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首页> 外文期刊>Biogeosciences >Carbon isotope discrimination of C3 vegetation in Central Asian grassland as related to long-term and short-term precipitation patterns
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Carbon isotope discrimination of C3 vegetation in Central Asian grassland as related to long-term and short-term precipitation patterns

机译:中亚草原C3植被的碳同位素判别与长期和短期降水模式的关系

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The relationship between carbon isotope discrimination (13Δ) of C3vegetation and long-term (30 years) and short-term (growing period)precipitation was investigated. Different species of Stipa, adominant grass genus in the (semi-)arid Asian steppes, and other C3 specieswere collected along aridity gradients in Inner Mongolia in 2005 (11 sites,71 samples) and in the Republic of Mongolia in 2006 (40 sites, 45 samples).The data set was expanded with published and unpublished data ofStipa and other C3 species (11 studies covering 8 years, including64 observations of Stipa, and 103 observations of other C3 species)and C3 community bulk-samples (11 samples). Weather data weregeostatistically interpolated for all sampling sites and years. 13Δ of Stipa followed different relationships for the individual yearswhen related to mean annual precipitation due to large anomalies betweenannual and long-term average precipitation patterns. However, the13Δ response to rainfall converged when the (long-term) meanannual precipitation was replaced by year-specific mean daily precipitationduring the growing period ( style="border-top: 1px solid #000;">PG). Remarkably, the 13Δ-response to ( style="border-top: 1px solid #000;">PG) for C3 species as a whole (including herbaceousdicots, semi-shrubs and grasses) and also the C3 community-level responsewere virtually identical to that of Stipa. The relation was alsovalid outside the geographical and climatic range where it was developed,giving proof of its robustness.
机译:研究了C3植被碳同位素判别( 13 Δ)与长期(30年)和短期(生长期)降水之间的关系。 2005年在内蒙古(共11个地点,71个样本)沿干旱梯度收集了不同物种的(i)Stipa ,(半)干旱亚洲草原的优势草属以及其他C3物种。蒙古于2006年(40个站点​​,45个样本)。该数据集扩展了 Stipa 和其他C3物种的已公开和未公开数据(涵盖8年的11个研究,其中包括 Stipa 的64个观测值) i>,以及其他C3物种的103个观测值)和C3群落整体样本(11个样本)。对所有采样地点和年份的天气数据进行了地统计插值。 Stipa 的 13 Δ在个体年中遵循不同的关系,这与年平均降水模式和长期平均降水模式之间的异常有关,这与年平均降水量有关。但是,当(长期)平均年降水量替换为生长期的特定年份的年平均日降水量时, 13 Δ对降雨的响应会收敛( style =“ border-top: 1px实心#000;“> P G )。值得注意的是, 13 Δ响应( style =“ border-top:1px solid#000;”> P G )对整个C3物种(包括草木,半灌木和草)以及C3群落水平的响应与 Stipa 几乎相同。该关系在其发展的地理和气候范围之外也是有效的,从而证明了其鲁棒性。

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