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Holocene vegetation and climate of Baja California Sur, Mexico
SERGIO PEDRIN AVILES
Gustavo Padilla
ERNESTO DIAZ RIVERA
Acceso Abierto
Atribución-NoComercial-SinDerivadas
URL: http://www.rmcg.unam.mx/index.php/rmcg/article/view/1205
ISSN: 2007-2902
Palynology, Paleoclimate, Holocene, Baja California Sur, Mexico
"Research has emphasized pollen and radiocarbon analyses of core samples from coastal mangroves and lagoons and two upland wetlands and dating of raised marine terraces. Mangroves north of La Paz are underlain by up to 4.25 m of peat and lagoonal sediments, deposited over a mid-Wisconsinan coral platform (ca. 25,000 yr BP). Pollen spectra show red mangrove and NAP dominance and suggest relative sea-level rise 9,000 years ago. Significant increases in thorn forest, red and white mangrove, grass and cheno-ams take place after 8,000 yr BP. A progradational event around 4,000 yr BP may be the result of crustal uplift. Subsequently, increases in white and black mangroves and NAP, and decreases in red mangrove suggest development of paludal conditions..."
Centro de Geociencias, UNAM
1994
Artículo
Revista Mexicana de Ciencias Geológicas
Inglés
GEOLOGÍA REGIONAL
Versión publicada
publishedVersion - Versión publicada
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