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Proceedings of the National Academy of Sciences of the United States of America(1)
700,000 years of tropical Andean glaciation
ArticleAbstract: Our understanding of the climatic teleconnections that drove ice-age cycles has been limited by a paPalabras claves:Autores:Abbott M.B., Bryan G. Valencia, Bush M.B., Bustamante M.G., Chen C.Y., Colman S.M., Delgado G., Finkenbinder M., Hatfield R.G., Hillman A.L., Katz S.A., Kück J., Larsen D.J., Lehmann S.B., Mark S.Z., McGee D., Morey A.E., Pierdominici S., Rodbell D.T., Rozas-Dávila A., Solada K.E., Stoner J.S., Tapia P.M., Valero-Garcés B.L., Wattrus N., Weidhaas N.C., Woods A.Fuentes:googlescopusGlobal climate evolution during the last deglaciation
ArticleAbstract: Deciphering the evolution of global climate from the end of the Last Glacial Maximum approximately 1Palabras claves:Autores:Adkins J.F., Bartlein P.J., Blois J.L., Brewer S., Brook E., Carlson A.E., Cheng H., Clark J., Clark P.U., Colman S.M., Curry W.B., Flower B.P., He F., Johnson T.C., Kaufman D.S., Liu Z., Lynch-Stieglitz J., Marchitto T.M., Markgraf V., McManus J., Mitrovica J.X., Mix A.C., Moreno P.I., Morrill C., Otto-Bliesner B.L., Pahnke K., Paul A. Baker, Russell J.M., Shakun J.D., Whitlock C., Williams J.W.Fuentes:scopus