http://www.cnr.it/ontology/cnr/individuo/prodotto/ID53035
Diatom response to mid-Holocene climate change in Lago di Massaciuccoli (Tuscany, Italy) (Articolo in rivista)
- Type
- Label
- Diatom response to mid-Holocene climate change in Lago di Massaciuccoli (Tuscany, Italy) (Articolo in rivista) (literal)
- Anno
- 2008-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1007/s10933-007-9154-6 (literal)
- Alternative label
Marchetto A., Colombaroli D.(1), Tinner W.(1) (2008)
Diatom response to mid-Holocene climate change in Lago di Massaciuccoli (Tuscany, Italy)
in Journal of paleolimnology
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Marchetto A., Colombaroli D.(1), Tinner W.(1) (literal)
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- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- (1)Università di Berna (literal)
- Titolo
- Diatom response to mid-Holocene climate change in Lago di Massaciuccoli (Tuscany, Italy) (literal)
- Abstract
- A sedimentary sequence from the Mediterranean coastal basin of Lago di Massaciuccoli
(Tuscany, Italy) was analyzed for diatoms, covering two periods over the past ca. 7,000 years. The site
was selected because it is situated in a sensitive position at the limit between Mediterranean and
Central European climates and biomes. Our focus is on the impact of accelerated human activity during
the recent past (water uptake in the catchment, sand extraction, wastewater discharge) and on a phase of
evident change between 6,600 and 5,400 cal. BP. The diatom record suggests fresh-water conditions and
rather high lake levels until ca. 6,000 years ago. The subsequent shift towards brackish conditions peaked
at around 5,500 cal. BP. We relate this shift to a pervasive change towards a drier climate that has
been observed elsewhere in the Mediterranean and Northern African regions, and stands in contrast to
the shift towards a cooler and more humid climate in the nearby Alps (200-350 km distant) and in central
Europe. Pollen and charcoal records from a previous study on the same sedimentary sequence were used to
gain additional insights about the causes of the changes in the diatom assemblages and apply
numerical methods to search for common trends and correlations. (literal)
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