Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/34505
Title: Biogeochemical processes controlling oxygen and carbon isotopes of diatom silica in Late Glacial to Holocene lacustrine rhythmites
Author: Hernández Hernández, Armand
Bao, Roberto
Giralt Romeu, Santiago
Barker, Philip A.
Leng, Melanie J.
Sloane, Hilary J.
Sáez, Alberto
Keywords: Sediments lacustres
Paleoclimatologia
Holocè
Lake sediments
Paleoclimatology
Holocene
Issue Date: 2011
Publisher: Elsevier B.V.
Abstract: Biogeochemical cycles and sedimentary records in lakes are related to climate controls on hydrology and catchment processes. Changes in the isotopic imposition of the diatom frustules (δ 18 O diatom and δ 13 C diatom ) in lacustrine sediments can be used to reconstruct palaeoclimatic and palaeoenvironmental changes. The Lago Chungará (Andean Altiplano, 18°15 ′ S, 69°10 ′ W, 4520 masl) diatomaceous laminated sediments are made up of white and green multiannual rhythmites. White laminae were formed during short-term diatom super-blooms, and are composed almost exclusively of large-sized Cyclostephanos andinus.These diatoms bloom during mixing events when recycled nutrients from the bottom waters are brought to the surface and/or when nutrients are introduced from the catchment during periods of strong runoff. Conversely, the green laminae are thought to have been deposited over several years and are composed of a mixture of diatoms (mainly smaller valves of C. andinus and Discostella stelligera ) and organic matter. These green laminae reflect the lake's hydrological recovery from a status favouring the diatom super-blooms (white laminae) towards baseline conditions. δ 18 O diatom and δ 13 C diatom from 11,990 to 11,530 cal years BP allow us to reconstruct shifts in the precipitation/evaporation ratio and changes in the lake water dissolved carbon concentration, respectively. δ 18 O diatom values indicate that white laminae formation occurred mainly during low lake level stages, whereas green laminae formation generally occurred during high lake level stages. The isotope and chronostratigraphical data together suggest that white laminae deposition is caused by extraordinary environmental events. El Niño-Southern Oscillation and changes in solar activity are the most likely climate forcing mechanisms that could trigger such events, favouring hydrological changes at interannual-to-decadal scale. This study demonstrates the potential for laminated lake sediments to document extreme pluriannual events.
It is part of: Palaeogeography Palaeoclimatology Palaeoecology, 2011, vol. 299, num. 3-4, p. 413-425
URI: http://hdl.handle.net/2445/34505
ISSN: 0031-0182
Appears in Collections:Articles publicats en revistes (Dinàmica de la Terra i l'Oceà)

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