An assemblage of large-sized insect traces in paleosols from the middle Miocene of northern Patagonia related to the climatic optimum
Autor: | Alejandro Gustavo Kramarz, M. Victoria Sánchez, Laura Cristina Sarzetti, Eduardo S. Bellosi, Jorge F. Genise |
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Rok vydání: | 2021 |
Předmět: |
010506 paleontology
biology Holocene climatic optimum Pyroclastic rock Geology Trace fossil 010502 geochemistry & geophysics biology.organism_classification 01 natural sciences Paleosol Paleontology Geotrupidae Assemblage (archaeology) Ichnofacies 0105 earth and related environmental sciences Earth-Surface Processes Dung beetle |
Zdroj: | Journal of South American Earth Sciences. 109:103249 |
ISSN: | 0895-9811 |
DOI: | 10.1016/j.jsames.2021.103249 |
Popis: | A new assemblage of large insect trace fossils is recognized in paleosols of the middle Miocene pyroclastic deposits from extra-Andean north Patagonia. This assemblage includes Racemusichnus jacobacciensis igen. isp. nov., the largest trace fossil in paleosols attributed to solitary insects. R. jacobacciensis is represented by clusters of two to seven thickly walled cylinders horizontally orientated in the paleosol. The cluster arrangement, its orientation, the large size and wall of the cylinders suggest a dung beetle, probably a representative of the Geotrupidae as the possible trace maker. The new ichnoassemblage, also comprising large-sized specimens of Coprinisphaera ispp., Teisseirei barattinia and Feoichnus challa, belongs to the Rosellichnus assemblage-SAPIA of the Coprinisphaera Ichnofacies. Mollic paleosols along with the trace fossils, mammal remains and previous data for this unit suggest an open grassy habitat compatible with high productive grass savannas, under a temperate-warm and seasonal subhumid climate. This assemblage of large-sized trace fossils is attributed to highly productive ecosystems related to the rise of temperature occurred during the Middle Miocene Climatic Optimum. |
Databáze: | OpenAIRE |
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