We reconstructed the vegetation history in and around the Minamihama Mire in a maar on Rishiri Island, northern Hokkaido dating back to ca. 5,500 cal BP. This reconstruction is based on the analysis of plant remains and pollen from three core samples taken from different parts of the mire, including both the margin and the central areas. After volcanic eruptions ceased, wetland vegetation started to grow around 5,500 cal BP in the maar. Ombrotrophic bogs, dominated by
Sphagnum moss, began to form around 4,100 years ago in the central part of the maar. However, minerotrophic bogs persisted along the margin of the mire until about 220 cal BP due to the inflow of surface water from the maar slope.
Picea glehnii forest started spreading into the wetland around 1,340 cal BP possibly due to a decrease in the moisture level on the bog’s surface. The lowland forests on Rishiri Island, including the maar slope, were a mixed coniferous and broadleaved forest dominated by deciduous Quercus until around 3,100 cal BP since the middle Holocene climate optimum. The Late Holocene climate deterioration led to a shift in the dominant tree species within the forests, with conifers such as
Abies sachalinensis and
Picea becoming prevalent. The forest on the maar wall was eliminated before ca. 80 cal BP and has since transitioned to the current bamboo community.
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