Recent work indicates that a new biostratigraphic criterion and a new stratotype are required to define the Tournaisian-Visean (T-V) boundary. Investigation of the T-V transition in Guangxi (South China) has provided data which give a new insight on the problem. The foraminifer Eoparastaffella provides a goon new criterion for the establishment of the T-V boundary, based on its evolutionary stages. The sequence stratigraphy of this interval may also play a part in the recognition of the boundary. The idea of a type basin rather than a type section is put forward in preference to a single section as a better way of understanding the transition.
Hance, L., Brenckle, P., Coen, M., Hou, H., Liao, Z., Munchez, P., Paproth, E., Nicholas, T., Riley, N., Roberts, J., & Wu, X. (1997). The search for a new Tournaisian-Visean boundary stratotype. Episodes : journal of international geoscience, 20(3), 176-180. https://hdl.handle.net/2078.5/86489 (Original work published 1997)