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- W2047405501 abstract "Abstract Lacustrine deposits exposed around Lake Aricota, Peru (17° 22′S), a 7.5-km 2 lake dammed by debris flows, provide a middle to late Holocene record of lake-level fluctuations. Chronological context for shoreline deposits was obtained from radiocarbon dating of vascular plant remains and other datable material with minimal 14 C reservoir effects (<350 yr). Diatomites associated with highstands several meters above the modern lake level indicate wet episodes. Maximum Holocene lake level was attained before 6100 14 C yr B.P. and ended ∼2700 14 C yr B.P. Moderately high lake levels occurred at 1700 and 1300 14 C yr B.P. The highstand at Lake Aricota during the middle Holocene is coeval with a major lowstand at Lake Titicaca (16°S), which is only 130 km to the northeast and shares a similar climatology. Comparisons with other marine and terrestrial records highlight emerging contradictions over the nature of mid-Holocene climate in the central Andes." @default.
- W2047405501 created "2016-06-24" @default.
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- W2047405501 date "2001-09-01" @default.
- W2047405501 modified "2023-09-23" @default.
- W2047405501 title "Holocene Lake-Level Fluctuations of Lake Aricota, Southern Peru" @default.
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- W2047405501 doi "https://doi.org/10.1006/qres.2001.2263" @default.
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