Subtropical montane vegetation dynamics in response to Holocene climate change in central Taiwan
Author:
Funder
National Science and Technology Council
Publisher
Springer Science and Business Media LLC
Subject
Paleontology,Plant Science,Archeology
Link
https://link.springer.com/content/pdf/10.1007/s00334-024-00988-8.pdf
Reference75 articles.
1. Adhikari DP, Kumon F, Kawajiri K (2002) Holocene climate variability as deduced from the organic carbon and diatom records in the sediments of Lake Aoki, central Japan. J Geol Soc Jpn 108:249–265. https://doi.org/10.5575/geosoc.108.249
2. Birks HJB, Line JM (1992) The use of Rarefaction Analysis for estimating Palynological Richness from Quaternary Pollen-Analytical Data. Holocene 2:1–10. https://doi.org/10.1177/095968369200200101
3. Blaauw M, Christen JA (2011) Flexible paleoclimate age-depth models using an autoregressive gamma process. Bayesian Anal 6:457–474. https://doi.org/10.1214/ba/1339616472
4. Cartapanis O, Jonkers L, Moffa-Sanchez P et al (2022) Complex spatio-temporal structure of the Holocene Thermal Maximum. Nat Commun 13:5662. https://doi.org/10.1038/s41467-022-33362-1
5. Chen S-H, Wu J-T (1999) Paleolimnological environment indicated by the diatom and pollen assemblages in an alpine lake in Taiwan. J Paleolimnol 22:149–158
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