5
views
0
recommends
+1 Recommend
1 collections
    0
    shares
      • Record: found
      • Abstract: found
      • Article: found
      Is Open Access

      Los mamíferos finipleistocénicos de la Formación Quebrada Quereo (IV Región-Chile): biogeografía, bioestratigrafía e inferencias paleoambientales Translated title: The Late Pleistocene mammal record of Quebrada Quereo Formation: biogeography, biostratigraphy and paleoclimatic inferences

      research-article

      Read this article at

      Bookmark
          There is no author summary for this article yet. Authors can add summaries to their articles on ScienceOpen to make them more accessible to a non-specialist audience.

          Translated abstract

          This paper describes the fossil fauna recovered from the Quebrada Quereo Formation (Late Pleistocene - Holocene) located at Choapa Province, IV Region, Chile. In this formation, two cultural levels (Quereo I y II) with Pleistocenic fauna were detected. The remains identified include living species (Dusycion cf. D. culpaeus), as well as extinguished fauna (Palaeolama sp., Antifer sp., Equus [Amerhippus] sp., cf. Panthera onca, Milodontidae, and Gomphoteriidae). For each of these, we present taxonomic, paleogeographic and paleoclimatic remarks. The possible presence of P. onca in Quebrada Quereo Formation constitutes the first evidence of a locally extinct felid outside the Patagonic area of Chile. The identified faunal assemblage presents differences with those recorded in Argentinean territory; which is explained by the presence of the Cordillera de los Andes. The Chilean paleofaunistic assemblages, therefore, are related to those found in Bolivia and the Andean occidental sector in general, although some enrichment with taxa from the oriental side of the range is not discarded.

          Related collections

          Most cited references85

          • Record: found
          • Abstract: found
          • Article: not found

          Palynological Evidence for Increased Aridity on the Central Chilean Coast during the Holocene

          The late Quaternary vegetation of the semiarid coast of central Chile is inferred from the palynological analysis of profiles from Quereo (31°55′S) and Quintero (32°47′S). Prior to 11,400 yr B.P., wet conditions are suggested by the abundance of pollen indicators of swamp and aquatic taxa, such as Cyperaceae and Myriophyllum , and by the presence of traces of arboreal pollen. Since ca. 10,000 yr B.P., a trend toward increasingly drier conditions is implied by the almost complete absence of arboreal and aquatic taxa, and a general decrease in the diversity of the semiarid shrubland indicators. From 3000 yr B.P. onward, the pollen records show the reappearance of swamp and aquatic taxa, presumably associated with wetter conditions, which led to recolonization by forest taxa at 1720 yr B.P. in Quintero. The drier climate detected along the semiarid coast of central Chile during most of the Holocene extended inland to the Andean foot-hills, within the present mediterranean-type climate zone of Chile, and also affected the distribution of the winter-deciduous Nothofagus forests and the northern boundary of the temperate rain forests.
            Bookmark
            • Record: found
            • Abstract: not found
            • Article: not found

            The Pleistocene Gomphotheriidae (Proboscidea) from South America

              Bookmark
              • Record: found
              • Abstract: found
              • Article: not found

              Late pleistocene faunal extinctions in southern patagonia.

              V Markgraf (1985)
              Major environmental changes recorded in pollen records from various sites in southern Patagonia and Tierra del Fuego are also reflected in pollen and cuticle data from dung of the late Pleistocene groundsloth. The most prominent change was the large-scale reduction of steppe environment about 10,000 years ago, which coincides with the latest dates for extinctions of many large grazers such as the giant groundsloth. Stress on food resources for all the large grazers may well have hastened their extinction. Hunting pressure by paleoindians may have been the final blow.
                Bookmark

                Author and article information

                Contributors
                Role: ND
                Role: ND
                Journal
                mznt
                Mastozoología neotropical
                Mastozool. neotrop.
                Sociedad Argentina para el Estudio de los Mamíferos (SAREM) (Mendoza, Mendoza, Argentina )
                0327-9383
                1666-0536
                June 2006
                : 13
                : 1
                : 89-101
                Article
                S0327-93832006000100007
                d1866c81-89e6-4b44-a193-750f17187671

                This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.

                History
                : 23 April 2006
                : 15 May 2005
                Page count
                Figures: 0, Tables: 0, Equations: 0, References: 64, Pages: 13
                Product

                SciELO Argentina


                Chile,Extinct fauna,Late Pleistocene–Early Holocene,Quebrada Quereo Formation

                Comments

                Comment on this article