Authors Liu, Xian-zhao; Zhang, Yong; Li, Zhen-guo; Feng, Teng; Su, Qing; Song, Yan
Journal ECOLOGY AND EVOLUTION , DEC 2017,24:7
DOI 10.1002/ece3.3548 PubMed 29299240
Abstract Plant C-13-temperature (-T) relation has been established in many systems and is often used as paleotemperature transfer function. However, it is still unclear about the exact contributions of temperature variation to plant C-13 discrimination because of covariation between temperature and precipitation (aridity), which reduces confidence in reconstruction of paleoclimate. In this study, we measured carbon isotope composition (C-13) of 173 samples of C3 perennial herbs from 22 sites across a temperature gradient along the 400mm isohyet in the farming-pastoral zone of North China. The results showed that precipitation obviously affected the correlations of temperatures and foliar C-13. After removing the influence of precipitation by analysis of covariance (ANCOVA), a more strongly positive relationship was obtained between site-mean foliar C-13 and annual mean temperature (AMT), with a regression coefficient of 0.1636 parts per thousand/degrees C (p=.0024). For widespread species, Artemisia lavandulaefolia and Artemisia capillaries, the slopes (or coefficients) of foliar C-13 and AMT were significantly steeper (larger) than those of foliar C-13 and AMT where the precipitation influence was not excluded, whereas the -T coefficients of Polygonum persicaria and Leymus chinensis showed little change across the transect after deducting the precipitation effect. Moreover, the positive relationship between temperature and C-13 over the transect could be explained by soil moisture availability related to temperature. Our results may afford new opportunities for investigating the nature of past climate variability.
Species covered 春蓼 Polygonum persicaria 蒿属 Artemisia 野艾蒿 Artemisia lavandulaefolia
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