4.6 Article

C3 plant carbon isotope discrimination does not respond to CO2 concentration on decadal to centennial timescales

期刊

NEW PHYTOLOGIST
卷 229, 期 5, 页码 2576-2585

出版社

WILEY
DOI: 10.1111/nph.17030

关键词

atmosphere; biogeochemistry; carbon; climate; evolution; isotopes; paleoclimate; plants

资金

  1. NSF [1812949]
  2. Geological Society of America
  3. Directorate For Geosciences [1812949] Funding Source: National Science Foundation
  4. Division Of Earth Sciences [1812949] Funding Source: National Science Foundation

向作者/读者索取更多资源

The study tested the impact of various climate factors on plant carbon isotope discrimination and found that climate variables are not the main driver of carbon isotope discrimination. It was discovered that the discrimination is intrinsic to each taxon and can quantitatively link phylogenetic relationships and adaptation to climate.
Plant carbon isotope discrimination is complex, and could be driven by climate, evolution and/or edaphic factors. We tested the climate drivers of carbon isotope discrimination in modern and historical plant chemistry, and focus in particular on the relationship between rising [CO2] over Industrialization and carbon isotope discrimination. We generated temporal records of plant carbon isotopes from museum specimens collected over a climo-sequence to test plant responses to climate and atmospheric change over the past 200 yr (including Pinus strobus, Platycladus orientalis, Populus tremuloides, Thuja koraiensis, Thuja occidentalis, Thuja plicata, Thuja standishii and Thuja sutchuenensis). We aggregated our results with a meta-analysis of a wide range of C-3 plants to make a comprehensive study of the distribution of carbon isotope discrimination and values among different plant types. We show that climate variables (e.g. mean annual precipitation, temperature and, key to this study, CO2 in the atmosphere) do not drive carbon isotope discrimination. Plant isotope discrimination is intrinsic to each taxon, and could link phylogenetic relationships and adaptation to climate quantitatively and over ecological to geological time scales.

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