea-level curve? Evidence from cross-regional statistical regressions of fixed biological indicators;Baker;Marine Geology,2000

5. Smooth or oscillating late Holocene sea-level curve? Evidence from palaeo-zoology of fixed biological indicators in east Australia and beyond;Baker;Marine Geology,2000

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