Late Holocene environmental changes reconstructed from stable isotope and geochemical records from a cushion‐plant peatland in the Chilean Central Andes (27°S). (17th February 2019)

• Record Type: Journal Article
• Authors: Kock, S. T.; Schittek, K.; Mächtle, B.; Wissel, H.; Maldonado, A.; Lücke, A.
• Is Part Of: Journal of quaternary science. Volume 34:Number 2(2019)
• Page Start: 153
• Page End: 164
• Publication Date: 2019-02-17
• Subjects: cellulose -- Central Andes -- cushion peatlands -- Late Holocene -- stable isotopes; Geology, Stratigraphic -- Quaternary -- Periodicals; Paleontology -- Quaternary -- Periodicals; 551.79
• DOI: 10.1002/jqs.3088
• Languages: English
• ISSNs: 0267-8179

Abstract

ABSTRACT: A Late Holocene paleoenvironmental record was obtained from the Lagunillas cushion peatland (LP, 27°12′S, 69°17′W), located in the dry Puna of the western Central Andes. Ten radiocarbon dates build the chronology for the last 1800 cal a BP. Analyses of stable isotopes on cellulose (δ 18 Ocell, δ 13 Ccell ) and geochemical proxies on organic matter (δ 13 COM, δ 15 Nbulk, TOC, TN, LOI, T535 ) were conducted to identify major paleoenvironmental changes in this record. Simultaneously, ambient water (δ 18 O, δ 2 H) and plant samples of the dominant species Oxychloe andina (δ 18 Ocell, δ 13 Ccell ) reveal insights into modern conditions. The record reveals distinct multi‐centennial oscillations of peat layer thickness and δ 18 Ocell . Decomposition, changes in the dominating plant species as well as in plant parts (leaves/roots) can be excluded as driving factors for these oscillations. Thus, δ 18 Ocell seems to be externally forced and reflects humidity changes. Around 470 cal a BP a distinct change towards increased humidity occurred, lasting during the Little Ice Age until about 70 cal a BP. Humid conditions prevailed between 1530 and 1270 cal a BP. Increasing δ 18 Ocell values since 30 cal a BP mark a trend towards again increased aridity.