Siphonodella banraiensis is from the Late Devonian of Thailand.[4]Siphonodella nandongensis is from the Early Carboniferous of the Baping Formation in China.[5]
^Conodonts. EB Branson and MG Mehl, in HW Shimer and RR Shrock, Index Fossils of North America. 1944
^Andrey V. Zhuravlev (2017). "A new species of the conodont genus Siphonodella Branson & Mehl (late Tournaisian)". Estonian Journal of Earth Sciences. 66 (4): 188–192. doi:10.3176/earth.2017.15.
^Sandra I. Kaiser; Tomáš Kumpan; Vojtěch Cígler (2017). "New unornamented siphonodellids (Conodonta) of the lower Tournaisian from the Rhenish Massif and Moravian Karst (Germany and Czech Republic)". Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen. 286 (1): 1–33. doi:10.1127/njgpa/2017/0684.
^Late Devonian conodonts from northwestern Thailand. Norman M. Savage (2013). Bourland Printing / Trinity Press. pages 1–48, ISBN 978-0-578-11919-9
^New material of the Early Carboniferous conodonts from the lower member of the Baping Formation in Nandong, Guangxi, China. Zhihong Li, Zhongqin Peng, Long Cheng, Chuanshang Wang and Baozhong Wang, Acta Micropalaeontologica Sinica, 2014, volume 31, issue 3, pages 271–284
Siphonodella is an extinct genus of conodonts. Siphonodella banraiensis is from the Late Devonian of Thailand. Siphonodella nandongensis is from the Early...
appearance of the conodont Siphonodella sulcata within the evolutionary lineage from Siphonodella praesulcata to Siphonodella sulcata. This was ratified...
appearance of the conodont Siphonodella sulcata within the evolutionary lineage from Siphonodella praesulcata to Siphonodella sulcata. The first appearance...
Tournaisian is in La Serre, with the first appearance of the conodont Siphonodella sulcata. In 2006 it was discovered that this GSSP has biostratigraphic...
Lower GSSP ratified 1972 Upper boundary definition FAD of the Conodont Siphonodella sulcata (discovered to have biostratigraphic issues as of 2006). Upper...
Dollymae bouckaerti the zone of Gnathodus typicus and Siphonodella isosticha the zone of Siphonodella quadruplicata and Patrognathus andersoni (upper zone...
zone. They also belong to the praesulcata conodont zone (named after Siphonodella/Eosiphonodella praesulcata) and the DFZ7 foraminifera zone (characterized...
Lower GSSP ratified 1993 Upper boundary definition FAD of the conodont Siphonodella sulcata (discovered to have biostratigraphic issues as of 2006). Upper...
conodont biozones, four of which contain Patrognathus species: the zone of Siphonodella quadruplicata and Patrognathus andersoni (upper zone of Patrognathus...
Dollymae bouckaerti the zone of Gnathodus typicus and Siphonodella isosticha the zone of Siphonodella quadruplicata and Patrognathus andersoni (upper zone...
semiglaber and Polygnathus communis the zone of Gnathodus typicus and Siphonodella isosticha The Visean, the second age of the Mississippian, contains four...
Mountains in Wyoming. In 1944, he described with Mehl the conodont genus Siphonodella. In 1947, with his son Carl Colton Branson, he reviewed the Lower Silurian...
Crisis equivalent deposits and associated conodont faunas including Siphonodella progenitors from late Devonian island arc settings (Indert Formation...
S2CID 251162865. Plotitsyn, A. N. (2022). "New group of Tournaisian advanced Siphonodella (Conodonts, Lower Carboniferous)". Rivista Italiana di Paleontologia...
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