USGS visual identity mark and link to main Web site

USGS Open-File Report 94-588

Beetle and seed fossils from the Meyer Desert Formation, Sirius Group: New records for Antarctica

Allan C. Ashworth
Department of Geosciences, North Dakota State University
David M. Harwood
Department of Geology, University of Nebraska
Peter N. Webb
Department of Geological Sciences, The Ohio State University
Fossils of a beetle and four vascular plant species have been recovered from a 3.97 kg sample of laminated silts of the Meyer Desert Formation, Sirius Group, Oliver Bluffs, Antarctica. The beetle fossils consist of a tibia and a femur, 1.1 and 2.0 mm in length, respectively. The chitin is opaque and cracked, and is indented by sand grains. Punctuation, sites for the insertion of setae, is clearly evident on both specimens. Based on morphology, the specimens are identified as leg parts of a flightless weevil in the tribe Listroderini (subfamily Cylindrorhininae). Listroderines are well represented in the southern hemisphere, especially in South America. They are most abundant in wet moorland habitats, frequently in association with patches of Nothofagus forest.

More than 100 seeds of vascular plants were recovered from the same sample that yielded the beetle fossils. The seeds are exceptionally well- preserved with interiors filled with authigenic crystals. The seeds are tentatively identified as Empetrum, cf. Ranunculus, cf. Carex, and a species of Rosaceae. None of these taxa presently occurs in Antarctica. Empetrum is a common plant of better-drained locations in the Magellanic Moorland vegetation of the wet Pacific Coast of South America, but also occurs in the heath vegetation of drier sites on the basaltic mesetas of Patagonia.

Based on the domination of Nothofagus pollen in the Sirius Group, it has been suggested that the vegetation was more depauperate than any presently existing in the regions surrounding Antarctica. The beetle and seed fossils suggest a biota with a higher diversity. In combination with Nothofagus, previously described from wood and leaves, and Dacrydium, described from its pollen occurrence, the biota would have had similarities with the Magellanic Moorland of the wet, Pacific coast of South America.

The existing non-parasitic insect fauna of Antarctica consists only of springtails (Collembola) and midges (Chironomidae). The listroderine weevil is the first tangible evidence that Antarctica had a richer insect fauna. Entomologists have long argued this based on the amphi-Antarctic distribution of many insect species but have never had the proof. Given that the specimen was about 8 mm in length and flightless, it is most improbable that it was transported to Antarctica by wind or water currents. Most probably, it represents a member of a lineage whose ancestors inhabited Antarctica from the time of Gondwanaland.

More insect and plant macroscopic remains can be expected to be found in the Sirius Group as different sedimentary facies are discovered and as larger examples are examined. Potentially, these fossils are important for answering questions relating to (1) the depositional environment of the formation, and (2) evolutionary rates and the dispersion of the fauna.


This page is <https://pubs.usgs.gov/openfile/of94-588/02_Ashworth.html>
Maintained by Eastern Publications Group Web Team
Last modified 28-Feb-2001