@article{oai:kanazawa-u.repo.nii.ac.jp:00055342,
 author = {田中, 源吾 and Tanaka, Gengo},
 issue = {3},
 journal = {Earth Science, 地球科学},
 month = {Jun},
 note = {島根県,出雲市菅沢の大森層より26属42種の介形虫化石を抽出し,2つの介形虫群(Ambostracon-Argilloecia-Cytheropteron群集およびPaijenborchella-Palmoconcha-Urocythereis pohangensis群集)を認めた.これらの群集は冷温〜温暖な公海の下浅海環境を示唆する.大森層および布志名層からの介形虫化石群の主成分分析は,その堆積環境が上部層準に向かってしだいに深くなっていったことを示唆する.5新種(Cytheropteron shimanense, Loxoconcha izumoensis, Paradoxostoma yakumotatsunus, Schizocythere sakanoueiおよびUrocythereis sugesawensis)を記載した., Ostracods from the Omori Formation in Sugesawa (Izumo City, Shimane Prefecture) comprise 42 species belonging to 26 genera. Five new species, Cytheropteron shimanense, Loxoconcha izumoensis, Paradoxostoma yakumotatsunus, Schizocythere sakanouei and Urocythereis sugesawensis are described. Two ostracod assemblages (Ambostracon-Argilloecia-Cytheropteron assemblage and Paijenborchella-Palmoconcha-Urocythereis pohangensis assemblage) are recognized. These assemblages indicate that the uppermost of the Omori Formation was deposited under the environments from cool to warm open sublittoral condition. Principal components analysis of ostracod assemblages from the Omori and Fujina Formations indicates that, in general, the depositional environment becomes deeper and deeper towards the upper horizon., 金沢大学国際基幹教育院GS教育系},
 pages = {111--127},
 title = {Middle Miocene ostracods from the Omori Formation, Izumo City, Southwest Japan},
 volume = {57},
 year = {2003}
}