Climate and hydrologic controls on late Holocene sediment supply to an Amazon floodplain lake

2020

Article référencé dans le Web of Science WOS:000554058500002

Moreira L. S., Moreira Turcq Patricia, Cordeiro R. C., Turcq Bruno, Aniceto K. C., Moreira-Ramirez M., Cruz A. P. S., Caquineau Sandrine, Silva V. C.

Journal of Paleolimnology, 2020, 64 (4), 389-403 ISSN 0921-2728

Organic and inorganic geochemical analyses on sediments from Preto Lake, a central Amazon basin floodplain water body, were used to document hydrological changes of the Solimoes River during the late Holocene. Between 3600 and 400 cal yr BP, Preto Lake received smectite-rich sediment from the Solimoes River, with high concentrations of Al (similar to 53 x 10(3) ppm) and Si (similar to 210 x 10(3) ppm). The high detrital input suggests there was a direct connection between Preto Lake and the main river channel. High river inflow maintained lake stage and was responsible for the contribution to sediments of phytoplankton-derived organic matter. Low sediment organic carbon concentrations characterized this period (mean similar to 3.8 wt%), probably because of dilution by river-borne lithogenic matter. Although the river inputs remained high, abrupt increases in TOC content around 1800 and 1200 cal yr BP suggest brief increases in fluvial nutrient supply to Preto Lake. During the last 400 cal yr, substantial declines in smectite (mean 40%), Al (similar to 29 x 10(3) ppm) and Si (138 x 10(3) ppm) suggest the establishment of a semi-isolated lake, with reduced river inflow. A large proportion of C3-plant-derived organic matter, supplied by runoff from the kaolinite-rich watershed, was observed during this period, and was accompanied by high autochthonous primary production, driven by development of an aquatic macrophyte community. This change in sediment organic matter source accounted for the greater TOC content (similar to 20%) of sediments deposited during this period. Although Holocene climate change was an important control on fluvial sediment supply to upper and lower Amazon Basin floodplain lakes, sedimentation processes in Preto Lake can also be linked to changes in the river's course. The transition to a semi-isolated lake could have been a consequence of lateral and vertical sediment accretion, which formed a natural levee that blocked fluvial input to Preto Lake.

Sciences du milieu [021] ; Limnologie physique / Océanographie physique [032] ; Hydrologie [062] ; Géologie et formations superficielles [064]

BRESIL

Fonds IRD [F B010079392]

fdi:010079392