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Amazon Basin sediment accumulation influenced by La Ni'±a

October 10, 2003

Continental-scale rivers can transport enormous sediment loads. In periods of flood, a proportion of these is deposited on flood-plains. In the Amazon Basin, crossed by the Earth's largest river, great volumes of such sequestered sediment accumulations occur. This is especially so in the Llanos, the Bolivian lowland flood-plains which stretch from the foot of the Andes. An estimated 100 to 150 million tonnes of sediment are deposited each year respectively in the Rio Beni and the Rio Mamore flood-plains. These are the two Andean tributaries of the Rio Madeira, one of the Amazon's main tributaries and source of more than half the sediment load transported by that river.

The inter-annual sediment accumulation rate has up to now been considered to be generally constant. Now a study conducted in the floodplain which receives these two tributaries refutes this. It is the first to reveal an episodic pattern. During the past century, large sediment accumulation events indeed occurred only quite infrequently (11 events recorded over 90 years of analysis), corresponding to an average recurrence interval of eight years.

These results were the fruit of investigations forming part of the HyBAm (Hydrogéodynamique du Bassin amazonien) programme, conducted by a joint research team involving the IRD (working in the combined research unit UMR LMTG-CNRS-IRD- Paul Sabatier University of Toulouse), the Universities of Washington1 and California2, and the Bolivian National Meteorology and Hydrology Service (SENAMHI) of La Paz. 210Pb3    activity profile analysis on 300 sediment cores sampled from the Beni and Mamore basin flood-plains, interpreted using a new geochronological model developed by the University of Washington,1 enabled them to date discrete sedimentary packages to near-annual resolution. They revealed evidence of an episodic pattern in the main sedimentation events.
Why does sediment accumulation in this part of the Amazon Basin show an episodic pattern? Climatic variability plays a prime role. The team established a significant correlation between these periods of mass sediment deposition and La Ni'±a, the cold phase of the ENSO (El Ni'±o Southern Oscillation) climatic cycle. During most La Ni'±a years over the past century, the Andean relief has been subjected to torrential rainfall generating fierce flooding and intensive mechanical erosion on the Andean slopes. Recordings from a hydrological station situated at the foot of the Andes showed this. Measurements were continued and followed up in the Hybam programme. When these floods occur, huge volumes of sediment are eroded from the Andean piedmont sub-basins and transported towards the floodplain. For a proportion of these sediments to have been deposited there (for example up to 40% in the Beni Basin flood-plain), the researchers estimate that the water-level rise, during these years of high sedimentation rate, must have been extremely rapid, in excess of 8 000 m3/s. The floods would then have reached the force necessary to cut crevasses in small natural levees along the main stems of the Beni and Mamore rivers and inundate a large expanse of the plain.

With the new data the research team also studied the century-long depositional history in the floodplain of mercury associated with fine particles and the role of these in trapping metal elements transported by the great Amazonian rivers and their tributaries. Also brought to light was a strong increase, over the past 30 years, of mercury concentrations in the sediment particles deposited in the Rio Beni plain. This corresponds to the recent "boom" in gold prospecting, now at an end, but also to the colonization of new arable land on the steep flanks of the Andean piedmont.

1 Quaternary Research Center and Department of Earth and Space Sciences, Rolf Aalto.
2 Donald Bren School of Environmental Science and Management and Department of Geological Sciences, Thomas Dunne.
3 A radioactive isotope used to determine the age of particles deposited in the various beds of sediment.

Institut de Recherche pour le Développement, Paris (IRD)