6 0 0 0 日本の植物相と植生帯(第三回日本植物分類学会賞受賞記念論文)
- 著者
- 村田 源
- 出版者
- 日本植物分類学会
- 雑誌
- 分類 (ISSN:13466852)
- 巻号頁・発行日
- vol.5, no.1, pp.1-8, 2005
- 参考文献数
- 31
5 0 0 0 OA 原色日本植物図鑑草本編III(単子葉類)に発表した新名及び新見解
4 0 0 0 OA 新しい帰化植物
- 著者
- 村田 源
- 出版者
- 日本植物分類学会
- 雑誌
- 植物分類,地理 (ISSN:00016799)
- 巻号頁・発行日
- vol.31, no.4-6, pp.212-214, 1980-11-10 (Released:2017-09-25)
2 0 0 0 OA 新しい渡來植物
- 著者
- 村田 源
- 出版者
- 日本植物分類学会
- 雑誌
- 植物分類,地理 (ISSN:00016799)
- 巻号頁・発行日
- vol.16, no.3, pp.90, 1956-04-30 (Released:2017-09-25)
2 0 0 0 OA タンゴイワガサのtype localityと木梨延太郎について
- 著者
- 村田 源
- 出版者
- 日本植物分類学会
- 雑誌
- 植物分類・地理 (ISSN:00016799)
- 巻号頁・発行日
- vol.37, no.1, 1986-09-30
- 被引用文献数
- 1
1 0 0 0 OA 植物分類雑記13
- 著者
- 村田 源
- 出版者
- 日本植物分類学会
- 雑誌
- 植物分類,地理 (ISSN:00016799)
- 巻号頁・発行日
- vol.30, no.4-6, pp.134-147, 1979-12-20 (Released:2017-09-25)
1 0 0 0 OA コミカンソウ属の新帰化植物ブラジルコミカンソウ(新称)
1 0 0 0 OA 日本産アオウキクサ類の再検討
1 0 0 0 OA 日本の植物相と植生帯(第三回日本植物分類学会賞受賞記念論文)
- 著者
- 村田 源
- 出版者
- 日本植物分類学会
- 雑誌
- 分類 (ISSN:13466852)
- 巻号頁・発行日
- vol.5, no.1, pp.1-8, 2005-02-28 (Released:2017-03-25)
- 参考文献数
- 31
1 0 0 0 コミカンソウ属の新帰化植物ブラジルコミカンソウ(新称)
1 0 0 0 OA 植物分類雑記21
- 著者
- 村田 源
- 出版者
- 日本植物分類学会
- 雑誌
- 植物分類,地理 (ISSN:00016799)
- 巻号頁・発行日
- vol.43, no.2, pp.147-153, 1992-12-30 (Released:2017-09-25)
Four species of eastern Asian plants are studied. Three new taxa are described; Melampyrum macrantha as new species, Galium pseudoasprellum var. bingoense as new variety and Benthamidia capitata f.grandis as new form. Chloris truncata is newly found in Japan as naturalized plant.
1 0 0 0 OA 変異の問題 (学名の使用と標本の保存)-分類学の立場から-
- 著者
- 村田 源
- 出版者
- 日本雑草学会
- 雑誌
- 雑草研究 (ISSN:0372798X)
- 巻号頁・発行日
- vol.36, no.4, pp.307-310, 1991-12-26 (Released:2009-12-17)
- 参考文献数
- 7
1 0 0 0 OA 日本産シャクナゲ類の葉の表皮系に見られる特徴
- 著者
- 釘貫 ふじ 村田 源
- 出版者
- 日本植物分類学会
- 雑誌
- 植物分類,地理 (ISSN:00016799)
- 巻号頁・発行日
- vol.38, pp.349-358, 1987-09-25 (Released:2017-09-25)
An attempt was made as to the epidermal system of both adaxial and abaxial surfaces of foliage in some species of Rhodoendron which has been scarcely investigated. Using our original method, an observation of wide scope can be made concerning the epidermal layers of leaves by the light microscope from the polar view. The epidermal cells of the adaxial surface are found to be amoeboid in shape in R. aureum, R. brachycarpum and R. makinoi, while those to be not amoeboid but polygon in shape in R. metternichii var. metternichii, R. metternichii var. hondoense, R. yakushimanum and R. degronianum. In R. brachycarpum, the epidermal system of the adaxial surface is observed to be 2-layers near midrib, but to become one layer at the margin of leaves. there is sporadically an aggregate of cells which are well stained by fuchsin. In R. aureum, the hair stalks which are multicellar are observed in the abaxial surface of leaves. In R. brachycarpum, the base of hairs is found to be 2 cells, while that in the other species examined to be 2-4 cells. Considering the unique mode of the distribution and the density in stomata and hairs, and the epidermal cells being elliptic polygon, R. yakushimanum is thought to be clearly distinguished from R. metternichii and R. degronianum.
1 0 0 0 襲速紀要素について (西南日本外帯の自然史科学的総合研究-2-)
The "Sohayaki element" was defined by the late Dr. Gen-ichi KOIDZUMI in 1931 as one of the important floristic elements of Southwest Japan, and 101 species of vascular plants were enumerated by him as the components of the element (in MAYEBARA, 1931). Since then, several investigations have been attempted to clarify the entity of the present element. It is now regarded as one of the most ancient flora of Japan. No one, however, has reevaluated the species enumerated by KOIDZUMI. Having the specimens deposited in the herbaria of Kyoto University (KYO), University of Tokyo (TI), Tokyo Metropolitan University (Makino Herbarium-MAK) and National Science Museum, Tokyo (TNS), the flowering plants cited by KOIDZUMI as the components of the "Sohayaki element" are studied in this paper from taxonomic and phytogeographic point of view. The phytogeographic significance of the present element is also discussed. As shown in Table 1,the following five groups are recognized in the "Sohayaki element" by the distribution pattern of each species. The distribution maps, based on the specimens kept in the herbaria cited above, are drawn by the KLIPS-C computer system designed by Dr. H. KANAI, National Science Museum, Tokyo. I : The plants are distributed in the Sohayaki region which includes Kii Peninsula, Shikoku and Kyushu (as shown in Fig. 1), though they are divided into 5 subgroups(A-E). The plants belonging to the subgroups of B, C, D, and E are distributed in rather narrow area than those of A. II : The plants are distributed only in the West Japan as shown in Fig. 2. III : The plants are distributed in both West and East Japan, though they are divided into 5 subgroups (A-E). Distribution areas of B and C are shown in Fig. 3 and 4,respectively. IV : The plants are distributed from the Sohayaki region in West Japan to rather north area in central Honshu as shown in Fig. 5. V : The plants are distributed from Japan to Northeast China throughout Korean Peninsula. VI : The plants are widely distributed in both Japan and the Chinese Continent. KOIDZUMI also described the following elements with the enumeration of the species, i.e. , "Central Chinese element : 51 spp.", "Kuma-Kanto element : 22 spp.", "Manchuria-Korean element : 38 spp." and "Chugoku element : 27 spp.". The "Kuma-Kanto element" was considered as the plants endemic to the areas from Kyushu to Kanto district of Honshu, and the "Chugoku element" as those endemic to the Chugoku district of Honshu. Judging from his definition of each element and the distribution patterns summarized in Table 1,B and C of III are considered as the "Kuma-Kanto element", V is recognized as the "Manchuria-Korean element" and VI as the "Central Chinese element". I and II in Table 1 are the Sohayaki elements which are now generally recognized. The Sohayaki elements occur in the area of warm temperate zone from about 200m to 800m in altitude and are minor constituents in the present vegetation. The habitat of the elements is usually restricted within the limestone or serpentine areas, in rocky places near the river which often overflows and in the ill-nourished or dried places of mountain ridges. These facts suggest that the present elements, protected from extinction by the habitat mentioned above, have survived for long time in competition with the invaders of both glacial and interglacial period.