A multi-proxy paleoenvironmental interpretation spanning the last glacial cycle (ca. 117 ± 8.5 ka BP) from a lake sediment stratigraphy from Lake Kai Iwi, Northland, New Zealand
Author:
Funder
AINSE
Publisher
Springer Science and Business Media LLC
Subject
Earth-Surface Processes,Aquatic Science
Link
https://link.springer.com/content/pdf/10.1007/s10933-020-00151-z.pdf
Reference74 articles.
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2. Appleby PG, Oldfield F (1978) The calculation of lead-210 dates assuming a constant rate of supply of unsupported 210Pb to the sediment. CATENA 5:1–8
3. Augustinus P, D’Costa D, Deng Y, Hagg J, Shane P (2011) A multi-proxy record of changing environments from ca. 30,000 to 9000 cal. a BP: Onepoto maar palaeolake, Auckland, New Zealand. J Quat Sci 26:389–401
4. Blaauw M, Christen JA (2011) Flexible paleoclimate age-depth models using an autoregressive gamma process. Bay Anal 6:457–474. https://doi.org/10.1214/11-BA618
5. Chagué-Goff C, Chan JCH, Goff J, Gadd P (2016) Late Holocene record of environmental changes, cyclones and tsunamis in a coastal lake, Mangaia, Cook Islands. Isl Arc 25:333–349. https://doi.org/10.1111/iar.12153
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