Cited by 9Tree-ring climate responsesArchaeology and ancient environmental studiesIsotope Analysis in Ecology

Sample preparation of ring-less tropical trees for δ18O measurement in isotope dendrochronology

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Nakai, Wataru, Okada, Naoki, Sano, Masaki, Nakatsuka, Takeshi·2018·Tropics

Abstract

Radial variation of δ18O before and after cellulose extraction was assessed in Acacia auriculiformis, Eucalyptus camaldulensis, and Celtis timorensis growing in northeastern Thailand to examine the necessity of extracting α-cellulose to detect annual rings from trees without visible rings. Optimum sampling resolution to detect peaks in the radial variation of δ18O values was also examined. Cored samples were sectioned into 0.2mm thickness in the radial direction. Each circular section sliced from a wood core sample were divided along wood grain into two semicircular sections, both of which were located at the same radial and longitudinal positions, and were side-by-side tangentially. One half was used for bulk analysis and the other for extraction. Peak positions were assigned from the seasonal variation of δ18O. The δ18O values cyclically changed in both bulk wood and α-cellulose. The correlation coefficient between bulk wood and α-cellulose δ18O was high in every species, and the offset was almost constant across the radial position. The mean cycle length of one sample was longer than those of the other two samples, although annual increment based on dendrometer monitoring was smaller than those of the other two samples. That is, the seasonal variation in δ18O values recorded in the xylem was not completely detected because of low amplitude or insufficient radial resolution. Therefore, we concluded that α-cellulose extraction is unnecessary for annual ring detection. It is necessary to determine an appropriate sampling resolution based on growth rate for effective peak detection.

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Crossref · 10.3759/tropics.ms17-09

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  • The IntCal criteria were expanded for this iteration to include dendrochronologies derived from δ18O pattern matching.

    “The criteria were expanded for this iteration of the curve to include dendrochronologies derived from δ 18 Opattern matching.”

    From The IntCal20 Northern Hemisphere Radiocarbon Age Calibration Curve (0–55 cal kBP) (2020) · cites this paper as Nakai et al. 2018

    The section on radial variation of δ18O discusses cross-dating tree chronologies, but not criteria for including them in an IntCal curve. Searches for IntCal, expanded criteria, and calibration-curve inclusion found no passage addressing the claim in our copy. (LLM, conf=0.76)

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Authors
Nakai, W., Okada, N., Sano, M., & Nakatsuka, T.
Affiliations
  • Kyoto University (JP)
  • Waseda University (JP)
  • Research Institute for Humanity and Nature (JP)
Venue
Tropics
Published
2018
Volume
27
Issue
2
Pages
49-58
ISSN
  • 0917-415X (ISSN-L)
  • 1882-5729
OpenAlex
W2888982041
Cited by
9
References
24
Citations by year
2023: 1 · 2022: 3 · 2021: 1 · 2020: 3 · 2019: 1
FWCI
0.61
Type
journal article
Language
en
Open access
Locations
Tropics (publishedVersion)
Funders
Japan Society for the Promotion of Science (17H02020, 23658127, 16K14943, 17H01621)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Tree-ring climate responses
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Archaeology and ancient environmental studies
  • Physical Sciences › Environmental Science › Ecology › Isotope Analysis in Ecology
Keywords
oxygen isotopes, δ18O, tropical trees, radial resolution, seasonal variation, Acacia auriculiformis, Eucalyptus camaldulensis, xylem

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