Characteristic of Si:P:N ratio in bottom water in central Suo-Nada, western Seto Inland Sea
Author:
Publisher
Springer Science and Business Media LLC
Subject
Oceanography
Link
http://link.springer.com/content/pdf/10.1007/s10872-014-0262-4.pdf
Reference18 articles.
1. Abe K, Nakagawa N, Abo K, Tsujino M (2014) Dissolution of silica accompanied by oxygen consumption in the bottom layer of Japan’s central Seto Inland Sea in summer. J Oceanogr 70:267–276
2. Brzezinski MA (1985) The Si:C: N ratio of marine diatoms: interspecific variability and the effect of some environmental variables. J Phycol 21:347–357
3. Fujiwara T, Takasugi Y, Higo T (1989) Wind-induced phenomena in stratified basins. Bull Coast Oceanogr 27–1:38–46 (in Japanese with English abstract)
4. Gaider RJ, La Roche J (2002) Redfield revisited: variability of C:N: P in marine microalgae and its biogeochemical basis. Eur J Phycol 37:1–17
5. Iwao T (2001) Fluctuation in the water quality of the coastal zone along Suo-Nada in Oita prefecture. Bull Oita Ins Mar Fish Sci 3:19–25
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1. Seasonal variation in the current field and development of bottom cold water in Harima-Nada;Journal of Oceanography;2023-08-30
2. Interannual variation of a bottom cold water mass in the Seto Inland Sea, Japan;Ocean Science;2022-05-10
3. Si(OH)4- AOU characteristics in bottom water of Seto Inland Sea, Japan, in summer;Regional Studies in Marine Science;2017-05
4. Nutrient dynamics in core sediments of an artificial basal medium prepared with steelmaking slag and dredged materials;Journal of Oceanography;2016-06-29
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