New evidence of a Campanian age for the Cretaceous fossil-bearing strata of Cape Marsh, Robertson Island, Antarctica

Tobin, Thomas S., Roberts, Eric M., Slotznick, Sarah P., Biasi, Joseph A., Clarke, Julia A., O'connor, Patrick M., Skinner, Steven M., West, Abagael R., Snyderman, Lucia S., Kirschvink, Joseph L., and Lamanna, Matthew C. (2020) New evidence of a Campanian age for the Cretaceous fossil-bearing strata of Cape Marsh, Robertson Island, Antarctica. Cretaceous Research, 108. 104313.

[img] PDF (Published Version) - Published Version
Restricted to Repository staff only

View at Publisher Website:


Cape Marsh, located on the eastern end of Robertson Island to the east of the Antarctic Peninsula, exposes an isolated outcrop of Upper Cretaceous sedimentary strata. The outcrop is approximately 120 km southwest of the much better-studied exposures of similar age on and around James Ross Island (JRI): as such, its remoteness has complicated logistical access to the site and hindered geologic correlations on a regional scale. Here we present the results of fieldwork conducted in 2016 that yielded a more diverse invertebrate fossil assemblage than had been previously recognized, in addition to new U-Pb detrital zircon and magnetostratigraphic data. The invertebrate fauna, particularly the ammonites and inoceramids, support a biostratigraphic correlation of the upper Cape Marsh strata to Ammonite Assemblage 7 previously established on JRI. Detrital zircon U-Pb analysis conducted on a sandstone sample from the same strata indicates a maximum depositional age of 74.2 +/- 1.1 Ma, and magnetostratigraphic interpretation of the lower strata suggest a normal magnetochron. These results are all consistent with a Campanian age for the deposition of the upper strata at Cape Marsh, and deposition during magnetochron C33N for the lower layers. However, a slight age inconsistency between the biostratigraphic correlation and the detrital zircon-derived maximum depositional age may imply that the fossils are reworked. Regardless, these new data allow us to correlate the strata at Cape Marsh to the Santa Marta and Rabot formations (or possibly the lower part of the Snow Hill Island Formation) in the northern part of the James Ross Basin.

Item ID: 62562
Item Type: Article (Research - C1)
ISSN: 1095-998X
Keywords: Cretaceous, Campanian, James Ross Basin, Biostratigraphy, Detrital zircon, Antarctica
Copyright Information: (C) 2019 Elsevier Ltd. All rights reserved.
Funders: National Science Foundation (NSF), USA
Projects and Grants: NSF NT-1142129, NSF ANT-1142104, NSF ANT-1141820, NSF ANT-1142052, NSF ANT-1341729
Date Deposited: 18 Mar 2020 07:34
FoR Codes: 37 EARTH SCIENCES > 3705 Geology > 370506 Palaeontology (incl. palynology) @ 100%
SEO Codes: 97 EXPANDING KNOWLEDGE > 970104 Expanding Knowledge in the Earth Sciences @ 100%
Downloads: Total: 1
More Statistics

Actions (Repository Staff Only)

Item Control Page Item Control Page