Is the modern-day dieback of yellow-cedar unprecedented?

Author:

Gaglioti B.V.12,Mann D.H.3,Wiles G.C.42,Wiesenberg N.4

Affiliation:

1. Water and Environmental Research Center, Institute of Northern Engineering, University of Alaska Fairbanks, Fairbanks, Alaska 99775, USA.

2. Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964, USA.

3. Institute of Arctic Biology, University of Alaska, Fairbanks, Alaska 99708, USA.

4. Department of Earth Sciences, The College of Wooster, Wooster, Ohio 44691, USA.

Abstract

In Southeast Alaska, many stands of yellow-cedar (Callitropsis nootkatensis (D. Don) Oerst. ex D.P. Little; hereinafter “YC”) contain numerous standing, dead snags. Snag-age estimates based on tree morphology have been used to support the interpretation that a warming climate after ca. 1880 has triggered unprecedented YC dieback. Here, we present new estimates of YC snag longevity by cross-dating 61 snags with morphologies that suggest they stood dead for extended periods. All but four of these snags have lost their outermost rings to decay, so we estimate when they died using a new method based on wood-ablation rates measured in six living trees that display partial cambial dieback. The results indicate that ∼59% of YC snags that lost their branches to decay (Class 5 snags) have remained standing for >200 years, and some for as long as 450 years (snag longevity mean ± SD: 233 ± 92 years). These findings, along with supporting evidence from historical photos, dendrochronology, and snag-morphology surveys in the published literature suggest that episodes of YC dieback also occurred before 1880 and before significant anthropogenic warming began. The roles played by climate change in these earlier dieback events remain to be further explored.

Publisher

Canadian Science Publishing

Subject

Ecology,Forestry,Global and Planetary Change

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