TY - JOUR
T1 - A 60-million-year Cenozoic history of western Amazonian ecosystems in Contamana, eastern Peru
AU - Antoine, Pierre Olivier
AU - Abello, M. Alejandra
AU - Adnet, Sylvain
AU - Altamirano Sierra, Ali J.
AU - Baby, Patrice
AU - Billet, Guillaume
AU - Boivin, Myriam
AU - Calderón, Ysabel
AU - Candela, Adriana
AU - Chabain, Jules
AU - Corfu, Fernando
AU - Croft, Darin A.
AU - Ganerød, Morgan
AU - Jaramillo, Carlos
AU - Klaus, Sebastian
AU - Marivaux, Laurent
AU - Navarrete, Rosa E.
AU - Orliac, Maëva J.
AU - Parra, Francisco
AU - Pérez, María Encarnación
AU - Pujos, François
AU - Rage, Jean Claude
AU - Ravel, Anthony
AU - Robinet, Céline
AU - Roddaz, Martin
AU - Tejada-Lara, Julia Victoria
AU - Vélez-Juarbe, Jorge
AU - Wesselingh, Frank P.
AU - Salas-Gismondi, Rodolfo
N1 - Publisher Copyright:
© 2015 International Association for Gondwana Research.
PY - 2016/3/1
Y1 - 2016/3/1
N2 - We provide a synopsis of ~. 60 million years of life history in Neotropical lowlands, based on a comprehensive survey of the Cenozoic deposits along the Quebrada Cachiyacu near Contamana in Peruvian Amazonia. The 34 fossil-bearing localities identified have yielded a diversity of fossil remains, including vertebrates, mollusks, arthropods, plant fossils, and microorganisms, ranging from the early Paleocene to the late Miocene-?Pliocene (>. 20 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 the middle 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.
AB - We provide a synopsis of ~. 60 million years of life history in Neotropical lowlands, based on a comprehensive survey of the Cenozoic deposits along the Quebrada Cachiyacu near Contamana in Peruvian Amazonia. The 34 fossil-bearing localities identified have yielded a diversity of fossil remains, including vertebrates, mollusks, arthropods, plant fossils, and microorganisms, ranging from the early Paleocene to the late Miocene-?Pliocene (>. 20 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 the middle 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.
KW - Fossil record
KW - Paleobiology
KW - Paleogeography
KW - South America
KW - Stratigraphy
UR - http://www.scopus.com/inward/record.url?scp=84958113790&partnerID=8YFLogxK
U2 - 10.1016/j.gr.2015.11.001
DO - 10.1016/j.gr.2015.11.001
M3 - Review article
AN - SCOPUS:84958113790
SN - 1342-937X
VL - 31
SP - 30
EP - 59
JO - Gondwana Research
JF - Gondwana Research
ER -