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评估美国东北部四个地点六种树木的整株木材和α-纤维素的年轮δC和δO值中记录的气候信号。

Evaluating climate signal recorded in tree-ring δ C and δ O values from bulk wood and α-cellulose for six species across four sites in the northeastern US.

作者信息

Guerrieri Rossella, Jennings Katie, Belmecheri Soumaya, Asbjornsen Heidi, Ollinger Scott

机构信息

Earth Systems Research Center, University of New Hampshire, Durham, NH, 03824, USA.

Laboratory of Tree Ring Research, University of Arizona, Tucson, AZ, 85721-0045, USA.

出版信息

Rapid Commun Mass Spectrom. 2017 Dec 30;31(24):2081-2091. doi: 10.1002/rcm.7995.

Abstract

RATIONALE

We evaluated the applicability of tree-ring δ C and δ O values in bulk wood - instead of the more time and lab-consuming α-cellulose δ C and δ O values, to assess climate and physiological signals across multiple sites and for six tree species along a latitudinal gradient (35°97'N to 45°20'N) of the northeastern United States.

METHODS

Wood cores (n = 4 per tree) were sampled from ten trees per species. Cores were cross-dated within and across trees at each site, and for the last 30 years. Seven years, including the driest on record, were selected for this study. The δ C and δ O values were measured on two of the ten trees from the bulk wood and the α-cellulose. The offsets between materials in δ C and δ O values were assessed. Correlation and multiple regression analyses were used to evaluate the strength of the climate signal across sites. Finally the relationship between δ C and δ O values in bulk wood vs α-cellulose was analyzed to assess the consistency of the interpretation, in terms of CO assimilation and stomatal conductance, from both materials.

RESULTS

We found offsets of 1.1‰ and 5.6‰ between bulk and α-cellulose for δ C and δ O values, respectively, consistent with offset values reported in the literature. Bulk wood showed similar or stronger correlations to climate parameters than α-cellulose for the investigated sites. In particular, temperature and vapor pressure deficit and standard precipitation-evaporation index (SPEI) were the most visible climate signals recorded in δ C and δ O values, respectively. For most of the species, there was no relationship between δ C and δ O values, regardless of the wood material considered.

CONCLUSIONS

Extraction of α-cellulose was not necessary to detect climate signals in tree rings across the four investigated sites. Furthermore, the physiological information inferred from the dual isotope approach was similar for most of the species regardless of the material considered.

摘要

原理

我们评估了整木中树木年轮的δC和δO值的适用性,而不是更耗时且需实验室操作的α-纤维素δC和δO值,以评估美国东北部沿纬度梯度(北纬35°97′至45°20′)的多个地点和六种树木的气候和生理信号。

方法

从每个物种的十棵树上采集木芯(每棵树n = 4)。在每个地点的树木内部和之间以及过去30年对木芯进行交叉定年。本研究选择了包括有记录以来最干旱年份在内的七年。对来自整木和α-纤维素的十棵树中的两棵测量其δC和δO值。评估了材料之间δC和δO值的偏移量。使用相关性和多元回归分析来评估各地点气候信号的强度。最后,分析了整木与α-纤维素中δC和δO值之间的关系,以评估两种材料在CO2同化和气孔导度方面解释的一致性。

结果

我们发现整木和α-纤维素之间的δC和δO值偏移量分别为1.1‰和5.6‰,与文献报道的偏移值一致。在所研究的地点,整木显示出与气候参数的相关性与α-纤维素相似或更强。特别是,温度和蒸气压亏缺以及标准降水蒸发指数(SPEI)分别是δC和δO值中记录的最明显的气候信号。对于大多数物种,无论考虑哪种木材材料,δC和δO值之间均无关系。

结论

对于四个研究地点的树木年轮,检测气候信号无需提取α-纤维素。此外,无论考虑哪种材料,大多数物种从双同位素方法推断出的生理信息相似。

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