Palaeohydrological controls on sedimentary organic matter on Amazon floodplain lakes during the Holocene

Tuesday, 16 December 2014
Luciane Silva Moreira, Universidade Federal Fluminense, geochemistry, Niteroi, Brazil, Patricia F Moreira-Turcq, IRD UFF, Bondy, France, Renato Campello Cordeiro, Universidade Federal Fluminense, Niteroi, Brazil and Bruno Turcq, IRD, Bondy, France
A synthesis of the impacts of the Amazon River hydrological changes on the sedimentation process of organic matter (OM) in three different floodplain lakes (Santa Ninha, Maracá, and Comprido lakes) is presented in this study. Today the Santa Ninha and Maracá lakes are directly and permanently connected with the main channel of the Amazon River, in contrast to Comprido Lake, which is indirectly and periodically influenced by the Amazon River due to its high distance from the main channel. All the sedimentary lake records showed a reduced river inflow due to dry climatic conditions during the Early and Middle Holocene followed by a humid Late Holocene with an increased fluvial input. In Santa Ninha and Maraca Lakes the reduced river inflow period was characterized by sediments with a low abundance of smectite (on average ~20 wt. %), a clay mineral mainly transported by the fluvial system, high total organic carbon (TOC) contents and a predominant C3 vegetation input evidenced by the C/N ratio and d13C. During the Late Holocene, a higher smectite abundance (on average ~43 wt. %) and a low TOC content (on average ~1.4 wt. %) pointed to dilution with the riverine lithogenic matter. In this period a enhanced aquatic primary productivity was evidenced by the increased d13C values and by a C/N typical of algae, suggesting an increased lake water level. In Comprido Lake, a sedimentation gap occurred during the Early and Middle Holocene. The humid Late Holocene, after 3,000 cal years BP, was characterized by high TOC values (on average ~9 wt. %) and increasing abundance of planktonic species, like Aulacoseira sp., which reflects the expansion of water bodies. The predominance of C3-vegetation and low smectite content suggest that in Comprido Lake the soil OM input from the local catchment area was predominant during the humid Late Holocene due to its high distance from the Amazon River main stem. Consequently, our study shows that the sedimentation processes of OM in Amazonian floodplain lakes are strongly influenced by variations in the hydrodynamic regime of the Amazon River during the Holocene. However, its impacts on floodplain lakes were different, mainly depending on the distance from the main stem of the Amazon River.