Biogeochemical evidence of Holocene East Asian summer and winter monsoon variability from a tropical maar lake in southern China

• Published in: Quaternary science reviews Vol. 111; pp. 51 - 61
• Main Authors: Jia, Guodong, Bai, Yang, Yang, Xiaoqiang, Xie, Luhua, Wei, Gangjian, Ouyang, Tingping, Chu, Guoqiang, Liu, Zhonghui, Peng, Ping'an
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01.03.2015
• Subjects: East Asian monsoon; ENSO; Holocene; Isotope proxy; Tropical lake record; East Asian monsoon; Isotope proxy; Tropical lake record; ENSO; Holocene
• ISSN: 0277-3791; 1873-457X
• DOI: 10.1016/j.quascirev.2015.01.002

Lake Huguangyan (21°9′ N, 110°17′ E), a maar lake located near the South China Sea, can provide valuable sedimentary data regarding past changes of the East Asian monsoonal system. Here, we used the proxies of TOC, δ13Corg, δ15N, and leaf wax n-alkane δ13C values (δ13Cwax) to reconstruct the lake conditions, which, in turn, revealed patterns in monsoonal changes during the Holocene. Two distinct patterns of proxy changes were identified in the sedimentary profile. A marked shift in the δ13Cwax value at ∼9.2ka (thousand years ago) suggests the abrupt disappearance of C4 plants, signaling the enhancement of East Asian summer monsoon (EASM). Between 9.2 and 1.8ka, a nearly pure C3 terrestrial ecosystem was present, with the climax at ca 7–6ka. After ca 3ka, fewer tropical species and a reappearance of C4 plants at 1.8ka indicate a weakened EASM in the late Holocene. The TOC concentration and δ15N value proxies appear to be associated with lake aquatic production and upwelled nutrient supply and utilization, which are modulated by, and thus indicative of, the strength of the East Asian winter monsoon (EAWM). The two EAWM records suggest a weakening trend from the early to late Holocene, with the most significant transition at ∼6ka; thus, the EAWM trend was broadly in-phase with that of the EASM. However, the marked EASM intensification at 9.2ka occurred within the period of a strong EAWM between 10.5 and 6ka and lagged the monsoonal enhancement as inferred from the Dongge Cave δ18O values. Our EASM records displays an overall arid-wet-arid pattern, which is in-phase with the hydrological variability in tropical Australia and anti-phase with that in the outer-tropical Andes. These phase relationships might be linked to changes in the thermal state of the tropical Pacific during the Holocene. •Abrupt C4 plant vanishing and lake level rise at ∼9.2ka due to intensified EASM.•Less tropical species and C4 plant reappearance in late Holocene.•TOC and δ15N suggest declining EAWM from early to late Holocene.•Millennial changes in EASM are linked to mean ENSO state.