作者: Emmanuel Gandouin , Evelyne Franquet
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摘要: Changes in lake water temperature and trophic states were inferred using chironomid fossil assemblages from Lac Long Inferieur (Southern Alps, France). In the Late Glacial, a colder period, possibly analogous to Younger Dryas, is characterised by peak Micropsectra, cold stenothermic taxon. The increase temperatures during Glacial interstadial indicated decrease percentages of taxa (Tanytarsus lugens/Corynocera oliveri grp.) an linked development vegetation littoral zone. beginning Holocene marked presence adapted warmer more eutrophic waters. During Holocene, progressive warming climate status indicators. An tributary inflow into was also rheophilous taxa, reflecting increased snowmelt. Subatlantic, composition spectra suggests re-cooling and/or status.