Clastos con calcimicrobios y arqueociatos procedentes de depósitos marinos del talud de la Formación cámbrica del Monte Wegener, Coats Land, Cordillera de Shackleton Antártida

Rodriguez-Martinez M, Perejon A, Moreno-Eiris E, Menendez S, Buggisch W (2019)


Publication Type: Journal article

Publication year: 2019

Journal

Book Volume: 75

Article Number: e112

Journal Issue: 2

DOI: 10.3989/EGEOL.43586.567

Abstract

The carbonate clasts from the Mount Wegener Formation provide sedimentological, diagenetic and palaeontological evidences of the destruction and resedimentation of a hidden/unknown Cambrian carbonate shallow-water record at the Coats Land region of Antarctica. This incomplete mosaic could play a key role in comparisons and biostratigraphic correlations between the Cambrian record of the Transantarctic Mountains, Ellsworth-Whitmore block and Antarctic Peninsula at the Antarctica continent. Moreover, it represents a key record in future palaeobiogeographic reconstructions of South Gondwana based on archaeocyathan assemblages.

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APA:

Rodriguez-Martinez, M., Perejon, A., Moreno-Eiris, E., Menendez, S., & Buggisch, W. (2019). Clastos con calcimicrobios y arqueociatos procedentes de depósitos marinos del talud de la Formación cámbrica del Monte Wegener, Coats Land, Cordillera de Shackleton Antártida. Estudios Geológicos, 75(2). https://dx.doi.org/10.3989/EGEOL.43586.567

MLA:

Rodriguez-Martinez, M., et al. "Clastos con calcimicrobios y arqueociatos procedentes de depósitos marinos del talud de la Formación cámbrica del Monte Wegener, Coats Land, Cordillera de Shackleton Antártida." Estudios Geológicos 75.2 (2019).

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