Pierre-Olivier Combelles Posted February 27, 2017 Posted February 27, 2017 During the same years (1997-2000) and in the same region of the High Andes of Peru, I discovered the fossil fern and the fossil coral presented in my two other topics: http://www.thefossilforum.com/index.php?/topic/72054-fossil-fern-in-the-high-andes-of-peru/#comment-758432 http://www.thefossilforum.com/index.php?/topic/72061-coral-fossil-of-the-high-andes-of-peru/#comment-758464 , I took this picture (slide poorly scanned, sorry) of ammonites in the stone wall of San Pedro de Parish, an old little abandonned church of the beginning of the Hispanic Colony, on the shore of Lake Junin (or Chinchaycocha, en quechua), altitude 4125m. What do you think about it, especially in relation with the branching coral ? Thanks
Pierre-Olivier Combelles Posted February 27, 2017 Author Posted February 27, 2017 Lake Junin (orL. Chincaycocha) is on the right, Lima on the left. Peruvian map, 1855.
Pierre-Olivier Combelles Posted February 28, 2017 Author Posted February 28, 2017 The church of San Pedro de Parish, on the shore of Lake Junin (4125 m). May be XVIIe century. The ammonites are on a stone of the abutment at the right side of the entrance. This stone had been especially choosed for its decorative effect, of course...
Pierre-Olivier Combelles Posted August 10, 2017 Author Posted August 10, 2017 An interesting paper from french IRD (Institut de Recherche pour le Développement) of 2005: The Lower Carboniferous of the western edge of Gondwana in Peru and Bolivia: Distribution of sedimentary basins and associated magmatism Alberto Zapata M. \ Agapito Sanchez F. '. Segundo Carrasco V. 1, Agustin Cardona 2, Jorge Galdos H. 1, Fredy Cerrôn Z. 1, & Thierry Sempere 3 1 Direction of Regional Geology, Instituto Geologico Minero Metalurgico (INGEMMET), Lima, Peru 2 Phd student of the University of Sâo Paulo, Brazil 3 IRD, LMTG, Observatoire Midi-Pyrénées, 14 avenue Edouard Belin, 31400 Toulouse, France 6th International Symposium on Andean Geodynamics (ISAG 2005, Barcelona), Extended Abstracts: 817-820 http://horizon.documentation.ird.fr/exl-doc/pleins_textes/divers09-03/010040372.pdf Would date the fossils of this area and our ammonites, in the Carboniferous, somewhere between Tournaisien (-358.9) and Serpoukhovien (-323.2). See the extract below ("Junin-Huancavelica Sector"): Ambo Group. As said in the abstract of the paper, we are here in the western edge of Gondwana: "During the Early Carboniferous, the tectono-sedimentary and rnagrnatic configuration of the western edge of Gondwana (Eastern Cordillera of Peru and Cordillera Real of Bolivia, between latitudes 3°S and 24°S; Figure 1) associated a marine and continental sedimentation (Ambo Group), a volcanic arc (Lavasen Formation) and a related plutonism (Pataz-Balsas-Buldibuyo batholith, Higueras pluton , Amparaes and Cadenas granites). "
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