A 60-million-year Cenozoic history of western Amazonian ecosystems in Contamana, eastern Peru

Weprovide a synopsis of ~60million years of life history in Neotropical lowlands, based on a comprehensive survey of the Cenozoic deposits along the Quebrada Cachiyacu near Contamana in PeruvianAmazonia. The 34 fossilbearing localities identified have yielded a diversity of fossil remains, including...

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Detalles Bibliográficos
Autores principales: Antoine, Pierre Olivier, Abello, María Alejandra, Adnet, Sylvain, Altamirano Sierra, Ali J., Baby, Patrice, Billet, Guillaume, Boivin, Myriam, Calderón, Ysabel, Candela, Adriana Magdalena, Chabain, Jules, Corfu, Fernando, Croft, Darin A., Ganerød, Morgan, Jaramillo, Carlos, Klaus, Sebastian, Marivaux, Laurent, Navarrete, Rosa E., Orliac, Maëva J., Parra, Francisco, Pérez, María Encarnación, Pujos, François, Rage, Jean Claude, Ravel, Anthony, Robinet, Céline, Roddaz, Martin, Tejada Lara, Julia Victoria, Vélez Juarbe, Jorge, Wesselingh, Frank P., Salas Gismondi, Rodolfo
Formato: Articulo
Lenguaje:Inglés
Publicado: 2016
Materias:
Ciencias Naturales
fossil record
paleobiology
stratigraphy
paleogeography
South America
Acceso en línea:http://sedici.unlp.edu.ar/handle/10915/104972
https://www.sciencedirect.com/science/article/abs/pii/S1342937X15002543
Aporte de:
SEDICI (UNLP) de Universidad Nacional de La Plata
Descripción
Sumario:Weprovide a synopsis of ~60million years of life history in Neotropical lowlands, based on a comprehensive survey of the Cenozoic deposits along the Quebrada Cachiyacu near Contamana in PeruvianAmazonia. The 34 fossilbearing localities identified have yielded a diversity of fossil remains, including vertebrates,mollusks, arthropods, plant fossils, and microorganisms, ranging from the early Paleocene to the lateMiocene–?Pliocene (N20 successive levels). This Cenozoic series includes the base of the Huchpayacu Formation (Fm.; early Paleocene; lacustrine/ fluvial environments; charophyte-dominated assemblage), the Pozo Fm. (middle + ?late Eocene; marine then freshwater environments; most diversified biomes), and complete sections for the Chambira Fm. (late Oligocene–late early Miocene; freshwater environments; vertebrate-dominated faunas), the Pebas Fm. (late early to early late Miocene; freshwater environments with an increasing marine influence; excellent fossil record), and Ipururo Fm. (late Miocene–?Pliocene; fully fluvial environments; virtually no fossils preserved). At least 485 fossil species are recognized in the Contamana area (~250 ‘plants’, ~212 animals, and 23 foraminifera). Based on taxonomic lists from each stratigraphic interval, high-level taxonomic diversity remained fairly constant throughout themiddle Eocene–Miocene interval (8-12 classes), ordinal diversity fluctuated to a greater degree, and family/species diversity generally declined, with a drastic drop in the early Miocene. The Paleocene–?Pliocene fossil assemblages from Contamana attest at least to four biogeographic histories inherited from (i) Mesozoic Gondwanan times, (ii) the Panamerican realm prior to (iii) the time of South America’s Cenozoic “splendid isolation”, and (iv) Neotropical ecosystems in the Americas. No direct evidence of any North American terrestrial immigrant has yet been recognized in the Miocene record at Contamana.

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