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2001
DOI: 10.1023/a:1014557417689
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Cited by 7 publications
(2 citation statements)
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“…Several researchers have considered that these taxa are generalists with an r-strategy and their rapid substrate colonization and high reproduction rate confer them resilience to short-term environmental fluctuations, making them very competitive species under unstable limnological conditions (Lotter and Bigler 2000;Weckström and Juggins 2006;Lotter et al 2010). The presence of a given genus and species of this group has been used as an indication of changes in prolonged ice cover, water temperature, nutrient status, salinity, pH and climatedriven environmental variables (Smol 1988;Dixit et al 1992;Wilson et al 1997;Douglas and Smol 1999;Lotter and Bigler 2000;Karst-Riddoch et al 2009). Thus, they are regarded as good environmental indicators in research projects focused on paleo-and neolimnological conditions.…”
mentioning
confidence: 99%
“…Several researchers have considered that these taxa are generalists with an r-strategy and their rapid substrate colonization and high reproduction rate confer them resilience to short-term environmental fluctuations, making them very competitive species under unstable limnological conditions (Lotter and Bigler 2000;Weckström and Juggins 2006;Lotter et al 2010). The presence of a given genus and species of this group has been used as an indication of changes in prolonged ice cover, water temperature, nutrient status, salinity, pH and climatedriven environmental variables (Smol 1988;Dixit et al 1992;Wilson et al 1997;Douglas and Smol 1999;Lotter and Bigler 2000;Karst-Riddoch et al 2009). Thus, they are regarded as good environmental indicators in research projects focused on paleo-and neolimnological conditions.…”
mentioning
confidence: 99%
“…Model simulations demonstrate late glacial climate change (i.e., precipitation), drove the competitive replacement of droughtadapted vegetation (e.g., savannah or deciduous/semideciduous dry forest) by rainforest in drought-sensitive ecotonal areas (Beerling and Mayle, 2006). Precipitation increased in tropical lowland South America after ∼12,800 cal year BP, as indicated by more frequent flooding and rising lake levels at LLG (Whitney et al, 2011), and in the Andes, water levels increased at Salar de Uyuni (Servant-Vildary et al, 2001) and Lake Titicaca (Baker et al, 2001). Reconstructions from LLG indicate that deglacial temperatures in the lowland Bolivian Amazon rose by 4 • C at 19,500 cal year BP and have likely remained relatively consistent until present (Whitney et al, 2011), supporting the interpretation that temperature was not the dominant driver of late glacial-Holocene vegetation change at NKMNP.…”
Section: Discussionmentioning
confidence: 97%