Leipe, Christian; Müller, Stefanie; Hille, Konrad; Kato, Hirofumi; Kobe, Franziska; Schmidt, Mareike; Seyffert, Konrad; Spengler III, Robert; Wagner, Mayke; Weber, Andrzej W; Tarasov, Pavel E (2018): Surface pollen assemblages from Rebun Island, common fossil pollen taxa recorded in the RK12 sediment core (Lake Kushu) and dimensional measurements of charred barley grains from the Hamanaka 2 archaeological site (Rebun Island) [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.890926, Supplement to: Leipe, C et al. (2018): Vegetation change and human impacts on Rebun Island (Northwest Pacific) over the last 6000 years. Quaternary Science Reviews, 193, 129-144, https://doi.org/10.1016/j.quascirev.2018.06.011
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Abstract:
This study presents a high-resolution, chronologically well-constrained pollen record from Lake Kushu (45°25′58″N, 141°02′05″E) and a record of archaeobotanical remains from the nearby Hamanaka 2 archaeological site. The pollen record suggests continuous long-term cooling, which parallels the decline in Northern Hemisphere summer insolation. This cooling trend is overlaid by several rather quick transitions towards cooler conditions (ca. 5540/5350, 1550, and 390 cal BP) and one distinct decadal-scale cold event around 4130 cal BP. These shifts, on one hand, correspond with major hemispherical or global-scale climate transitions/events, including the 'Holocene Climate Transition', the onset of the 'Dark Ages Cold Period' main phase, the 'Little Ice Age', and the '4.2 kiloyear event', respectively. On the other hand, the shifts partly coincide with transformations in the Hokkaido prehistoric cultural sequence including the onset of the Middle Jomon (ca. 5000 cal BP), the Middle/Late Jomon transition (ca. 4000 cal BP), the immigration of Okhotsk culture groups (from ca. 1500 cal BP), and the establishment of the Classic Ainu culture (ca. 350 cal BP). AMS radiocarbon dating of charred macrobotanical remains from Hamanaka 2 suggests three discontinuous occupational periods ca. 390–50 BCE, 420–970 CE, and from 1640 CE, which correspond to the northern Hokkaido Epi Jomon (ca. 300–100 BCE), Okhotsk (ca. 500–1000 CE), and Classic Ainu (ca. 1600–1868 CE) cultural phases, respectively. While impact on the island's natural environments (forest clearance) was marginal during the Epi Jomon phase, it became significant during the Okhotsk and the Classic Ainu culture phases.
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Coverage:
Median Latitude: 45.422250 * Median Longitude: 141.010500 * South-bound Latitude: 45.340000 * West-bound Longitude: 140.970000 * North-bound Latitude: 45.460000 * East-bound Longitude: 141.050000
Event(s):
Hamanaka2 * Latitude: 45.433000 * Longitude: 141.010000 * Location: northern Rebun Island, Hokkaido, Japan * Comment: Hamanaka 2 archaeological site (northern Rebun Island).
Comment:
This dataset contains 3 Supplemental files including (i) absolute counts of surface pollen samples collected across Rebun Island (Hokkaido, northern Japan), (ii) a photographic documentation of the most common fossil pollen and spore taxa recorded in the upper part (10.4 m, ca. 6000-270 cal BP) of the RK12 sediment core extracted from Lake Kushu (northern Rebun Island), and (iii) dimensional and weight measurements of charred barley grains recovered from cultural layers of the Hamanaka 2 archaeological site (northern Rebun Island).
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
2 datasets
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Datasets listed in this publication series
- Leipe, C; Müller, S; Hille, K et al. (2018): Supplemental table S1: Absolute counts of surface pollen samples collected across Rebun Island (Hokkaido, northern Japan). https://doi.org/10.1594/PANGAEA.890924
- Leipe, C; Müller, S; Hille, K et al. (2018): Supplemental table S3: Dimensional and weight measurements of charred barley grains recovered from cultural layers of the Hamanaka 2 archaeological site, northern Rebun Island, Japan. https://doi.org/10.1594/PANGAEA.890925