阿尔泰山泥炭α-纤维素碳和氧同位素的古环境意义——以黑阳坡泥炭为例

doi:10.13866/j.azr.2022.01.04

Abstract

Abstract:

The Altai Mountains are affected by westerlies all year round and are therefore the focus of paleoclimate research. To explore the rationnality of using the modern process of carbon and oxygen isotopes from peat plants in centennial-or millennial-scale paleoclimate reconstruction in the Altai Mountains, we analyzed the relationship between the α-cellulose carbon and oxygen isotopes (δ ¹³C_cell and δ¹⁸O_cell) of Heiyangpo peatland and the meteorological parameters (temperature, precipitation, and relative humidity) measured in the cold season (October-April), warm season (May-September), and annually from Habahe station from 1962 to 2017. Significant relationships were found between δ¹³C_cell and relative humidity in May-August(r=-0.52, P<0.05), and between δ¹⁸O_cell and precipitation in November-January(r=0.49, P<0.05). Thus, δ¹³C_cell and δ¹⁸O_cell values are reliable proxies of May-August relative humidity and November-January precipitation, respectively. Our work provides multi-year scale data support for the interpretation of paleoclimate information recorded by peat cellulose isotopes in the Altai Mountains. The research not only informs the modern process study of peat isotopes in China, but also has great significance for quantitative paleoclimate reconstruction in areas using peat cellulose isotopes over long periods.

Key words: Heiyangpo peatland, carbon and oxygen isotopes, observed interval, Altai Mountains

LIU Qi,XU Zhonglin,ZHANG Dongliang. Paleoenvironmental implications of α-cellulose carbon and oxygen isotopes from Heiyangpo peatland in the Altai Mountains[J].Arid Zone Research, 2022, 39(1): 30-40.

Figures/Tables 7

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Paleoenvironmental implications of α-cellulose carbon and oxygen isotopes from Heiyangpo peatland in the Altai Mountains

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