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Years of lacustrine ecosystem changes from Lake Petit (Southern Alps, 2200 m a.s.l.)

Regime shift and resilience of algal communities

Datos Bibliográficos

ID19687188
AutoresRosine Cartier (0000-0002-7448-2693, Aix-Marseille University, CNRS, IRD, Collège de France, UM 34 CEREGE, France, autor de correspondencia), E Brisset (0000-0001-8706-0505, Université d'Avignon et des Pays de Vaucluse), Christine Paillès (0000-0002-6597-0791, Aix-Marseille University, CNRS, IRD, Collège de France, UM 34 CEREGE, France), Frédéric Guiter (0000-0003-0044-2426, Aix-Marseille University, CNRS, IRD, Avignon University, UMR 7263 IMBE, France), Florence Sylvestre (0000-0002-7870-0918, Aix-Marseille University, CNRS, IRD, Collège de France, UM 34 CEREGE, France), Florence Ruaudel (Aix-Marseille University, CNRS, IRD, Avignon University, UMR 7263 IMBE, France), Edward J Anthony (0000-0001-6822-2417, Aix-Marseille University, CNRS, IRD, Collège de France, UM 34 CEREGE, France), Cécile Miramont (0000-0001-5462-0131, Aix-Marseille University, CNRS, IRD, Avignon University, UMR 7263 IMBE, France)
Año2015
Volumen25
Número8
Páginas1231-1245
Fecha de publicación2015-04-20
Peer ReviewedSí
Open AccessSí
TipoARTICLE
RevistaThe Holocene (JOURNAL)
Identificadores de la revistaISSN: 0959-6836 • E-ISSN: 1477-0911
EditorialSAGE Publishing (PUBLISHER • US)
DOI10.1177/0959683615580862
OpenAlexW2141892284
IdiomaEN
Citas recibidas2
Referencias citadas106

Sediments from Lake Petit (2200 m a.s.l., Southern Alps) are particularly relevant for analysis of coupled landscape palaeoecology and palaeolimnology. Diatom assemblages, organic matter composition of sediments (total nitrogen and organic carbon) and Pediastrum boryanum concentrations were obtained from a 144-cm-long core, enabling the reconstruction of the aquatic ecosystem over nearly the last 5000 cal. BP. From 4800 to 4300 cal. BP, Lake Petit was a stable diatom-productive water body dominated by alkaliphilous diatoms ( Staurosirella pinnata). During this period, nutrients and cations were supplied by the chemical weathering of podzols that developed under conifer woodlands. This overall stability was suddenly interrupted at 4200 cal. BP by a major detrital pulse that was probably climate linked (4200 cal. BP event) and that triggered a drop in diatom productivity and diversity. From 4100 to 2400 cal. BP, diatom productivity progressively decreased, whereas Pediastrum developed. Diatom assemblages were more diversified (predominance of Pseudostaurosira robusta, P. brevistriata and P. pseudoconstruens) and reflected a regime of continuous erosion, whereas slopes were colonised by grazed grasslands. Finally, from 2400 cal. BP to the present day, diatom assemblages reveal a slight acidification and nutrient enrichment of waters concomitant with increasing human pressure in the catchment. These results demonstrate the close links between ecosystems and the ready propagation of disturbances throughout watersheds that might lead to abrupt regime shifts in such alpine environments

Biology · Diatom · Ecosystem · Nutrient · Environmental Science · Geological formations and processes · Geology and Paleoclimatology Research · Paleontology and Stratigraphy of Fossils · Ecology · Geology · Oceanography

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Obras citantes distintas2
Citas por año0,29
Intervalo de citas2019 - 2019 (1)
Velocidad de citaciónhistorical
Altamente citadoNo
Tipos de citaNeutras: 2
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