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Island Arc Award


ÂоÝÏÀʸ¡§Isozaki, Yukio, 2019, A visage of early Paleozoic Japan: Geotectonic and paleobiogeographical significance of Greater South China. Island Arc, 28: e12296.

Tectonic evolution of Great South China (GSC) during early Paleozoic is fundamental for considering the origin of the Japanese Islands, but has not yet been fully understood. Nevertheless, zircon U-Pb dates of Paleozoic granitoids and sandstones have provided critical information on the continental margin along which proto-Japan began to grow. Based on currently available dataset of the dating as well as paleogeographic data, Isozaki (2019) reconstructed the early Paleozoic evolution of Japan. He suggested that the tectonic setting changed from a passive continental margin (Stage I) to an active margin (Stage II) during Cambrian when the oldest arc granitoid, high-P/T blueschist, and clastic sediments were formed. The predominant occurrence of Neoproterozoic zircons in Paleozoic rocks indicates that the relevant continental block was a part of South China, probably forming a northeastern segment of GSC. He reconstructed that GSC was probably twice as large as the present conterminous South China. In addition, he summarized the faunal characteristics of the Permian marine fauna in Japan, which are in good accordance with the relative position of GSC with respect to the North China block during the late Paleozoic. This extensive summary and novel reconstruction provided clear pictures of the geological history of the Japanese Islands and prospective for future researches for the readers of Island Arc. Therefore, we decided that the paper by Isozaki is suitable for Island Arc Award in 2021.

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https://onlinelibrary.wiley.com/doi/full/10.1111/iar.12296

 

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ÂоÝÏÀʸ¡§Takashima, R., Hoshi, H., Wada, Y., Shinjoe, H., 2021. Identification of the source caldera for the Middle Miocene ash-flow tuffs in the Kii Peninsula based on apatite trace-element composition. Island Arc, 30, e13039. doi: 10.1111/iar.12404

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