25 Tropical Climate and Paleoclimate (Posters)

Monday, 21 March 2016
1:30 PM - 5:30 PM
Convention Hall


RECONSTRUCTING PAST AFRICAN RIVER HYDROLOGY BY MEANS OF FRESHWATER BIVALVE GEOCHEMISTRY

Paper number: 25-4
Program: Theme Sessions
Time: 1:30 PM – 5:30 PM


Authors


Abstract

Freshwater bivalves occur in nearly all river basins and different types of river ecosystems. Microsampling of the growth increments in their shells allows high-resolution reconstruction of intra-yearly changes in ambient river water geochemistry. Specimens were collected from locations across Africa (Niger, Mali, Central African Republic, D.R. Congo, Kenya, Botswana, Namibia, and South Africa). Isotope ratios of δ18O were measured in order to reconstruct δ18O of ambient water. Based on 3+ year monitoring of temperature and water δ18O in Bangui, Kinshasa and Kisangani (all Congo Basin), we show that different species, including Chambardia, Aspatharia and Etheria accurately record water δ18O in their shell carbonate, and can be used to reconstruct past river discharge. Intra-annual variability of δ18O in central Africa is relatively low, between -4.0 ‰ and -2.0 ‰ around the equator and between -4.0 and 0.0 ‰ at 5° N. Towards southern Africa, the seasonal range increases to 6.9 ‰, reflecting both temperature and δ18O-water variability. By contrast, specimens from Niger show a 12 ‰ range, from -8.0 to +4.0 ‰, and an Aspatharia from a Lake Faguibine tributary in Mali shows previously unrecorded δ18O values ranging up +11.3‰, reflecting contrasting humidity and highly evaporative conditions. These data provide a preliminary investigation of continental-scale variability in riverine δ18O variability as recorded by freshwater bivalves.

Geological Society of America Abstracts with Programs. Vol. 48, No. 1

doi: 10.1130/abs/2016NE-272922

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