Cainozoic Research November 2002 , 1(1-2) (2001), pp. 35-81, Lake Pebas: a palaeoecological reconstruction of a Miocene, long-lived lake complex in western Amazonia 1,7 4 4, F.P. M.E. Räsänen G. Irion H.B. Vonhof R. W. Renema¹, Wesselingh , ², ³, , Kaandorp 5 6 L.+Romero Pittman & M. Gingras 1 NationaalNatuurhistorischMuseum, P.O. Box 9517, NL-2300 RA Leiden,, the Netherlands: e-mail:
[email protected] department ofGeology, University of Turku, SF 20014 Turku, Finland 3 Senckenberg Meeresforschungsinstitut, D 26382 Wilhelmshaven, Germany 4 Department ofEarth Sciences, Vrije Universiteit, de Boelelaan 1085, NL-1081 HV Amsterdam, the Netherlands S INGEMMET, Avenida Canada 1470, San Borja, Lima 12, Peru 6 Departmentof Geology, University ofNew Brunswick, P.O. Box 4400, Fredericton-NB E3B#5A3, Canada 1 Biodiversity Centre, University of Turku, SF20014 Turku, Finland Received 20 February 2001; revised version accepted 19 February 2002 The taxonomic composition and palaeoecological signature of molluscan faunas from the Miocene Pebas Formation of Peruvian Amazonia are assessed. The Pebas fauna is almost entirely made up of extinct, obligate aquatic taxa, and is dominatedin numbers of species and specimens by endemic cochliopine hydrobiid gastropods and pachydontine corbulid bivalves. Molluscan assemblages are defined and linked to depositional environments. Isotope data from the shells indicate freshwater settings during deposition of with the Pebas Formation, the exception of a few incursion levels that were deposited under oligohaline-mesohaline conditions. Faunal and data to a freshwater lake at level with and to isotope geochemical point large, long-lived system sea swamps deltas, open marine settings in the north (Llanos Basin).