GCMD




	Agriculture

	Atmosphere

	Biological Classification

	Biosphere

	Climate Indicators

	Cryosphere

	Human Dimensions

	Land Surface

	Oceans

	Paleoclimate

	Solid Earth

	Spectral/Engineering

	Sun-Earth Interactions

	Terrestrial Hydrosphere



	Data Centers

	Locations

	Instruments

	Platforms/Sources

	Projects

Are you using a browser that doesn't support JavaScript or have you disabled JavaScript?

If you have disabled JavaScript, you must re-enable JavaScript to use this page.
Or you can view this record using the Text Only Format.

Record Search Query:

The Biostratigraphy of Middle and Late Cambrian Faunas of Northern Victoria Land, Antarctica

Entry ID: ASAC_143

[ Update this Record ]

Summary

Abstract: Most of the material refers to northern Victoria Land and was collected over two summer seasons (1974-75 with NZARP and in 1981-82 as part of the International North Victoria Land Expedition which was supported by ANARE). As shown on the maps in the publications the area of collection is bounded by latitudes 71 to 73 degrees S and 162 to 166 degrees E. Altitude was generally between 1500 and 2500 ... metres.

From the abstracts of some of the referenced papers:

New evidence bearing on the age and correlation of the Cambrian-Ordovician Bowers Supergroup of northern Victoria Land is outlined. Constraints in the age range of the lower unity, the Sledgers Group are derived from a variety of fossils including a small assemblage of polymerid trilobites in a limestone clast from conglomerate; an age range within the middle Cambrian older than the late Middle Cambrian Boomerangian Stage is most probable. Clastic sedimentation infilling the Bowers depositional depression thus commenced in about the early Middle Cambrian, considerably later than the late Precambrian to Early Cambrian age previously inferred. Similarly, the basaltic volcanism represented by the Glasgow Formation is now known to be of Middle Cambrian age rather than Vendian to Early Cambrian. The conformably overlying Mariner Group is now well dated by trilobites and ranges from late Middle Cambrian (Undillan or Boomerangian) to Late Cambrian (late Idamean or early post-Idamean) in age. The youngest unit, the predominantly fluviatile Leap Year Group, contains a trace fossil assemblage consistent with a Late Cambrian to Ordovician age. The Bowers Supergroup, is thought to have formed part of a zone of Cambrian rifting, subsidence, rapid sedimentation and volcanism that extended through Western Tasmania, providing a link between the Antarctic and Australian segments of Gondwanaland in Cambrian time.

New stratigraphical and palaeontological data from Early Palaeozoic Bowers Group of northern Victoria Land indicates that its depositional basin was probably closely linked with the Dundas Trough of western Tasmania. On the basis of these data, a revised reassembly of the Australo-Antarctic portion of Gondwanaland is proposed.

54 trilobite taxa from 15 new localities in the Bowers Terrane of Northern Victoria Land, including the first fossils from Molar Formation, are described. The fossils indicate an age range from late MIddle Cambrian (Boomerangian or older) to mid Late Cambrian (late Idamean). At Reilly Ridge, the Spurs Formation crops out in a number of fault-bounded slices; the new fossils indicate marked lateral facies contrasts between slices and suggest considerable lateral displacement along the bounding faults. At Houliston Glacier, trilobites of Mindyallan age in Molar Formation imply that the boundary between the Molar and Spurs Formations is strongly time transgressive. New specied described in this paper are Reillopleura braddocki gen. et sp. nov. and Notoaphelaspis horizontalis sp. nov. Faunal affinites are mainly with the Ellsworth Mountains (West Antarctica), western Queensland, and China.

Middle Cambrian, or probably Middle Cambrian, trilobites were collected at six localities in the Heritage Range of the Ellsworth Mountains, including Yochelson Ridge, Drake Icefall area, Edson Hills, Liberty Hills (two locations), and Marble Hills. The total fauna includes 14 genera (2 new) and 32 species (5 new). Due to original preservation and/or deformation, a number of the forms are not assignable to specific taxa. The new taxa described herein are Peronopsis deons sp. nove., Pagetia edsonensis sp. nov., Sohopleura drakensis gen. et. sp nov., Pseudobergeronites spinosa gen. et sp. nov., and Blountia perplexa sp. nov. The trilobites were found in formations of the upper Heritage Group (springer Peak Formation, Drake Icefall Formation, and Liberty Hills Formation). The trilobite faunas described show affinities with faunas from northern Victoria Land (Antarctica), Tasmania, Queensland, China, Kazakhstan, and North America. All faunas are probably Middle Cambrian in age (Templetonian and Boomerangian on the Australian biochronological scale).

Related URL

Link: VIEW PROJECT HOME PAGE

Description: Public information for ASAC project 143

Geographic Coverage

(Click for Interactive Map)

Spatial coordinates

	N: -71.0	S: -73.0	E: 166.0	W: 162.0
Min Altitude: 1500 M Max Altitude: 2500 M

Temporal Coverage

Start Date: 1974-09-01

Stop Date: 1975-03-31

Start Date: 1981-09-01

Stop Date: 1982-03-31

Paleo Temporal Coverage

Chrono Unit:

PHANEROZOIC > PALEOZOIC > CAMBRIAN

Location Keywords

CONTINENT > ANTARCTICA

GEOGRAPHIC REGION > POLAR

Science Keywords

CRYOSPHERE > GLACIERS/ICE SHEETS > GLACIERS

PALEOCLIMATE > LAND RECORDS > MACROFOSSILS

ISO Topic Category

CLIMATOLOGY/METEOROLOGY/ATMOSPHERE

GEOSCIENTIFIC INFORMATION

Platform

FIELD SURVEYS

FIELD INVESTIGATION

Quality The dates provided in temporal coverage are approximate only. Years are correct.

Access Constraints Copies of the referenced papers are available for download from the provided URL to AAD staff only.

Use Constraints This data set conforms to the PICCCBY Attribution License
(http://creativecommons.org/licenses/by/3.0/).

Please follow instructions listed in the citation reference provided at http://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=ASAC_143 when using these data.

This "The Biostratigraphy of Middle and Late Cambrian Faunas of Northern Victoria Land, Antarctica" is licensed under a Creative Commons Attribution 3.0 Unported License.

Ancillary Keywords

ACRITARCHS

ANTARCTICA

Data Set Progress

COMPLETE

Data Center

Australian Antarctic Data Centre, Australia

Data Center URL: http://data.aad.gov.au

Data Center Personnel
Name: DATA OFFICER AADC Phone: +61 3 6232 3244 Fax: +61 3 6232 3351 Email: metadata at aad.gov.au Contact Address: Australian Antarctic Division 203 Channel Highway City: Kingston Province or State: Tasmania Postal Code: 7050 Country: Australia

Distribution

Distribution Media: HTTP

Distribution Size: 22 MB

Distribution Format: pdf

Fees: free

Personnel

JAMES JAGO

Role: INVESTIGATOR

Role: TECHNICAL CONTACT

Role: DIF AUTHOR

Phone: +61 8 8302 3113

Fax: +61 8 8302 3379

Email: Jim.Jago at unisa.edu.au

Contact Address:

DEPARTMENT OF APPLIED GEOLOGY

University Of South Australia

SCHOOL OF ENGINEERING

City: The Levels

Province or State: South Australia

Postal Code: 5095

Country: Australia

Publications/References

Cooper, R.A., Jago, J.B., MacKinnon, D.I., Shergold, J.H., Vidal, G. (1977), Late Precambrian and Cambrian fossils from Northern Victoria Land and their stratigraphic implications., Antarctic Geoscience, 629-633

Creation and Review Dates

DIF Creation Date: 2000-07-19

Last DIF Revision Date: 2011-11-29

Reformat as FGDC document

View Text Only Format

NASA Privacy Policy and Important Notices

Responsible NASA Official: Lola Olsen
Webmaster: Monica Holland · Contact GCMD User Support for assistance