Premium
Holocene sedimentary history of some coastal plains in Hokkaido, Japan IV. Diatom assemblages in the sediments from Kushiro moor (2)
Author(s) -
Kumano Shigeru,
Ihira Masashi,
Maeda Yasuo,
Yamauchi Misako,
Matsumoto Eiji,
Matsuda Isao
Publication year - 1990
Publication title -
ecological research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.628
H-Index - 68
eISSN - 1440-1703
pISSN - 0912-3814
DOI - 10.1007/bf02346993
Subject(s) - holocene , marine transgression , peat , geology , bay , sedimentary rock , brackish water , diatom , oceanography , paleontology , archaeology , structural basin , geography , salinity
Diatom assemblages of sediments obtained from three sites on Kushiro Moor were analyzed to investigate the Holocene sedimentary history. The results showed that: 1) The Takkobu site was originally at the bottom of the paleo‐Kushiro Bay, and after‐wards the paleo‐Takkobu Lagoon developed, became sealed off, and changed to a freshwater lake. The succession to peat moor probably began about 2000 yr B.P. at the Takkobu site. 2) The Tsurui site was originally at the bottom of the paleo‐Kushiro Bay, then changed to the paleo‐Kushiro Lagoon and became peat moor as a result of the first Holocene regression, which finished about 3600 yr B.P. The site then returned to a brackish lake again, probably due to the second Holocene transgression between 3600 and 3000 yr B.P., thereafter passing through brackish lake and freshwater lake stages, and eventually becaming peat moor at about 2000 yr B.P., 3) At the Chuo site, the second paleo‐Kushiro Bay developed again as a result of the second Holocene transgression, which finished about 3000 yr B.P. Thereafter, brackish or freshwater lakes, rivers, and then peat moor developed in the central area of Kushiro Moor. 4) The second marine diatom zone (MD 2 Zone), which indicates the second Holocene transgression, complete by about 3000 yr B.P., is detected only at the Chuo site in the central area of Kushiro Moor.