Marine diatoms as a stratigraphic indicator for Quaternary sediments : Focusing on the potential biostratigraphic indicator for coastal shallow marine deposits
Author:
Affiliation:
1. Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST)
Publisher
Japan Association for Quaternary Research
Subject
General Earth and Planetary Sciences,General Environmental Science
Link
https://www.jstage.jst.go.jp/article/jaqua/58/4/58_289/_pdf
Reference48 articles.
1. Akiba, F. (1986) Middle Miocene to Quaternary diatom biostratigraphy in the Nankai Trough and Japan Trench, and modified lower Miocene through Quaternary diatom zones for middle-to-high latitudes of the North Pacific. Kagami, H. et al. (eds.) Initial Reports of the Deep Sea Drilling Project, 87, 393-481.
2. Akutsu, J. (1973) Geology of the Kawasaki to Kisarazu subsurface section, central part of Tokyo Bay, Japan. The science reports of the Tohoku University, Second series (Geology), special volume 6 (Hatai Memorial Volume), 465-476.
3. Alverson, A.J. (2014) Timing marine-freshwater transitions in the diatom order Thalassiosirales. Paleobiology, 40, 91-101.
4. Alverson, A.J., Kang, S.-H. and Theriot, E.C. (2006) Cell wall morphology and systematic importance of Thalaisiosira ritscheri (Hustedt) Hasle, with a description of Shionodiscus gen. nov. Diatom Research, 21, 251-262.
5. Alverson, A.J., Jansen, R.K. and Theriot, E.C. (2007) Bridging the Rubicon : phylogenetic analysis reveals repeated colonizations of marine and fresh waters by thalassiosiroid diatoms. Molecular Phylogenetics and Evolution, 45, 193-210.
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