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- W612329386 abstract "We present reconstructions of late Holocene changes in the source of organic matter and siliceous export production in the Relocanví Fjord (41°S, 72°W), Northern Chilean Patagonia, based on organic carbon content, δ 13 C org , N/C ratio, diatom assemblages and biogenic silica contents from three sediment cores. The age models are based on a combination of 210 Pb profiles, AMS 14 C dating, and on the first occurrence of the diatom Rhizosolenia setigera f. pungens , as a stratigraphic marker in the fjords. The cores span the last 300 to 700 yr. Diatoms dominate the siliceous assemblages in the three cores (98% on average). Our results suggest that precipitation seasonality in the region of Reloncaví was high in CE 1300–1400 and CE 1700–1850, with a clear decreasing trend since CE 1850. The latter trend is in agreement with instrumental records and tree-ring reconstructions. These fluctuations seem to be associated with the Southern Annular Mode (SAM)." @default.
- W612329386 created "2016-06-24" @default.
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- W612329386 date "2015-07-01" @default.
- W612329386 modified "2023-10-07" @default.
- W612329386 title "Late Holocene precipitation variability recorded in the sediments of Reloncaví Fjord (41°S, 72°W), Chile" @default.
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- W612329386 doi "https://doi.org/10.1016/j.yqres.2015.05.006" @default.
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