Late Holocene precipitation variability recorded in the sediments of Reloncaví Fjord (41°S, 72°W), Chile

TitleLate Holocene precipitation variability recorded in the sediments of Reloncaví Fjord (41°S, 72°W), Chile
Publication TypeJournal Article
Year of Publication2015
AuthorsRebolledo L, Lange CB, Bertrand S, Muñoz P, Salamanca M, Lazo P, Iriarte JL, Vargas G, Pantoja S, Dezileau L
JournalQuaternary Research
Volume84
Pagination21-36
Date PublishedJul
ISSN0033-5894
Accession NumberWOS:000358816900003
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, δ13Corg, N/C ratio, diatom assemblages and biogenic silica contents from three sediment cores. The age models are based on a combination of 210Pb profiles, AMS 14C 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).

DOI10.1016/j.yqres.2015.05.006