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

• Published in: Radiocarbon
• Main Authors: Noguchi, Makoto, Fujiki, Toshiyuki, Okuno, Mitsuru, Gualtieri, Lyn, Hatfield, Virginia, Sarata, Brenn, Torii, Masayuki, Wada, Keiji, Nakamura, Toshio, West, Dixie
• Format: Article in Journal/Newspaper
• Language: English
• Published: Cambridge University Press (CUP) 2018
• Subjects: General Earth and Planetary Sciences; Archeology; Adak; Haven Lake; aleut; Alaska; Aleutian Islands
• Online Access: http://dx.doi.org/10.1017/rdc.2018.103; https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033822218001030

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 μm 2 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.