Journal
MARINE GEOLOGY
Volume 250, Issue 3-4, Pages 223-233Publisher
ELSEVIER SCIENCE BV
DOI: 10.1016/j.margeo.2008.01.007
Keywords
Great Barrier Reef; Pleistocene reef development; mixed carbonate-siliciclastic sediments; Marion Plateau; carbonate sedimentology
Categories
Ask authors/readers for more resources
Significant synchronous shifts in the chemistry, mineralogy, grain sizes and color of the sediments at 6 m below sea floor (mbsf) at ODP Site 1195 on the Marion Plateau (NE Australia) are interpreted to reflect a major regional paleoceanographic change: the initiation of the southern province of the Great Barrier Reef (GBR). The onset of this massive carbonate production centre nearby resulted primarily in increased deposition of carbonate-rich sediments of neritic origin. Both sedimentation rate and terrigenous input record a coincident decline attributed to inshore trapping of materials behind the reefs. Our best estimate places the development of reef framework in the southern part of the GBR between 560 and 670 kyr B.P., based on an age model combining magnetostratigraphic and biostratigraphic data. The proposed estimation agrees with previous studies reporting an age between 500 and 930 kyr B.P., constraining more tightly their results. However, it does not support research placing the birth of the GBR in Marine Isotope Stage (MIS) 11 (similar to 400 kyr), nor the theory of a worldwide modem barrier reef development at that time. (C) 2008 Elsevier B.V. All rights reserved.
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available