Antarctic ice sheet history and stability: baseline palaeoclimate research on the Pagodroma Group, Prince Charles Mountains.Entry ID: ASAC_1220
Abstract: Detailed sedimentary information and palaeontological samples were collected from Battye Glacier Formation, of the Pagodroma Group in the Prince Charles Mountains, an area where little information is presently available. The mid to Upper Cenozoic Pagodroma Group provides direct evidence for past changes in climate and glacial environments from deep within the Antarctic continent. Evidence from ... several geological formations in the Pagodroma Group, many of them fossil-bearing, will help to determine the history of fluctuations in climate and the size of the East Antarctic Ice Sheet (EAIS). This will provide baseline data to help validate the predictive numerical models of ice sheet dynamics. There is a clear need to study the response of the EAIS to past times of global warming. Periods of significance include times when atmospheric CO2 levels were similar to today (Poore and Sloan 1996). Another key time interval is during the late Neogene, prior to the development of Northern Hemisphere glaciation, which has largely governed Antarctic Ice Sheet volume changes during the Quaternary (Clapperton and Sugden 1990; Mabin 1990; Huybrechts 1990, 1992).
An important aspect of the research is to build onto the geological data-set collected by ODP Leg 119, 120 and 188 in Prydz Bay. These operations have concentrated on the periphery of Antarctica and, therefore, record ice sheet retreat and advance at its outer-limits. The Pagodroma Group provides significant information about ice sheet variation at its the inner reaches. Together, these data-sets will shape our understanding of major fluctuations of the ice sheet through the Cenozoic, and will assist and test the models developed to predict ice sheet behavior in the future. Direct geological evidence for climatic conditions and the extent of the ice sheet during times of glacial retreat can be obtained only from onshore geological records, such as the Pagodroma Group. This is important given the current warming trends, expected ice sheet retreat and global sea-level rise, and general lack of geological data from onshore Antarctica for predicting the effects of this on the EAIS.
Fieldwork was conducted during November - December (2000). A number of significant findings were made from the Amery Oasis:
1) New outcrops of the glacio-marine Battye Glacier Formation were located and mapped. Up to 800 m of geological section was logged and sampled. Similar Antarctic records have only been made available through expensive international drilling efforts around the Antarctic shelf. This project highlights that there are extensive records exposed on land, that can be studied for a fraction of the cost of off-shore marine geoscience.
2) Unique diatomaceous marine mudstone deposits were discovered (~9 m thick). This is the most diatomaceous (up to 12% biogenic silica), in situ marine deposit that has have been found from inland Antarctica. Diatom biostratigraphy indicates that the formation is middle - late Miocene in age.
3) In situ and articulate marine mollusc fossil horizons were discovered. These occur over a lateral distance of ~ 1km and provide undisputable evidence for a major ice sheet retreat in the past.
4) Three erratics containing marine mollusc fossils were discovered. These erratic are potentially Cretaceous in age (Stilwell, pers. comm.). This is the first marine sediment of this age found in the Lambert Graben catchment.
Eleven pdf figures are available for download from the url below. Also included is a text file which explains what each of the figures are. Furthermore, two excel spreadsheets of data are also available.
The two excel spreadsheets in the download directly relate to the paper Whitehead, et al (2003).
Some explanatory notes for the excel files are:
Qualitative assessment of fossil preservation
vf = very fragmented with a few intact specimens seen per traverse of a microscope slide.
mf = moderately fragmented with an intact specimen seen every few fields of view (at 600x magnification).
(See Whitehead et al (2003) for more information.
Qualitative fossil abundance, where
X = (present) one valve (Diatom valves)/fossil seen during entire examination.
R = (rare) >3 valves/fossils seen during all microscope traverses on slide.
F = (few) >1 valve/fossil per 10 microscope fields of view (at 600x magnification).
C = (common) > valve/fossil each microscope field of view (at 600x magnification).
The fields in this dataset are:
Benthic Diatom Abundance
Bardin Bluffs Formation
Fisher Bench Formation
(Click for Interactive Map)
Start Date: 2000-11-01Stop Date: 2000-12-20
Paleo Temporal Coverage
CRYOSPHERE > GLACIERS/ICE SHEETS > ICE SHEETS
LAND SURFACE > EROSION/SEDIMENTATION > EROSION
LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENTATION
LAND SURFACE > EROSION/SEDIMENTATION > STRATIGRAPHIC SEQUENCE
LAND SURFACE > TOPOGRAPHY > LANDFORMS
OCEANS > MARINE SEDIMENTS > SEDIMENTATION
OCEANS > MARINE SEDIMENTS > TERRIGENOUS SEDIMENTS
PALEOCLIMATE > LAND RECORDS > MACROFOSSILS
PALEOCLIMATE > LAND RECORDS > MICROFOSSILS
ISO Topic Category
Access Constraints PDF copies of figures and a paper are available for download from the URL given below. Also available are some excel spreadsheets of data.
Use Constraints This data set conforms to the PICCCBY Attribution License
Please contact the technical contact (Dr. J. Whitehead) before using the data.
Data Set Progress
Distribution Media: HTTP
Distribution Size: 19,353 kb
Distribution Format: pdf, excel
Role: DIF AUTHOR
Phone: +61 3 6266 2980
Fax: +61 3 6226 2973
Email: Andrew.McMinn at utas.edu.au
Institute of Antarctic and Southern Ocean Studies University of Tasmania Private Bag 77
Province or State: Tasmania
Postal Code: 7001
Role: TECHNICAL CONTACT
Phone: +61 3 6226 2659
Fax: +61 3 6226 2973
Email: jm_whitehead at hotmail.com
IASOS GPO BOX 252-77 University of Tasmania
Province or State: Tasmania
Postal Code: 7001
Whitehead, J. M. and Harwood D. M. (Unknown), Stratigraphy of the Battye Glacier Formation, Amery Oasis, Prince Charles Mountains, Antarctica.
Whitehead J.M., Harwood, D.M. and McMinn, A. (2003), Ice-distal Upper Miocene marine strata from inland Antarctica, Sedimentology, 50, 531-552
Stilwell, J.D., Harwood, D.M. and Whitehead, J.M. (2002), Mid-Tertiary macroinvertebrate-rich clasts from the Battye Glacier Formation, Prince Charles Mountains, East Antarctica, Antarctic Science, 14, 1, 69-73
Bloemendal, J., Ehrmann, W., Hambrey, M.J., McKelvey, B. and Whitehead, J. (2003), Geochemical and Rock Magnetic Records from Sediments of the Cenozoic Pagodroma Group, Prince Charles Mountains, East Antarctica: Implications for Provenance and Weathering, Antarctic Science, 15, 3, 365-378
Ehrmann, W., Bloemendal, J., Hambrey, M.J., McKelvey, B.C., and Whitehead, J.M. (2003), Variations in the composition of the clay fraction of the Pagodroma Group: implications for determining provenance, Sedimentary Geology, 161, 1-2, 131-152
Whitehead, J.M. (Unknown), Cenozoic history of Antarctic benthic diatoms., Alcheringa
Creation and Review Dates
DIF Creation Date: 2000-08-10
Last DIF Revision Date: 2011-05-10