Paleoclimate variability in central Taiwan during the past 30 Kyrs reflected by pollen, delta C-13(TOC), and n-alkane-delta D records in a peat sequence from Toushe Basin

• Published in: Journal of Asian Earth Sciences
• Main Authors: Li, Hong-Chun, Liew, Ping-Mei, Seki, Osamu, Kuo, Tz-Shing, Kawamura, Kimitaka, Wang, Liang-Chi, Lee, Teh-Quei
• Other Authors: Department of Earth sciences
• Format: Article in Journal/Newspaper
• Language: English
• Published: Elsevier 2013
• Subjects: C and H stable isotope; Organic carbon content; Peat sequence of central Taiwan; Paleoclimate; Late Pleistocene; Greenland; Hulu; Greenland ice core; ice core
• Online Access: https://doi.org/10.1016/j.jseaes.2012.12.005; http://ir.lib.ncku.edu.tw/handle/987654321/147106; http://ir.lib.ncku.edu.tw/bitstream/987654321/147106/-1/index.html

A total of 233 samples from the upper 16 m of the Toushe peat core retrieved in central Taiwan were measured for TOC and delta C-13(TOC) values. From these samples, 17 selected samples with large delta C-13(TOC) fluctuations were analyzed for n-alkane and delta D of the C27 and C29 n-alkanes. Combining with the detailed high-resolution pollen and geochemical records, this study reveals more detailed climatic variations in terms of temperature and precipitation as well as abrupt climatic events during the past 30 Kyrs. Before the Last Glacial Maximum (LGM), climate was cold and damp with predominantly woodland vegetation in Toushe Basin, and turned to cold and dry after 25 Kyr BP. Climatic conditions there were the worst during LGM over the past 30 Kyrs, especially around 23 and 18 Kyr BP when the woodland was diminished and C4 grass was dominated. Although short durations of relatively wet conditions could be found at 17, 16 and 14 Kyr BP, cold and dry climates were prevailing during 29.5-28, 24-22, 17-15 and 13-11.5 Kyr BP, corresponding to Heinrich (H) Events 3, 2, 1, and Younger Dryas (YD), respectively. During the early Holocene, dry climate occurred at similar to 11, similar to 10, 9.7-9.2 and similar to 8 Kyr BP; whereas wet condition appeared at 10.3, 9.8, 9-7.5 Kyr BP. In the middle Holocene, climate kept warm and moderate wet in the first half period, but many dry events existed in the second half following a cold and dry event at 6 Kyr BP. After a sharply warm peak at 5.2 Kyr BP, the climate in Toushe turned to cold quickly, and tree/shrub vegetation disappeared completely with the replacement of C3 grasses. In the late Holocene, climate was relatively wetter with predominant C3 grasses in the basin. Our climatic interpretations based on the peat records agree well with the Greenland ice core and Chinese speleothem records on millennium time scales during the last glacial period. Dry climates corresponding to weakening of the East Asian Summer Monsoon (EASM) during the Heinrich events and Younger Dryas in central Taiwan and eastern China demonstrate the climatic forcing on such long time scales in concert with regional monsoon climate. However, the discrepancies exist between our peat record and the Dongge/Hulu stalagmite record on: (1) the age of H2; (2) climate intensities of LGM and HI; and (3) wetness condition during Holocene. These observations call for further study on high-resolution climatic changes especially on moisture budget in the East Asian monsoonal region. (C) 2012 Elsevier Ltd. All rights reserved.