posted on 2025-03-13, 09:55authored byChieko Shimada, Shu Ozawa, Yuichiro Tanaka, Naoki Nemoto, Makoto Yamasaki
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<p><strong>Table OD-1.csv</strong>; <strong>Table OD-1.jpg</strong>: Occurrence list of diatoms from the type locality of the Kuromatsunai Formation, western Hokkaido, northern Japan. The definition of the diatom datum planes and their ages is based on Yanagisawa and Akiba (1998) and Yanagisawa and Watanabe (2011). </p>
<p><em>N. ko-N. ka</em>: <em>N. koizumii</em>-<em>N. kamtschatica</em>; <em>N. ko</em>: <em>N. koizumii</em>; G: good; M: moderate; P: poor. </p>
<p>Asterisk (*): present; dagger (†): not included in the total counts.</p>
<p>References:</p>
<p>Yanagisawa, Y. and Akiba, F. (1998) Refined Neogene diatom biostratigraphy for the northwest Pacific around Japan, with an introduction of code numbers for selected diatom biohorizons. Jour Geol Soc Japan, 104: 395-414. DOI <a href="https://doi.org/10.5575/geosoc.104.395" target="_blank">https://doi.org/10.5575/geosoc.104.395</a> </p>
<p>Yanagisawa, Y. and Watanabe, M. (2011) Data report of the Neogene and Quaternary diatom biostratigraphy in the Toga and Funakawa district, Oga Peninsula, Akita Prefecture, Japan, no. 533, Geol. Surv. Japan, AIST.</p>
Table OD-1.csv; Table OD-1.jpg: 北海道西部に分布する黒松内層模式地から得られた珪藻化石の産出リスト.珪藻化石帯の境界の定義と地質年代値は,Yanagisawa and Akiba (1998)および柳沢・渡辺(2011)を参照した.
N. ko-N. ka: N. koizumii-N. kamtschatica; N. ko: N. koizumii; G: good; M: moderate; P: poor.
Asterisk (*): present: dagger (†): not included in the total counts.
引用文献:
Yanagisawa, Y. and Akiba, F. (1998) Refined Neogene diatom biostratigraphy for the northwest Pacific around Japan, with an introduction of code numbers for selected diatom biohorizons. Jour Geol Soc Japan, 104: 395-414.
DOI https://doi.org/10.5575/geosoc.104.395
柳沢幸夫・渡辺真人(2011)5万分の1地質図幅「戸賀及び船川」地域(男鹿半島)の新第三紀及び第四紀の珪藻化石層序資料.地質調査総合センター研究資料集, 533: 1-17. 産業技術総合研究所地質調査総合センター.