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土尔干槽珊瑚属Tyrganolites是Б.Б.切尔尼舍夫(Чернышев)1951年建立的,当时只有一个种,采自苏联库兹涅茨盆地和巴尔哈什湖附近中泥盆统。此后相继在苏联哈萨克斯坦、阿尔泰以及我国北部地区多次被发现。目前已有18个种,它们广泛分布于中泥盆统,由于分布集中,地史历程很短,属的构造特征十分明显。因此,不管在系统分类,还是地层划分对比方面,都具有非常重要的生物学和地层学意义。本文根据该属的构造特征,空间分布规律以及共生化石组合面貌,重点讨论该属的分类
The Tyrganolites are Б.Б. Чернышев established in 1951, with only one species at the time, from the Middle Devonian near the Kuznets Basin in the Soviet Union and Lake Balkhash. Since then, one after another in the Soviet Union, Kazakhstan, Altai and northern China were found. At present, there are 18 species, which are widely distributed in the Middle Devonian. Due to the concentrated distribution and short history of geo-history, the tectonic features of the genera are very obvious. Therefore, it has very important biological and stratigraphic significance both in terms of systematic classification and stratigraphic division. According to the tectonic features, spatial distribution and the assemblage of symbiotic fossils, this article focuses on the classification of the genus