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Synchronisation of sedimentary records using tephra: A postglacial tephrochronological model for the Chilean Lake District

Abstract:
Well-characterised tephra horizons deposited in various sedimentary environments provide a means of synchronising sedimentary archives. The use of tephra as a chronological tool is however still widely underutilised in southern Chile and Argentina. In this study we develop a postglacial tephrochronological model for the Chilean Lake District (ca. 38 to 42°S) by integrating terrestrial and lacustrine records. Tephra deposits preserved in lake sediments record discrete events even if they do not correspond to primary fallout. By combining terrestrial with lacustrine records we obtain the most complete tephrostratigraphic record for the area to date. We present glass geochemical and chronological data for key marker horizons that may be used to synchronise sedimentary archives used for palaeoenvironmental, palaeoclimatological and palaeoseismological purposes. Most volcanoes in the studied segment of the Southern Volcanic Zone, between Llaima and Calbuco, have produced at least one regional marker deposit resulting from a large explosive eruption (magnitude ≥ 4), some of which now have a significantly improved age estimate (e.g., the 10.5 ka Llaima Pumice eruption from Llaima volcano). Others, including several units from Puyehue-Cordón Caulle, are newly described here. We also find tephra related to the Cha1 eruption from Chaitén volcano in lake sediments up to 400 km north from source. Several clear marker horizons are now identified that should help refine age model reconstructions for various sedimentary archives. Our chronological model suggests three distinct phases of eruptive activity impacting the area, with an early-to-mid-Holocene period of relative quiescence. Extending our tephrochronological framework further south into Patagonia will allow a more detailed evaluation of the controls on the occurrence and magnitude of explosive eruptions throughout the postglacial.
Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1016/j.quascirev.2016.02.015

Authors


More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author


More from this funder
Funding agency for:
Rawson, H
Fontijn, K
Grant:
NE/I013210/1
NE/I013210/1


Publisher:
Elsevier
Journal:
Quaternary Science Reviews More from this journal
Volume:
137
Pages:
234–254
Publication date:
2016-02-01
Acceptance date:
2016-02-15
DOI:
EISSN:
1873-457X
ISSN:
0277-3791


Keywords:
Pubs id:
pubs:604828
UUID:
uuid:bb0c008d-df61-49cc-ba23-8dcde60a951e
Local pid:
pubs:604828
Source identifiers:
604828
Deposit date:
2016-02-18

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