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dc.creatorARANEDA,ALBERTO
dc.creatorCRUCES,FABIOLA
dc.creatorTORRES,LAURA
dc.creatorBERTRAND,SEBASTIEN
dc.creatorFAGEL,NATHALIE
dc.creatorTREUTLER,HANS C
dc.creatorCHIRINOS,LUIS
dc.creatorBARRA,RICARDO
dc.creatorURRUTIA,ROBERTO
dc.date2007-06-01
dc.date.accessioned2019-04-25T12:53:39Z
dc.date.available2019-04-25T12:53:39Z
dc.identifierhttps://scielo.conicyt.cl/scielo.php?script=sci_arttext&pid=S0716-078X2007000200002
dc.identifier.urihttp://revistaschilenas.uchile.cl/handle/2250/62821
dc.descriptionChironomid assemblages and sedimentological parameters (grain size, organic content, mineralogy) of a short sediment core from Lake Galletué (38°41' S, 71°17' W) were analysed. The sedimentary record includes one volcanic ash (tephra) layer, which has a completely different composition than the host sediment in terms of organic content, grain size, and mineralogy. According to the geochronology (210Pb and 137Cs), this ash layer corresponds to the eruption of Llaima Volcano in 1956-1957. The tephra deposition had an impact on chironomid assemblages producing, among other changes, an increase in Parakiefferiella and a decrease in Ablabesmyia, although no noticeable change was detected in the diversity index. When compared with other studies, our results also show an impact in terms of the presence of chironomid head capsules within the tephra. The presence of these head capsules could result from the effects of percolation, since the coarse grain size of the tephra particles provides large interstitial spaces. The recovery in the abundances of some taxa after the tephra input, suggests the lake is probably restoring the conditions prevailing before the tephra fall
dc.formattext/html
dc.languageen
dc.publisherSociedad de Biología de Chile
dc.relation10.4067/S0716-078X2007000200002
dc.rightsinfo:eu-repo/semantics/openAccess
dc.sourceRevista chilena de historia natural v.80 n.2 2007
dc.subjectchironomids
dc.subjectlake sediments
dc.subjecttephra layer
dc.subjectsouthern Chile
dc.titleChanges of sub-fossil chironomid assemblages associated with volcanic sediment deposition in an Andean lake (38°S), Chile


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