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对秘鲁北部植物的碳氮同位素调查:古饮食和古生态学研究的基线。

Carbon and nitrogen isotopic survey of northern peruvian plants: baselines for paleodietary and paleoecological studies.

机构信息

Department of Anthropology, The University of Western Ontario, London, Ontario, Canada.

出版信息

PLoS One. 2013;8(1):e53763. doi: 10.1371/journal.pone.0053763. Epub 2013 Jan 16.

Abstract

The development of isotopic baselines for comparison with paleodietary data is crucial, but often overlooked. We review the factors affecting the carbon (δ(13)C) and nitrogen (δ(15)N) isotopic compositions of plants, with a special focus on the carbon and nitrogen isotopic compositions of twelve different species of cultivated plants (n = 91) and 139 wild plant species collected in northern Peru. The cultivated plants were collected from nineteen local markets. The mean δ(13)C value for maize (grain) was -11.8±0.4 ‰ (n = 27). Leguminous cultigens (beans, Andean lupin) were characterized by significantly lower δ(15)N values and significantly higher %N than non-leguminous cultigens. Wild plants from thirteen sites were collected in the Moche River Valley area between sea level and ∼4,000 meters above sea level (masl). These sites were associated with mean annual precipitation ranging from 0 to 710 mm. Plants growing at low altitude sites receiving low amounts of precipitation were characterized by higher δ(15)N values than plants growing at higher altitudes and receiving higher amounts of precipitation, although this trend dissipated when altitude was >2,000 masl and MAP was >400 mm. For C(3) plants, foliar δ(13)C was positively correlated with altitude and precipitation. This suggests that the influence of altitude may overshadow the influence of water availability on foliar δ(13)C values at this scale.

摘要

建立同位素基线以与古饮食数据进行比较至关重要,但往往被忽视。我们综述了影响植物碳(δ(13)C)和氮(δ(15)N)同位素组成的因素,特别关注了 12 种不同栽培植物(n=91)和在秘鲁北部采集的 139 种野生植物的碳和氮同位素组成。栽培植物来自 19 个当地市场。玉米(谷物)的平均 δ(13)C 值为-11.8±0.4 ‰(n=27)。豆科栽培种(豆类、安第斯羽扇豆)的 δ(15)N 值显著较低,而 %N 显著较高。从海拔 0 至 4000 米以上的莫切河谷地区的 13 个地点采集了 139 种野生植物。这些地点的年平均降水量从 0 至 710 毫米不等。在接收低降水量的低海拔地点生长的植物,其 δ(15)N 值高于在高海拔和接收高降水量的地点生长的植物,但当海拔>2000 米且 MAP>400 毫米时,这种趋势就消失了。对于 C(3)植物,叶片 δ(13)C 与海拔和降水呈正相关。这表明在这个尺度上,海拔的影响可能超过水分可用性对叶片 δ(13)C 值的影响。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/42b9/3547067/335a08b8a2d6/pone.0053763.g001.jpg

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