Boletín de la Sociedad Geológica Mexicana

Volumen 75, núm. 3, A110923, 2023

http://dx.doi.org/10.18268/BSGM2023v75n3a091123

 

 

The Hettangian-Bajocian flora of the Shemshak Group, Kerman, Iran

 

La flora Hettangiano-Bajociano del Grupo Shemshak, Kerman, Iran

 

Hamed Ameri 1,*, Parisa Shaghayeghi 2

 

Department of Ecology, Institute of Science, High Technology and Environmental Science, Graduate University of Advanced Technology, Kerman, Islamic Republic of Iran.

Department of Geology, Kerman Institute of Higher Education, Kerman, Islamic Republic of Iran.

* Corresponding author: (H. Ameri) This email address is being protected from spambots. You need JavaScript enabled to view it.

 

How to cite this article:

Ameri, H., Shaghayeghi, P., 2023, The Hettangian- Bajocian flora of the Shemshak group, Kerman, Iran: Boletín de la Sociedad Geológica Mexicana, 75 (3), A110923. http://dx.doi.org/10.18268/BSGM2023v75n3a110923

 

Manuscript received: July 16, 2023; Corrected manuscript received: August 30, 2023.; Manuscript accepted: September 5, 2023.

 

 

ABSTRACT

Numerous examples of macro plant fossils can be found in the Kerman region’s Early and Middle Jurassic successions. The Ab-e-Haji, Badamu, and Hojedk formations were among these patterns. One of the suitable regions for paleobotanical study is the Chatroud section. In this region, the Lower-Middle Jurassic is approximately 210 meters thick. 18 species of macro plant fossils from 14 genera, including Nilssonia polymorphaPterophyllum nathorstiPodozamites distansElatocladus zamioidesElatides thomasiiNilssonia feriziensisNilssonia herriesi, and Beania sp., which are identified and described in this study, along with Pterophyllum schenkiAnomozamites marginatus, and Klukia exilis. In this region, there are two plant assemblage zones known as Anomozamites marginatus-Pterophyllum schenki Zone and Klukia exilis Zone. The Hettangian-Bajocian age is preserved at the Chatroud section.

Keywords: Jurassic, Hettangian-Bajocian, plants, Biozone, Kerman, Iran.