Department of Biological Sciences, Faculty of Science and Engineering, Chuo University, 1-13-27 Kasuga, Bunkyo-ku, Tokyo, 112-8551, Japan,
J Plant Res. 2014 Mar;127(2):221-32. doi: 10.1007/s10265-013-0619-6. Epub 2013 Dec 28.
Palynomorphs are reported for the first time from the Nishihiro Formation (Wakayama Prefecture, Outer Zone of southwest Japan). The Nishihiro Formation consists of brackish to shallow marine deposits, dated as late Barremian to Aptian from geological correlations. Spores prevail in the assemblage, representing Filicopsida (mainly Cyatheaceae and Anemiaceae), Marchantiopsida and Lycopsida. The pollen assemblage is dominated by Coniferales, whereas Gnetales and Bennettitales/Cycadales are only rarely observed. Moreover, we report angiosperm pollen grains of the genus Retimonocolpites for the first time in the Early Cretaceous sediments of Japan. Pollen grains of the Retimonocolpites Group are typical of early angiosperms and commonly found in assemblages from the early to mid-Cretaceous of all paleofloristic provinces. Until this paper, the oldest angiosperm fossils in Japan were represented by a single seed and a wood reported from the Albian of Hokkaido. The oldest reliable angiosperm pollen grains were reported in Hokkaido from the Cenomanian, and in Honshu from the Coniacian. Thus, Retimonocolpites pollen grains reported in the present study represent the oldest record of angiosperms in Japan. They indicate an appearance of the angiosperms in Japan older than thought until now, which is consistent with that proposed elsewhere in eastern Asia.
孢粉首次报道于日本西南部外区和歌山县的西広地域的西広组。西広组由半咸水至浅海沉积组成,通过地质对比,其年代被确定为晚巴雷姆期至阿普特早期。组合中以石松类(主要为石松科和紫萁科)、地钱类和木贼类为主。花粉组合以松柏类为主,而买麻藤类和苏铁类/苏铁类则很少见。此外,我们首次报道了日本早白垩世沉积物中的被子植物花粉属 Retimonocolpites。Retimonocolpites 组的花粉粒是早期被子植物的典型代表,常见于所有古植物区系早至中白垩世的组合中。在这篇论文之前,日本最古老的被子植物化石仅由北海道阿尔布期的一粒种子和一块木材代表。北海道最早可靠的被子植物花粉粒报告于白垩纪的塞诺曼期,本州的则报告于科尼亚克期。因此,本研究中报道的 Retimonocolpites 花粉粒代表了日本最古老的被子植物记录。它们表明,被子植物在日本的出现比之前认为的更早,这与东亚其他地区的观点一致。