Cited by 4Archaeology and ancient environmental studiesTree-ring climate responsesIsotope Analysis in Ecology

Possible Depletion in 14C in Trees Growing in Calcareous Soils

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Tauber, Henrik·1983·Radiocarbon

Abstract

14 C activities of decadal samples from beech trees growing under extreme calcareous conditions were compared to 14 C activities of decadal samples of the same age from a beech tree growing in a normal mold soil in order to see whether part of the carbon assimilated during photosynthesis might originate from 14 C-deficient carbonates in the soil. The calcareous soils contained from 18 to 52% calcium carbonate, and this carbonate had a mean 14 C age of 10,200 to 17,600 years BP. A comparison was also made with the 14 C activity of contemporaneous samples from Douglas Fir from the US North Pacific (Stuiver, 1982). No significant depletion in 14 C activity in beech trees growing in the highly calcareous soils was detected. The measured mean difference in 14 C activity in beech trees from calcareous and non-calcareous sites corresponds to an uptake of 0.12 ± 0.3% carbon from soil carbonates in the calcareous sites.

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Authors
Tauber, H.
Affiliations
National Museum of Denmark (DK)
Corresponding author
Tauber, Henrik
Venue
Radiocarbon
Published
1983
Volume
25
Issue
2
Pages
417-420
ISSN
  • 0033-8222 (ISSN-L)
  • 1945-5755
OpenAlex
W2498385671
Cited by
4
References
0
Citations by year
2012: 1
FWCI
0.00
Type
journal article
Language
en
Open access
Locations
  • Radiocarbon (publishedVersion)
  • UA Campus Repository (The University of Arizona) (acceptedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Archaeology and ancient environmental studies
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Tree-ring climate responses
  • Physical Sciences › Environmental Science › Ecology › Isotope Analysis in Ecology
Keywords
calcareous soils, soil carbonates, beech, Pseudotsuga menziesii, carbon assimilation, calcium carbonate

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