Cordeiro R. C., Turcq Bruno, Sifeddine Abdelfettah, Lacerda L. D., Silva E. V., Gueiros B., Potty Y. P., Santelli R. E., Padua E. O., Patchinelam S. R. (2011). Biogeochemical indicators of environmental changes from 50 Ka to 10 Ka in a humid region of the Brazilian Amazon. Palaeogeography Palaeoclimatology Palaeoecology, 299 (3-4), p. 426-436. ISSN 0031-0182.
Titre du document
Biogeochemical indicators of environmental changes from 50 Ka to 10 Ka in a humid region of the Brazilian Amazon
Année de publication
2011
Auteurs
Cordeiro R. C., Turcq Bruno, Sifeddine Abdelfettah, Lacerda L. D., Silva E. V., Gueiros B., Potty Y. P., Santelli R. E., Padua E. O., Patchinelam S. R.
Source
Palaeogeography Palaeoclimatology Palaeoecology, 2011,
299 (3-4), p. 426-436 ISSN 0031-0182
We present a geochemical record of a 113.6-cm sediment core (LFT V) from Lagoa da Pata, which is located in the forested upper Rio Negro basin. The record reveals significant changes in the environmental history of Amazonia during the late Quaternary. The results of biogeochemical analyses revealed three hydrological and climatic regimes from 50,000 to 10,000 cal yr BP. The first phase, between 50,000 and 26,300 cal yr BP, was characterized by a relatively wet climate as suggested by relatively high total organic carbon (TOC) and chlorophyll derivate concentrations, indicating high productivity linked to a high lake level. A decrease of the TOC and chlorophyll derivate accumulation rates between 43,100 cal yr BP and 26,300 cal yr BP marks a decrease in the productivity linked to a reduced lake level, indicating a decrease in moisture at the end of this phase. The second phase, between 26,300 and 15,300 cal yr BP, was characterized by a decrease in productivity, reaching a minimum at 21,950 cal yr BP, as indicated by a minima in sedimentary chlorophyll and TOC accumulation rates. Values of delta C-13 increased by 5 parts per thousand in relation to the preceding phase, indicating an influence of the C-4 organic matter. High iron concentrations and accumulation rates, related to intense erosion of the lateritic crust in the watershed, were observed. All of the observations indicate a dry phase during this period. A third phase, from approximately 15,300 to 10,000 cal yr BP, was characterized by an increase in lacustrine productivity, as shown by an increased in TOC and chlorophyll derivate concentrations and accumulation rates. These increases likely correspond to a lake level rise due to a wetter climate. Crown Copyright (c) 2010 Published by Elsevier B.V. All rights reserved.
Plan de classement
Géologie et formations superficielles [064]
Localisation
Fonds IRD [F B010053075]
Identifiant IRD
fdi:010053075
