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Miocene Floras of Taiwan: an Overview in Comparison with Those of Southwestern End of Japan

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Miocene Floras of Taiwan: an Overview in Comparison with Those of Southwestern End of Japan 国立科博専報，（44），2006年3月28日 Mem. Natn. Sci. Mus., Tokyo, (44), March 28, 2006 Miocene Floras of Taiwan: an Overview in Comparison with Those of Southwestern End of Japan Kazuhiko Uemura1 and Ching-Yao Li2 1 Department of Geology and Paleontology, National Science Museum, Tokyo, 3–23–1 Hyakunin-cho, Shinjuku-ku, Tokyo, 169–0073 Japan E-mail: [email protected] 2 Tung Fang Institute of Technology, Hu-Nei Shang, Kaohsiung Co., Taiwan Abstract. Miocene megafossil floras in Taiwan are reviewed, and floral characteristics for the Shihti flora (Early Miocene) in the northern part of Taiwan and Lilongshan flora (Late Miocene) in the southern part are briefly discussed. In particular, the comparison is made with the Early to Middle Miocene floras from the Yaeyama Group in Yonaguni-jima and Iriomote-jima, southwest- ern end of Japan. The Shihti and Lilongshan floras, together with the flora from Yonaguni-jima, show the feature of oak-laurel forest in the warm-temperate to subtropical regions. The flora from Iriomote-jima is characterized by wetland and more temperate elements. These floras in Taiwan and Yonaguni-jima and Iriomote-jima in Japan provide evidence of Miocene floras in the low- latitudes where little is known up to the present. Key words : Miocene, megafossil flora, Taiwan, Yonaguni-jima, Iriomote-jima. crofossils (Huang & Huang, 1984; and others). Introduction Furthermore, since Miocene floras of Taiwan In Taiwan, Tertiary sediments are widely dis- represent one of the low-latitude floras, these tributed throughout the island. Miocene sedi- provide evidence of the latitudinal gradient of the ments crop out in the western mountainous and Miocene floras in the eastern maritime areas of hilly lands along the Central Mountain Ranges the Eurasian Continent. In this paper, we briefly made up mainly of the Paleogene rocks. These show the outline of the Miocene floras in Taiwan Miocene sediments are conformably overlain by and compare these with the Miocene floras in the Pliocene sediments. More limited Miocene distri- southwestern end of Japan (Fig. 1). butions are also known in the southern and east- ern coastal areas. These Miocene sediments are Overview of the Miocene Floras in Taiwan mostly marine in origin. In the northern and east central parts, littoral and non-marine coal-bear- Miocene plant megafossils have been recorded ing sediments are intercalated at three horizons: since Deguchi (1912) listed plant megafossils in the Lower, Middle, and Upper coals (Chang, the explanatory text of the geological and miner- 1967; Ho, 1988). alogical map of Taiwan. Subsequently, many Although many palynological and geological Japanese geologists noted the occurrence of plant works for Miocene sediments have been made, megafossils from the Miocene rocks, mostly as- our knowledge on the Miocene floras is still in- sociated sediments with workable coal seams sufficient. Clearly, studies on the Miocene floras (see Hayasaka, 1939). Tan (1940) cited S. Endo’s in Taiwan are important, because the Miocene unpublished data and listed such plants as Ficus sequence is more complete than that of the Main- tiliaefolia Heer (ϭ“Alangium” aequalifolium land China and is well constraint biostratigraphi- (Goeppert) Kryshtofovich et Borsuk), Ficus ? cally by abundant marine invertebrates and mi- sp., Cinnamomum cf. vera Berry, and Podogoni- 186 Kazuhiko Uemura and Ching-Yao Li Fig. 1. Index map showing plant megafossil localities in Taiwan and Yaeyama-retto, Japan. um sp. from the “Lower Coal” in the northern ern Taiwan. part of Taiwan (see also Tan, 1971). However, Very recently, Li (2000) studied Miocene plant these plant megafossils have only listed without megafossils (Lilongshan flora) from the Lilong- any illustration or description of the plants. shan Formation (Late Miocene: Chen et al., After the World War II, Chaney and Chuang 1985; Sung, 1990) in the southern part of Tai- (1968) published the “Middle” Miocene flora wan, and described 32 leaf and seed species. He from the Shihti Formation in the northeastern also described petrified woods from the part of Taiwan. Subsequently, Canright (1972) Kungkuan Tuff in Taoyuan, northern part of Tai- reported the occurrence of Metasequoia from the wan: Taxodioxylon sequoianum Gothan, same formation. This Shihti flora has been the Bischofia javanoxyla Li et al., and Camellia only well-studied megafossil flora, though any il- kueishanensis Li et al. (Li, 2000; Li et al., 1999, lustration and description of the floral compo- 2003). The Kungkuan Tuff is of Early Miocene nents had not been given except for three new below the Shihti Formation or the Middle Coal. species. In recent bio- and chronostratigraphy, Additionally, Li (2000) restudied the cycadean the Shihti Formation is the late Early Miocene fossil forest reported by Cheng and Tang (1974) older than the age of the N8 zone in the plank- in Nanchuang. tonic foraminifer zonation. Apart from plant megafossils, palynological Plant megafossils from the Upper Coal hori- studies were made by Ling (1965), Canright zon have been unknown until Cheng and Tang (1974), Mei and Shaw (1983), and Huang and his (1974) reported in situ cycadean trunks from the co-authors (Huang, 1978–1992; Chaw & Huang, Nanchuang Formation in Nanchuang area, north- 1981; Hsieh & Huang, 1985; Shaw & Huang, Miocene Floras of Taiwan 187 1983; Hsieh et al., 1985). These studies will pro- floras in their floral composition. The Shihti flora vide a basis for the palynostratigraphic synthesis is of late Early Miocene, and the Lilongshan flora in the Miocene of Taiwan, together with the com- is of Late Miocene. parison with that of East China Sea (Hu & Chaney and Chuang (1968) listed 22 species, Sarjeant, 1992; Iwata & Oshima, 2001). in 19 genera and 13 families, of the Shihti flora. The flora is characterized by evergreen members of the Lauraceae, associated by evergreen faga- Shihti and Lilongshan Floras ceous members. Monocots of bambusoid and As noted above, the Shihti flora in the northern Palmae members are also charactersitic (Table part of Taiwan and the Lilongshan flora in the 1). As they pointed out, the Shihti flora shows the southern part are relatively well-studied fossil resemblance with evergreen sclerophyll broad- Table 1. List of leaf remains of the Miocene Shihti and Lirongshan floras. Genera and species Shihti1 Lilongshan2 Coniogramme devoli Chaney et Chuang ϫ – Pseudodrynaria sp. – ϫ Metaseuoia occidentalis (Newb.) Chaney ϫ – Actinodaphne nipponica Tanai ϫ – Cinnamomum sp. ϫϫ(2 species) Machilus sp. ϫϫ Neolitsea sp. ϫ – Neolitsea sp. cf. N. aciculata (Bl.) Koidzumi – ϫ Lindera sp. – ϫ (2 species) Phoebe mioformosana Tanai – ϫ Castanopsis miocuspidata Matsuo ϫ – Castanopsis sp. – ϫ (3 species) Cyclobalanopsis praegilva Kryshtofovich – ϫ Fagus protolongipetiolata Huzioka – ϫ Quercus sp. – ϫ (2 species) Pasania spp. ϫ (2 species) – Juglans sp. – ϫ Cleyera sp. ϫ – Diospyros sp. ϫ – Ardisia sp. ϫ – Mallotus sp. ϫ – Photinia sp. ϫ – Pongamia sp. – ϫ Leguminosae indet. ϫ – Sapindus sp. – ϫ Acer juani Chaney et Chuang ϫ – Alangium sp. ϫ – Aucuba sp. – ϫ Celastrus sp. ϫ – Gymnosporia sp. – ϫ Microtropis sp. cf. C. protojaponica Murai ϫ – Perrottetia miocenica Chaney et Chuang ϫ – Dicots indet. – ϫ (4 species) Smilax sp. cf. S. trinervis Morita – ϫ Smilax sp. – ϫ Bambusa sp. ϫ – Phyllostachys sp. ϫ – Rhapis sp. ϫ – 1 Shihti flora after Chaney & Chuang (1968) and Canright (1972). 2 Lilongshan flora after Li (2000); seed records of Cephalotaxus, Luffa, Nyssa, Diospyros, Ctrus, Ipomoea, and Sapindus are excluded in this table. 188 Kazuhiko Uemura and Ching-Yao Li Fig. 2. Selected plant megafossils from the Lilongshan Formation (Late Miocene). A, Cyclobalanopsis man- draliscae (Gaudin) Tanai, NSM-PP 11551; B, C. praegilva Kryshtofovich, NSM-PP 11552; C, C. sp. cf. C. nathorstii (Kryshtofovich) Huzioka, NSM-PP 11553; D, Cinnamomum sp., NSM-PP 11554; E, Dicot indet. cf. Apocynaceae, NSM-PP 11556; F, Lauraceae cf. Actinodaphne, NSM-PP 11555. Scales: 10 mm. leaved forests distributed at altitudes of 500 to Sterculiaceae or Tiliaceae (see Tanai, 1989). 2000 m of the present-day Taiwan. The presence Li (2000) recognized 26 leaf species of the Li- of the deciduous members of Acer and possibly longshang flora (Table 1). This flora is evidently Alangium are noteworthy. Although taxonomic allochthonous accumulated in a shallow marine status of Chaney and Chuangs’ Alangium is un- basin. Although taphonomic factors must take certain, it may represent an extinct genus of the into the consideration, an overall feature of the Miocene Floras of Taiwan 189 Fig. 3. Selected plant megafossils from the Yaeyama Formation (Early to Middle Miocene) from Iriomote-jima and Yonaguni-jima. A, Neolitsea sp., NSM-PP 15160a; B, Salix sp. 1, NSM-PP 11557; C, Cinnamomum lanceolatum (Unger) Heer, NSM-PP 15161; D, “Alangium” aequalifolium (Goeppert) Kryshtofovich et Bor- suk, NSM-PP 11558; E, Zelkova ungeri (Ettingshausen) Kovats, NSM-PP 1515191; F, Carpinus sp., NSM- PP 15180; G, Alnus sp. (infructescence), NSM-PP 11559; H, Liquidambar miosinica Hu et Chaney, NSM-PP 15164; I, Podogonium knorrii Heer, NSM-PP 15186; J, Alnus sp. cf. A. preneparensis Hu et Chaney, NSM- PP 11560. A, C, H, loc. Arakawa-bana, Yonaguni-jima; B, D, G, loc. west of Uebaru, Iriomote-jima, collected by T. Onoe; E, F, I, loc. west of Mt. Goza-dake, Iriomote-jima, collected by Y. Saito and others; J, loc. south of Sonai, Iriomote-jima. Scales: 10 mm, except for figs F and G (in mm). 190 Kazuhiko Uemura and Ching-Yao Li flora shows the resemblance with evergreen scle- dominance of Alnus pollen. Although the occur- lophyllous broad-leaved forests, as is the case of rence of plant megafossils from the Yaeyama the Shihti flora. Among all, evergreen members Group, including silicified woods, have been of the Fagaceae are abundant and diverse, togeth- known, no detailed study was published. The er with many evergreen members of the Lau- Yaeyama Group is assigned as the Early to Mid- raceae (Fig.
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