Late Miocene paleoenvironment of the Lambert Glacier embayment, East Antarctica, evident from: mollusc paleontology, sedimentology and geochemistry

Whitehead, Jason M.; Ehrmann, Werner; Harwood, David M.; Hillenbrand, Claus-Dieter ORCID: https://orcid.org/0000-0003-0240-7317; Quilty, Patrick G.; Hart, Charles; Taviani, Marco; Thorn, Vanessa; Mcminn, Andrew. 2006 Late Miocene paleoenvironment of the Lambert Glacier embayment, East Antarctica, evident from: mollusc paleontology, sedimentology and geochemistry. Global and Planetary Change, 50 (3-4). 127-147. 10.1016/j.gloplacha.2005.07.003

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Official URL: http://dx.doi.org/10.1016/j.gloplacha.2005.07.003

Abstract/Summary

The Upper Miocene (10.7–9.0 Ma) Battye Glacier Formation was deposited 250 km inland from the modern Amery Ice Shelf edge in Prydz Bay, East Antarctica. The composition of clay minerals distinguishes a Lower Member, which reflects regional erosion of Precambrian metamorphic basement, from an Upper Member, which records increased erosion of local Permian–Triassic Amery Group strata. The Upper Member was deposited in an ice-proximal environment akin to the modern fjords of East Greenland, with substantial diamict deposition resulting from melting iceberg discharge. The Lower Member was deposited in an ice-distal environment and included the accumulation of the fossil-bearing McLeod Beds. The McLeod Beds contain much siliceous biogenic sediment (≤ 15% opal), which is rare to absent in the predominantly hemipelagic mud of modern East Greenland fjords. The McLeod Beds also contain largely monospecific in situ Hiatella sp. mollusc assemblages suggestive of environmental stress, potentially caused by low salinity melt-water and a high input of terrigenous sediment, which excluded most other benthic taxa. Geochemical results from primary aragonite in Hiatella shells imply large freshwater input into the marine environment during mollusc growth, causing low δ18O, Na, Mg and high Fe values. The present study indicates that iceberg melt-water influence entering the marine environment was greater during the Late Miocene than today around Antarctica, and documents the paleoenvironment associated with a discrete period of ice margin retreat and marine incursion into the Lambert embayment.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1016/j.gloplacha.2005.07.003
Programmes:	BAS Programmes > Global Science in the Antarctic Context (2005-2009) > Glacial Retreat in Antarctica and Deglaciation of the Earth System
ISSN:	0921-8181
Format Availability:	Electronic, Print
Additional Information. Not used in RCUK Gateway to Research.:	Full text not available from this repository
Additional Keywords:	Palaeoenvironments
NORA Subject Terms:	Earth Sciences
Date made live:	24 Jul 2007 10:17 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/156

Item Type:

Publication - Article

Digital Object Identifier (DOI):

10.1016/j.gloplacha.2005.07.003

Programmes:

BAS Programmes > Global Science in the Antarctic Context (2005-2009) > Glacial Retreat in Antarctica and Deglaciation of the Earth System

ISSN:

0921-8181

Format Availability:

Electronic, Print

Additional Information. Not used in RCUK Gateway to Research.:

Full text not available from this repository