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Vegetation Changes around Haven Lake, Adak Island, Central Aleutians, Alaska, Determined from Pollen Analysis

Published online by Cambridge University Press:  19 November 2018

Makoto Noguchi
Affiliation:
Department of Applied Science, Graduate School of Science, Okayama University of Science, 1-1 Ridai-cho, Kita-ku, Okayama 700-0005, Japan
Toshiyuki Fujiki*
Affiliation:
Department of Applied Science, Faculty of Science, Okayama University of Science, 1-1 Ridai-cho, Kita-ku, Okayama 700-0005, Japan
Mitsuru Okuno
Affiliation:
Department of Earth System Science, Faculty of Science, Fukuoka University, 8-19-1 Nanakuma, Jonan-ku, Fukuoka 814-0180, Japan
Lyn Gualtieri
Affiliation:
Civil and Environmental Engineering, Seattle University, 901 12th Avenue Seattle, WA 98122, USA
Virginia Hatfield
Affiliation:
Museum of the Aleutians, 314 Salmon Way, PO BOX 648, Unalaska, AK 99685USA
Brenn Sarata
Affiliation:
Fugro Engineers BV, Prismastraat 4, 2631 RT, 2630 AC, Nootdorp, The Netherlands
Masayuki Torii
Affiliation:
Disaster Mitigation Laboratory, Center for Water Cycle, Marine Environment and Disaster Management, Kumamoto University, 2-39-1 Kurokami, Chuo-ku, Kumamoto 860-8555, Japan
Keiji Wada
Affiliation:
Hokkaido University of Education, 9 Kitamon-cho, Asahikawa, Hokkaido 070-8621, Japan
Toshio Nakamura
Affiliation:
Institute for Space-Earth Environmental Research, Nagoya University, Furo-cho, Chikusa-ku, Nagoya 464-8602, Japan
Dixie West
Affiliation:
Biodiversity Institute and Natural History Museum, The University of Kansas, 1345 Jayhawk Blvd. Lawrence, KS 66045, USA
*
*Corresponding author. Email: [email protected].

Abstract

We collected peat sediments (sediment core ADK13083002) from Haven Lake on the north side of Adak Island (central Aleutian Islands, Alaska) to determine whether the vegetation has changed. We confirmed the presence of six tephra layers, including Forty Years (0.3 cal ka BP), T2, YBO (3.3 cal ka BP), Intermediate (6.4 cal ka BP), Main (9.5 cal ka BP), and T6. We identified four major pollen assemblage zones (HL-1 to HL-4, in descending order) in the cored sediment. HL-1 was dominated by Ranunculaceae and Empetrum pollen; H-2 was dominated by Poaceae, Ranunculaceae, and Empetrum pollen; HL-3 was dominated by Poaceae and Empetrum pollen; and HL-4 was dominated by Poaceae, Cyperaceae, Lycopodiaceae, and Empetrum pollen. Small charcoal particles, likely transported from a distance, were found at low frequencies until 6.4 cal ka BP. The total cross-sectional area of charcoal particles increased to 1500 μm2 or more by 6.4 cal ka BP, implying that the large charcoal particles originated from nearby Aleut settlements, which were established around the same time.

Type
Water, Sediment, Karst
Copyright
© 2018 by the Arizona Board of Regents on behalf of the University of Arizona 

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Footnotes

Selected Papers from the 2nd Radiocarbon in the Environment Conference, Debrecen, Hungary, 3–7 July 2017

References

REFERENCES

Bank, TP II. 1952. Botanical and ethnobotanical studies in the Aleutian Islands. I. Aleutian vegetation and Aleut culture. Papers of the Michigan Academy of Science, Arts and Letters 37:1330.Google Scholar
Black, RF. 1976. Late Quaternary glacial events, Aleutian Islands, Alaska. In: Easterbrook DJ, Sibrava V, editors. Quaternary Glaciations in the Northern Hemisphere. INQUA. p 285301.Google Scholar
Davis, RS, Knecht, RA. 2010. Continuity and change in the eastern Aleutian archaeological sequence. Human Biology 82:507524 Google Scholar
Erdtman, G. 1934. Über die verwendund von essigsäureanhydrid bei pollenuntersuchungen. Svenska Botanica Tiddskrift 28:354361.Google Scholar
Fujiki, T, Okuno, M, Moriwaki, H, Nakamura, T, Kawai, K, McComack, G, Cowan, G, Maoate, P. 2014. Vegetation changes viewed from pollen analysis in Rarotonga, southern Cook Islands, eastern Polynesia. Radiocarbon 56(2):699708.Google Scholar
Fujiki, T, Miyoshi, N, Kimura, H. 2016. Pollen Flora of Japan. 2nd edition. Sapporo, Japan: Hokkaido University Press. 1016 p.Google Scholar
Heusser, CJ. 1978. Postglacial vegetation on Adak Island, Aleutian Islands, Alaska. Bulletin of the Torrey Botanical Club 105:1823.Google Scholar
Heusser, CJ, Peteet, DM. 1988. Spore of Lycopodium and Selaginella of North Pacific America. Canadian Journal of Botany 66(3):508525.Google Scholar
Heusser, CJ. 1990. Late Quaternary vegetation of the Aleutian Islands, southwestern Alaska. Canadian Journal of Botany 68:13201326.Google Scholar
Hughes, PDM, Mallon, G, Brown, A, Essex, HJ, Stanford, JD, Hotes, S. 2013. The impact of high tephra loading on late-Holocene carbon accumulation and vegetation succession in peatland communities. Quaternary Science Reviews 67:160175.Google Scholar
Hultén, E. 1960. Flora of the Aleutian Islands. Cramer, Weinheim. 376 p.Google Scholar
Kitagawa, H, Masuzawa, T, Nakamura, T, Matsumoto, E. 1993. A batch preparation method for graphite targets with low back ground for AMS 14C measurements. Radiocarbon 35:295300.Google Scholar
Kito, N, Ohtsuki, J, Tsuji, S, Tsuji, K. 2017. The impact of tephra fall on vegetation and long-term recovery processes: A case study of the mid-Holocene Towada-Chuseri Tephra fall. Japanese Association of Historical Botany 26(1):1526.Google Scholar
Koizumi, T. 2009. Transition of the distribution of alpine and sub-alpine vegetation after the last glacial period and present alpine environment. In: Masuzawa T, editor. Alpine Botany – Alpine Environment and General Science of Plants. Tokyo: Kyoritsu Publishing. p 1733. In Japanese.Google Scholar
Krawiec, ACL, Kaufman, DS, Vaillencourt, DA. 2013. Age models and tephrostratigraphy from two lakes on Adak Island, Alaska. Quaternary Geochronology 18:4153.Google Scholar
Laughlin, WS, Jorgensen, J, Frohlich, B. 1979. Aleuts and Eskimos: Survivors of the Bering land bridge coast. In: Laughlin WS, Harper AB. editors. The First Americans: Origins, Affinities, and Adaptations. New York: Gustav Fischer. p 91104.Google Scholar
Nakamura, J. 1980a. Diagnostic characters of pollen grains of Japan, part I. Special Publications from the Osaka Museum of Natural History 13. 91 p. In Japanese.Google Scholar
Nakamura, J. 1980b. Diagnostic characters of pollen grains of Japan, part II. Special Publications from the Osaka Museum of Natural History 12. 157 p. In Japanese.Google Scholar
Nakamura, T, Niu, E, Oda, H, Ikeda, A, Minami, M, Ohta, T, Oda, T. 2004. High precision 14C measurements with the HVEE Tandetron AMS system at Nagoya University. Nuclear Instruments and Methods in Physics Research B 223–224:124129.Google Scholar
Nasu, T, Seto, K. 1986a. Spore morphology of Japanese pteridophytes, part I. Special Publications from the Osaka Museum of Natural History 18. 42 p.Google Scholar
Nasu, T, Seto, K. 1986b. Spore morphology of Japanese pteridophytes part I. (plates). Special Publications from the Osaka Museum of Natural History 16–17. 174 p.Google Scholar
O’Leary, M. 2001. Volcanic ash stratigraphy for Adak Island, central Aleutian archipelago, In: Dumond DE, editor. Archaeology in the Aleut Zone of Alaska. University of Oregon Anthropological Papers 58. Eugene: Museum of Natural and Cultural History, University of Oregon. p 215233.Google Scholar
Okuno, M, Gualtieri, L, West, D, Wilmerding, EG, Nakamura, T. 2007. Aleut shell mounds intercalated with tephra layers in Adak Island and Adjacent volcanoes in the west-central Aleutians, Alaska, USA. The Journal of the Geological Society of Japan 113(8):XIXII.Google Scholar
Okuno, M, Wada, K, Nakamura, T, Gualtieri, L, Brenn, S, Dixie, W, Torii, M. 2012. Holocene tephra layers on the northern half of Adak Island in the west-central Aleutian Islands, Alaska. In: West D, Hatfield V, Wilmerding E, Lefèvre C, Gualtieri L, editors. The People Before: The Geology, Paleoecology and Archaeology of Adak Island, Alaska. British Archaeological Reports International Series 2322. Oxford. p 5974.Google Scholar
Reimer, PJ, Bard, E, Bayliss, A, Beck, JW, Blackwell, PG, Bronk Ramsey, C, Buck, CE, Cheng, H, Edwards, RL, Friedrich, M, Grootes, PM, Guilderson, TP, Haflidason, H, Hajdas, I, Hatté, C, Heaton, TJ, Hoffmann, DL, Hogg, AG, Hughen, KA, Kaiser, KF, Kromer, B, Manning, SW, Niu, M, Reimer, RW, Richards, DA, Scott, EM, Southon, JR, Staff, RA, Turney, CSM, van der Plicht, J. 2013. IntCal13 and Marine13 radiocarbon age calibration curves 0–50,000 years cal BP. Radiocarbon 55(4):18691887.Google Scholar
Saito-Kokubu Y, Matsubara A, Miyake M, Nishizawa A, Ohwaki Y, Nishio T, Sanada K, Hanaki T. 2015. Progress on multi-nuclide AMS of JAEA-AMS-TONO. Nuclear Instruments and Methods in Physics Research Section B 361: 48–53.Google Scholar
Savinetsky, AB, West, D, Antipushima, ZA, Khassanov, BF, Kiseleva, NK, Krylovich, OA, Pereladov, AM. 2012. The reconstruction of ecosystems history of Adak Island (Aleutian Islands) during the Holocene. In: West D, Hatfield V, Wilmerding E, Lefèvre C, Gualtieri L, editors. The People Before: The Geology, Paleoecology and Archaeology of Adak Island, Alaska. British Archaeological Reports International Series 2322. Oxford. p 75106.Google Scholar
Stuiver, M, Reimer, PJ. 1993. Extended 14C data base and revised CALIB 3.0 14C age calibration program. Radiocarbon 35(1):215230.Google Scholar
Takiya, M, Hagiwara, N. 1997. Vegetation history of Mt. Yokotsudake, southwestern Hokkaido, since the last glacial. Quaternary Research (Daiyonki Kenkyu) 35:217234. In Japanese with English abstract.Google Scholar
van der Leeden, F, Troise, FL. 1974. Climates of the States: A Practical Reference Containing Basic Climatological Data of the United States. Port Washington (NY): Water Information Center. 975 p.Google Scholar
West, D, Lefevre, D, Corbett, A, Savinetsky, B. 1999. Radiocarbon dates for the Near Islands, Aleutian Islands, Alaska. Current Research in the Pleistocene 16:8385.Google Scholar