浙江古田山自然保护区苔藓植物区系特点及其与邻近山体的比较

浙江开化县古田山自然保护区共有苔藓植物３２５种（包括种下等级）其中苔类植物８９种,隶属于２２科和３９属,藓类植物２３６种,隶属于３３种和１０３属,古田山苔藓植物区系地理成分复杂,以东亚成分为主,欧亚－北美成分和世界热带成分也占有较大的比例;地理联系广泛,与日本苔藓植物区的联系较为密切,古田山苔藓植物区系及邻近几个山体苔藓植物区系的比较结果表明,古田山苔藓植物区系介于安徽黄山和江西三清山之间,并与三     

陕西天华山自然保护区苔藓植物区系研究

根据调查和参考有关文献,对陕西天华山自然保护区苔藓植物区系进行了初步分析,结果表明：种类丰富,本区共有苔藓植物46科95属180种（包括种下类群）。其中苔类植物14科18属37种。藓类植物32科77属143种;优势科为青藓科、提灯藓科、丛藓科、羽藓科、真藓科、绢藓科和灰藓科,优势属为提灯藓属、真藓属、青藓属、光萼苔属、绢藓属、灰藓属、凤尾藓属、丛本藓属、缩叶藓属、羽藓属和仙鹤藓属;地理成分复杂、多样。区系联系广泛;种的地理成分统计分析表明。温带成分占绝对优势。热带成分也占有一定比例,反映了本区苔藓植物区系的热带亲缘性;东亚成分也占有重要地位,有42种,其中中国-日本分布有15种;中国特有种有16种,中国特有分布中以西南区系成分为主。本区苔藓植物区系隶属于华中地区,但兼有多种成分。体现本区苔藓植物区系的南北过渡特征。     

贵州施秉喀斯特世界自然遗产提名地苔藓植物区系特征

由于地理环境优越、海拔跨度大、生境异质性高、人为影响小等原因,贵州施秉喀斯特世界自然遗产提名地的苔藓植物丰富,共有50科128属286种（含变种和亚种）,其中苔类17科23属43种,藓类33科105属243种。其优势科、属均反映了该区系的温带向热带过渡的性质。区系地理成分分析结果显示,该区苔藓植物北方温带成分、热带成分和东亚成分分别占37．12％、31．82％和30．30％,其中中国特有分布型占12．12％,反映了施秉喀斯特苔藓植物区系具有温热并重、东亚色彩浓厚、特有性较高的特征。通过对施秉喀斯特与其它五个区域的苔藓区系进行对比发现．施秉苔藓区系丰富度高,与同为云贵区的香纸沟、马岭河、罗平喀斯特地区亲缘关系最近。     

广东内伶仃岛自然保护区的苔藓植物

报道广东内伶仃岛自然保护区的苔藓植物共１９ 科、３４ 属、６１ 种, 其中藓类１３ 科、２６属、５０ 种, 苔类６ 科、８ 属、１１ 种。全缘疣鳞苔（ Ｃｏｌｏｌｅｊｅｕｎｅａ ｓｃｈｗａｂｅｉ） 等３ 种苔类和拟阔叶小石藓（ Ｗｅｉｓｉａ ｐｌａｔｙｐｈｙｌｌｏｉｄｅｓ） 等１０ 种藓类为广东省新记录。分析了保护区内的苔藓植物区系特点, 并与车八岭、黑石顶、鼎湖山及南岭自然保护区的苔藓植物区系进行了比较。研究表明, 内伶仃岛的苔藓植物区系由于受地理位置及地形特征的影响而具有一定的特殊性。     

贵州红水河谷地区苔藓植物区系研究

对贵州红水河谷地区的500余号苔藓植物标本进行了调查、采集和分类鉴定,得到苔藓植物36科,78属,204种(包括8亚种4变种和1变型)。其中藓类植物23科60属163种,苔类植物13科18属41种。为贵州增加新记录5种。划为13种类型。其中具热带性质的区系成分最丰富,占总数的38.02%,构成该区苔藓植物区系成分的主体;具温带性质的成分占总数的33.85%;东亚成分、特有成分、东亚-北美成分占该区的1.56%。选择9个地区,通过属和种的相似性系数全面比较,表明该地区与同纬度茂兰自然保护苔藓植物的相似性最高,关系最密切;与低纬度鼎湖山的相似性较高,关系较近;与高纬度小五台山和长白山相似性最低,关系最远。还统计了各地区的植物区系谱,分析该地区与其它地区的藓类植物区系关系。并着重就该区的热带边缘性的特点进行了讨论。     

小秦岭自然保护区苔藓植物区系分析

小秦岭自然保护区共计有苔藓植物53科128属281种10变种2变型。其中苔类植物19科22属37种2变种l变型;藓类植物34科106属244种8变种l变型．其区系的基本特征是：地理成分多样,区系联系广泛;以温带性质为主,但有较明显的热带残遗性和亲缘性;隶属于华北植物区系,但兼有多种区系成分,体现了本区苔藓植物区系南北过渡,东西交汇的特征。     

山东昆嵛山苔藓植物多样性及区系特征

通过对采自山东昆嵛山的4000余号苔藓植物标本进行鉴定,发现昆嵛山分布有苔藓植物56科131属318种,包括山东新记录种69种。在昆嵛山的苔藓植物中,苔类植物有22科28属41种,藓类植物有34科103属277种。昆嵛山苔藓植物区系主要由青藓科（45种）、真藓科（33种）、丛藓科（31种）、灰藓科（24种）、绢藓科（18种）、曲尾藓科（15种）等一些大科组成。单种属和寡种属数量较多,但特有现象不明显。土生和石生群落优势明显,水生和树生群落缺乏。区系地理成分复杂,分布类型多样,温带成分优势明显,但也具有一定的热带成分。本研究旨在进一步促进山东苔藓植物研究,并与现代苔藓植物学的发展接轨,也为中国苔藓植物的研究提供新的资料。     

湖南小溪自然保护区树附生苔藓植物研究

采用水平拉线法调查了小溪国家级自然保护区中树附生苔藓植物的种类,并对其进行了地理成分的分析.研究结果表明:该地区附生苔藓植物共18科26属共43种,其中苔类植物6科6属6种,藓类植物12科20属37种;树附生苔藓植物区系成分以东亚成分为主,其次为热带亚洲成分,再次为旧世界温带成分及温带亚洲成分.     

浙江省清凉峰自然保护区苔藓植物区系成分研究

通过对2013~2014年于清凉峰自然保护区采集的1 500余份苔藓植物标本进行鉴定和文献研究,统计分析了清凉峰自然保护区苔藓植物种类组成,区系地理成分及特点,并对该地区与相邻8个地区藓类植物的丰富度系数比较和相似性系数比较,以明确该地区苔藓植物不同的生态分布类型,揭示浙江清凉峰保护区苔藓植物多样性的变化规律。结果表明:(1)浙江省清凉峰国家自然保护区苔藓植物共有62科143属337种(包括3个变种),其中苔类植物20科29属49种,藓类植物42科114属288种。(2)藓类植物的优势科9个、优势属16个。(3)该地区苔藓植物区系成分主要以东亚成分为主(占总种数41.84%),温带成分次之(占总种数28.57%),热带成分再次之(占总种数20.74%)。(4)浙江清凉峰自然保护区苔藓植物区系与浙江省境内的金华山、大盘山、天目山和凤阳山的亲缘关系较为密切。(5)浙江清凉峰自然保护区苔藓植物生态分布类型复杂多样,以石生类型(占总标本数的47.09%)最多,其次为岩面土生(占总标本数的27.68%)和土生(占总标本数的12.85%)类型。     

镜泊湖世界地质公园火山口地下森林苔藓植物区系

镜泊湖世界地质公园火山口孕育了罕见的原始地下森林，本研究为完善中国火山生态系统苔藓植物区系地理起源提供重要资料。基于前期野外调查、标本采集和物种鉴定数据，已知苔藓植物53科126属292种，采用分层聚类分析和主成分分析方法探讨区系地理特点。结果表明：(1)镜泊湖火山口地下森林苔藓植物单种属和寡种属占绝对优势，共106属(占总属数84.13%)152种(占总种数52.05%)。(2)区系地理成分共11种，北温带分布占主体(49.12%)，东亚分布次之(21.55%)，中国特有分布第三(8.48%)。(3)地下森林中国特有苔藓植物可能沿“北线”以山脉为通道进行传播。(4)镜泊湖火山口地下森林与镜泊湖火山熔岩台地苔藓植物区系相似性最高。此外，发现受威胁苔藓植物7种。总之，镜泊湖火山口地下森林苔藓植物区系的主要特点为起源古老，组成复杂，北温带性质明显，与东亚苔藓植物区系具有深厚的历史渊源，凭火山锥内部优越的微生境成为中国特有和珍稀濒危苔藓植物的避难所。     

Recent Advances in Bryological Research

In the last two decades, all the branch fields of bryology, with classical taxonomy gradually developing into multidisciplinecourses, have witnessed a great progress. The author is attempting to give a brief view of bryology in the following five paragraphs. The first part introduces the fundamental characteristics of bryology in the recent decades. Publication of “New Manual of Bryology” Vol. I and II, edited by Schuster(1983-1984) , marked a new epoch of bryology. A series of books, “The Biology of Mosses” (Richardson, 1981), the “New Advances in Bryology “and the other bryological publications showed that bryologists were working not only on bryofloras in different regions of the world, but also deeply engaged in the micro-view fields of bryology. Evidently, the world bryological researches have entered a prosperous period. The second part gives some recent examples of investigations on taxonomy, morphology, cytology, paleobotany, ecology, reproductive biology and ecological physiology of bryophytes. In discussing the tendency of the future research, the author emphasizes that systematic and evolutionary botany of bryophytes is one of the main subjects .Following the increase of taxa, the development of chemotaxonomy, cytology, numerical taxonomy etc.will reveal the relationships between orders, families or infrafamiliar groups. However, the main problem in this respect is lacking of key fossil records of bryophytes. On the other hand, the monographs increase steadily, and they are helpful in correcting some previously reported disjunct distribution of species and distribution of regional new species. Plant geography of bryophytes can also be used for explaining the continental drift (Schuster 1969, 1972).Moss indicators, which are more sensitive than vascular plants, have been noticed. The traditional utilization of mosses will be continuous. Chinese bryology has been greatly improved in the past half a century, and about a hundred papers involving taxonomy, phytogeography, phytocoenology, morphology, cytology, numerical taxonomy and applied bryology, were published in last two decades. In China, the foundation of taxonomy of bryophytes is developing, although we already have several bryological research centers. It seems to me that too many new taxa have been described, while no sufficient attention has been paid on studies on relationships and evolution of bryophytes. Due to identification of bryophytes, hryofloras between some neighbouring regions are not comparable. Fossils of bryophytes are usually treated as the “unknown kind of plants”, so we lack the geological evidence of bryophytes. We are facing the problem in training a new generation of bryologists due to the limited funds. Finally, some suggestions are made for Chinese bryology. The ways for seeking the origin of bryophytes will be: l.Searching for primitive groups of bryophytes.2.Comprehensive studies on key genera and species.3.Expeditions to the unknown native localities of special groups of bryophytes. Further studies on the bryoflora and phytogeography are necessary in China. Studies on the distribution centers of genera endemic to China and East Asiatic endemic genera in China will provide some pieces of evidence on the origin oe the Chinese bryoflora. New records of macrofossils and microfossils of bryophytes will help to break the “neck of bottle “ of the above-mentioned problems. Experimental projects are almost unknown in China. lt is very important, therefore, to encourage people to work on them for original data on phylogeny and origin of bryophytes, although it will be a long-term task inChina.     

庞泉沟国家级自然保护区苔藓植物区系分析

庞泉沟自然保护区共计有苔藓植物29科63属192种（包括12变种1亚种）。其中苔类植物8科9属14种;藓类植物21科54属178种。其区系的基本特征是：地理成分多样,区系联系广;区系成分以北温带成分为主,兼有较明显的东亚色彩;隶属于华北植物区系。     

海南岛苔藓植物研究历史、现状与展望

综述了海南岛苔藓植物的研究历史和现状。目前海南岛已记录的苔藓植物共有87科227属806种,其中苔类33科71属366种,藓类51科152属436种,角苔类3科4属4种;苔藓植物的区系组成以热带亚洲成分为主,与香港、台湾地区的种属相似性高;对海南岛苔藓植物的研究集中在尖峰岭、霸王岭、吊罗山3个国家级自然保护区;叶附生苔是海南热带雨林主要的苔藓生态分布类型之一,共有7科23属123种;初步统计濒危苔藓植物有15种。今后应继续开展广泛和持续的物种多样性调查,从生态学、植物化学、分子生物学等领域进行研究,促进合理的开发利用和推动保护工作。     

河北省侧蒴藓类植物的地理成分及其与邻近地区的比较

通过对河北省侧蒴藓类植物较详尽的野外考察、标本采集、鉴定和系统研究,已知河北省侧蒴藓类植物17科,66属,196种(包括种下单位),其地理成分可划分为9种类型,北温带分布型占主导地位,东亚分布型次之,热带分布型不起主要作用。运用物种丰富度、优势科比较、属相似性系数等统计方法,对河北与邻近地区的区系地理成分进行了比较、分析和讨论。从河北省与我国东北、内蒙古、山东、秦岭、西藏和横断山等6个地区侧蒴藓类区系组成的比较分析得出,本省该类群物种丰富度位居第4,横断山居于第1位,河北与其它6个地区的共有优势科前3位为青藓科、柳叶藓科、灰藓科;河北与内蒙古、山东相似程度最高,与东北和秦岭相似程度次之,与西藏、横断山相差最大。同时对这7个地区的具体地理成分也作了比较。这些结果有力地说明了河北省侧蒴藓类植物区系具有明显的温带性质,同时兼有浓厚的东亚区系色彩,也表明了中国华北与日本、欧洲和北美东北部在苔藓植物区系物种起源上有深厚的历史渊源。     

Relationships Between the Bryoflora of Mt. Wuyi,SE China,and Those of Neighbouring Mountain Regions

Mt. Wuyi, located at 27°37‛-27°54‛ N, 117°27‛-117°51‛ E, is the highest mountain in South-East China. Its main peak, Huanggangshan, is 2158 m above the sea level. In 1955, P. C. Chen organized the first expedition to Mt. Wuyi, and the authors investigated the different ravines and the forests of that area in 1976 and from 1979 to 1984 respectively. Up to now 355 species of the bryophytes have been found in Mt. Wuyi. I. The influence of the factors of geological history on the bryoflora of Mt. Wuyi Fujian Province, belonging to Cathaysian, one of three Chinese ancient lands, was a part of ocean until the end of the lower Tertiary. In the early Devonian, Fujian uplifted above the sea level, but it submerged in the sea later, and then uplifted above the sea level again in the upper Triassic. By the end of the lower Triassic the Himalayan movement influenced the paleogeography of China deeply, and the eastern and central mountains of Fujian uplifted again. In the Tertiary, Fujian was influenced by the hot maritime weather, so the tropical evergreen forests existed in southern Fujian at that time. The conclusion was made by Z. B. Zhao in 1983 after his long period of study on geological history of Fujian Province since the Yanshan movement. According to the morden geographical distribution of Chinese bryophytes, it seems that the above influence might be related to the bryophytes of Mt. Wuyi and also the southern part of Zhejian Province. By the end of the Tertiary the weather became cold in most parts of China. Since then the cold weather and hot weather alternated several times. One kind of the endemic elements of the bryoflora formed in the area from the south-eastern coast of China to the southeastern Xizang (Tibet), including Japan. They are not specialized at the family level or closely related to each other, but they have similar distribution and belong to different families. In the Quaternary, Mt. Wuyi gradually uplifted following the Himalayan movement. As the weather cooled down in the upper part of the mountain, deciduous broad-leaved and needleleaved trees increased there. Meanwhile, temperate genera and species of the bryophytes spread and invaded South China and entered Mr. Wuyi. Rhytidiadelphus and Hvlocomium probably began to grow in Mt. Wuyi at that time, and their distribution is quite different from their primary one. On the other hand, a part of tropical and subtropical bryophytes might enjoy the changed weather and environment in the Quaternary and existed in a few small localities of Mt. Wuyi, and the genera Haplomitrium, Endotrichella and Floribundaria are probably their representatives. From the point of view of geological history we are now living in the interglacial period and the present natural conditions will last continuously, so they will steadily influence the bryoflora of Mt. Wuyi in a long period of time. 2. Essential characteristics of the bryoflora in Mt. Wuyi Due to the geographical position and the other factors of Mt. Wuyi the bryoflora is represented by numerous tropical and subtropical elements (34.1%), but the East-Asiatic endemic ones (79.2%) are characteristic of the bryoflora in Mt. Wuyi (Tab. 1). The tropical and subtropical families of the bryophytes, found south of Changjiang (Yangtzi) River, are Haplomitriaceae (1 genus, 3 species), Porellaceae (2 genera, 8 species), Frullaniaceae (2 genera, 10 species), Lejeun eaceae (21 genera, 35 species), Trachypodaceae (3 genera, 4 species), Meteoriaceae (10 genera, 17 species), Neckeraceae (5 genera, 8 species) and Hookeriaceae (3 genera, 3 species). The above 8 families, including 46 genera and 85 species, represent about 1/4 genera (24.3%) and less than 1/4 species (23.9%) of the bryoflora of Mt. Wuyi. Most species of East-Asiatic elements show very close relationships with Japan, and are widely distributed from the low altitude of Mt. Wuyi to the summit of Mt. Huanggangshan. However, the Holarctic species (26.8%) are also important elements of the bryoflora in Mt. Wuyi, showing its transition nature, although it is located in the subtropics. Moreover, the in fluence of the Himalayas also exists in Mt. Wuyi, and the Himalayan elements cover 14.4% in the bryoflora of Mt. Wuyi. The similarity coefficients between the bryofloras of Central and South America, Africa and Oceania and that of Mt. Wuyi are from 5.0-9.2% respectively. The endemic species are not very many and cosmopolitan species are only 7 there. In 1958, P. C. Chen designated Mt. Wuyi as “the transition region of South and North China rich in East-Asiatic genera and species”. His very important conclusion is essentially in accordance with the fact of the bryoflora on Mt. Wuyi. Recently, some of the new records fur ther show the characteristics of the bryoflora in Wuyi. Two facts are worth being mentioned. One is that East-Asiatic genera are only five in Mt. Wuyi. However, there are 9 East-Asiatic genera in Mt. Huangshan more than in Mt. Wuyi; 4 East-Asiatic genera are recorded in Mt. Shennongjia. The other is that epiphyllous liverworts in Mt. Wuyi, consisting of 7 families, 21 genera and 36 species, are less than on Hainan Island and Xishuangbannan, located in the tro pics in China. 3. Comparison between the bryoflora of Mt. Wuyi and those of the neighbouring regions As China covers a very large area, bryofloristic elements are quite different in the diffe rent regions. In this section, we are concentrated on making a comparison between the bryof loras of Mt. Wuyi and the regions belonging to the Central China of the bryoflora named by P. C. Chen. Huaping Forest Region, Guangxi Zhuang Autonomous Region in South China, with both latitute and altitude very similar to Mt. Wuyi, is included in this comparison (Fig. 1). According to the rough estimation, the similarity coefficient of moss genera between Mt. Wuyi and Huaping is 56.3%, and those between the mountain and southern Zhejian and Mt. Huangshan, Anhui, are 62.7% and 51.6% respectively, while the similarity coefficient of the genera of the mossfloras between Mt. Shennongjia and Mt. Wuyi is 46.8%. Table 2 shows the statistics of mosses in Mt. Wuyi and the others, but the bryoflora of Huaping needs further study However, it is very interesting to note that Haplomitrium and Pleurozia of liverworts are both found in Mt. Wuyi and Huaping Forest Region, and the similarity coefficient between the mossfloras of Mt. Wuyi and Zhejian Province is also higher than those mentioned above. Tropical and subtropical elements reduce towards the north in China, and temperate ones increase. Huaping is located in the south, and, as expected, some tropical and subtropical genera such as Hookeriopsis and Symphyodon have been found there, but not in Mt. Wuyi; several temperate genera, such as Schwetschkeopsis and Fauriella, have been recorded in Mt. Huangshan, but not in Mt. Wuyi. For some unknown reasons, Octoblepharum and Neckeropsis are only found in southern Zhejiang, but not in Mt. Wuyi. Mt. Shennongjia, with its main peak over 1000 m higher than that of Mt. Wuyi, is located in its northwest, and more than ten temperate genera, such as, Ceratodon, Aulacomnium Myurella, Bryonoguchia and Abietinella have been found there. Generally, Mt. Wuyi belongs to the central subtropical region of China, and East-Asiatic endemic genera are the main elements of its bryoflora, but the bryoflora also consists of tropical and subtropical elements with some temperate ones. 4. East-Asiatic endemic genera in the bryoflora of Mt. Wuyi In the bryoflora of Mt. Wuyi, one of the main elements, East-Asiatic endemic genera, should not be neglected (Tab. 4). East-Asiatic endemic genera in Mt. Wuyi (five) are less than in Mt. Huangshan and Mt. West Tianmu, although the positions of the latter two are very close to Mt. Wuyi. East-Asiatic endemic genera of liverworts are Trichocolea and Macvicaria so far found in Mt. Wuyi, and the mosses are Myuriopsis, Meteoriella, Pseudospiridentopsis (Fig. 1). Myuriopsis is only distributed in Taiwan Province and Mt. Wuyi, and the other four are distributed in Mt. Huangshan or Mt. West Tianmu, and also in Taiwan, besides in Mt. Wuyi. About thirty EastAsiatic endemic genera have so far been known in China, which means that about one sixth of East- Asiatic endemic genera of the bryophytes occur in Mt. Wuyi. We may notice that nine and seven East-Asiatic endemic genera of the bryophytes have been recorded in Mt. Huangshan and Mt. West Tianmu respectively. In Mt. Shennongjia, Central China, there are four East Asiatic endemic genera, but only two have been found in the Huaping Forest Region, South China. In Mt. Dinghua, located south of Mt. Wuyi, on East-Asiatic endemic genus of the bryophytes has so far been found. East-Asiatic endemic genera of the bryophytes are mainly limited to China, Korea and Japan, including the East Himalayas, rarely occur in South Asia, Siberia of the Soviet Union. Therefore, these genera enjoy a warm and moist environment. In Mt. Wuyi, all the East-Asiatic endemic genera are monotypic ones with a disjunct distribution. Now in Taiwan Province five of six recorded East-Asiatic endemic genera are common to Mt. Wuyi. In Japan, about eleven, i.e. one third of, East Asiatic endemic genera so far found are common to China, which shows a long history of the phytogeographical relationships between Japan and China. East Asiatic endemic genera of the bryophytes might therefore exist on islands of Taiwan Province and Japan before they were separated from the mainland of Asia. However the fossil evidence is still lacking in the bryophytes, so we are not able to discuss about the distribution area and the distribution center of the East-Asiatic bryoflora in detail. The above estimation is more or less related to geological history, and we assume that the East-Asiatic endemic genera have existed at least since the end of the Tertiary. Starting from the Quaternary, the climatic change during glacial epoch has been possibly the most important factor affecting the bryoflora in Asia, and the upheaval of the Himalayas has stimulated the diversity and the specialization of the bryophy tes. Considering these factors, East-Asiatic endemic genera might be the “Tertiary fossil plants”. Another problem is difficult to explain, because Mts. Huangshan, West Tianmu and Shen nongjia were once influenced by glaciation directly, although Chinese geologists hold different views. However, no evidence of glaciation has been found in Mt. Wuyi. It is worth to study the close relationships between Mt. Wuyi, Mt. Huangshan and Mt. West Tianmu, where is the distri bution center of the East-Asiatic endemic genera. The above three mountain regions share half of the East-Asiatic endemic genera, and about 32% genera of the others are found in two of them (Fig. 2). Myuriopsis, one of the East Asiatic types, was only recorded in Taiwan Pro vince, Japan and Korea. Neodolichomitra, occuring in Taiwan Province, is endemic to China. More or less the differentiation has taken place in Mt. Huangshan, Mt. West Tianmu and Mt. Wuyi. The number of the East-Asiatic endemic genera is smaller in Mt. Wuyi, so it is possibly located on the border of the distributional center of the East-Asiatic endemic genera. Moreo ver, three of four East-Asiatic endemic genera in Mt. Shennongjia are also found in Mt. Huang shan and Mt. West Tianmu, but the other East-Asiatic genus in Mt. Wuyi is common to the mountain areas in SW China, the Qinglin Range of NW China, and the isolated mountain areas of NE China. Considering all the characteristics of the bryoflora of Mt. Shennongjia, we assume that Mt. Shennongjia may belong to another distribution center, including SW part of Sichuan Province, and the other neighbouring mountains.     

福建苔类和角苔类植物最新名录与区系分析

福建地处亚热带,其维管植物多样性已经有过广泛的研究,但其苔类和角苔类植物的多样性却鲜为人知。在本研究中,作者基于先前的苔藓植物文献报道和近期的野外工作以及对华东师范大学标本馆部分馆藏标本的研究结果,编写了福建苔类和角苔类植物的最新名录。福建共有苔类植物41科79属351种,角苔类植物1科4属6种。本研究新增福建苔类新记录82种。福建苔类和角苔类植物区系主要由细鳞苔科（94种）,耳叶苔科（32种）,羽苔科（25种）,扁萼苔科（23种）和指叶苔科（21种）等一些热带和亚热带的大科组成。除种数较多的属以外,63个属的种数不足5种,其中包括33个单种属。福建苔类和角苔类植物的区系地理分布主要以东亚、热带亚洲和北温带成分为主。福建特有种仅Solenostoma parviperianthum一种。与台湾相比,尽管两地植物间具有较高的相似性,福建在苔类和角苔类植物的多样性以及特有成分上都还远不及台湾丰富。     

福建苔类和角苔类植物最新名录与区系分析

福建地处亚热带,其维管植物多样性已经有过广泛的研究,但其苔类和角苔类植物的多样性却鲜为人知。在本研究中,作者基于先前的苔藓植物文献报道和近期的野外工作以及对华东师范大学标本馆部分馆藏标本的研究结果,编写了福建苔类和角苔类植物的最新名录。福建共有苔类植物41科79属351种,角苔类植物1科4属6种。本研究新增福建苔类新记录82种。福建苔类和角苔类植物区系主要由细鳞苔科（94种）,耳叶苔科（32种）,羽苔科（25种）,扁萼苔科（23种）和指叶苔科（21种）等一些热带和亚热带的大科组成。除种数较多的属以外,63个属的种数不足5种,其中包括33个单种属。福建苔类和角苔类植物的区系地理分布主要以东亚、热带亚洲和北温带成分为主。福建特有种仅Solenostoma parviperianthum一种。与台湾相比,尽管两地植物间具有较高的相似性,福建在苔类和角苔类植物的多样性以及特有成分上都还远不及台湾丰富。     

贵州乌江东风水库库区消落带苔藓植物区系分析

采用典型调查与路线调查相结合的方法,对贵州乌江东风水库库区消落带苔藓植物区系的物种组成、生活型、分布区类型和丰富性进行了调查和分析.结果表明:该区域共有苔藓植物18科58属101种,其中,藓类植物有16科56属99种,苔类植物有2科2属2种;优势科为灰藓科(Hypnaceae)、青藓科(Brachytheciaceae)和丛藓科(Pottiaceae),优势属为青藓属(Brahchythecium B.S.G.)、真藓属(Bryum Hedw.)和小曲尾藓属〔Dicranella(Müll.Hal.)Schimp.〕;单属科和单种属所占比例均较高,分别占该区域苔藓植物总科数和总属数的500%和638%.该区域分布的苔藓植物生活型可分为交织型、丛集型、垫状和平铺型4类,以丛集型种数最多(48种),占该区域苔藓植物总种数的475%.该区域分布的苔藓植物可划分为12个分布区类型,其中,温带成分种类最多,所占比例为815%;热带成分所占比例仅为185%;中国特有种所占比例也较高,为207%.该区域苔藓植物的丰富性综合系数(Si)为-03608,低于相邻的六冲河下游流域.综合分析结果表明:该区域的苔藓植物多样性较为丰富,多数种类具有较强的抗逆性,且丛集型苔藓种类最多,与库区消落带的特殊生境相适应;地理成分以东亚成分和北温带成分为主,总体属温带性质,且中国特有种较多,反映出该区域苔藓植物区系的特殊性和复杂性.     

中国苔藓植物的地理分区及分布类型

在对中国苔藓植物相关研究资料进行总结归纳的基础上,对中国苔藓植物的分区进行了重新划分,将最初的7个分区划分为10个分区,从华中区中分出华东区,由华北区中分出华西区,并将青藏区及云贵区内的云南西北部、四川西南部和西藏东南部组成单独的横断山区。就中国苔藓植物的分布类型及可能的分布路线也作了讨论,指出中国苔藓植物的分布路线有3条,一条是从喜马拉雅地区经滇西北、川西沿长江流域到中国的东南部;一条位于喜马拉雅、横断山区和台湾之间;第三条则从喜马拉雅地区通过秦岭直至长白山区。