国产爵床科芦莉花族植物的花粉形态

报道了国产爵床科Acanthaceae芦莉花族Ruellieae芦莉花亚族Ruelliinae 2属7种、假杜鹃亚族Barlerinae 1属3种和马蓝亚族Strobilanthinae 16属34种植物扫描电镜下的花粉形态.芦莉花亚族的地皮消属Pararuellia和喜花草属Eranthemum的花粉均为圆球形,具3孔或3孔沟,外壁为不同的网状结构; 假杜鹃亚族的假杜鹃属Barleria的花粉为长球形,具3孔沟,外壁亦为网状结构;马蓝亚族植物(包含广义的马蓝属Strobilanthes s.l.)花粉形态多样,结构复杂.依据花粉萌发孔和外壁纹饰特征,可将马蓝亚族16属植物和上述两亚族3属植物的花粉形态归纳成3大类型: 1. 具3孔类型.其中又有(1)外壁具网状纹饰者,见于地皮消属; (2)外壁具芽胞状纹饰者,见于黄猄草属Championella; (3)外壁具刺状(棒状)纹饰者,见于南一笼鸡属Paragutzlaffia、叉花草属Diflugossa和假蓝属Pteroptychia.2. 具3孔沟及具3孔沟与假沟类型(肋条带型).其中又有(1)具3孔沟和网状纹饰者,见于喜花草属和假杜鹃属; (2)具刺状(棒状)纹饰者,见于南一笼鸡属、叉花草属和假蓝属; (3)具3孔沟与假沟,外壁纹饰具节隔、肋条带状或网状,网眼纵向排列成行,网眼内有细网纹者,见于耳叶马蓝属Perilepta、马蓝属Pteracanthus(大部分)、金足草属Goldfussia、紫云菜属Strobilanthes(部分)和合页草属Sympagis; (4)具3孔沟与假沟类型,肋条带状,但不具节隔,外壁纹饰网状,网眼不成行或不明显纵向排列,网内无细网纹者,见于尖蕊花属Aechmanthera、板蓝属Baphicacanthus、马蓝属(部分)和糯米香属Semnostachya; (5)具双脊及细网状纹饰者,见于环毛紫云菜Strobilanthes cycla.3. 具(4-)5孔沟及假沟类型(肋条带型),外壁具网状或拟网状纹饰,见于腺背蓝属Adenacanthus.另外兰嵌马蓝属Parachampionella、山一笼鸡属Gutzlaffia和肖笼鸡属Tarphochlamys的花粉有无萌发孔尚不清楚,有待进一步研究.综上所述,芦莉花族植物的花粉形态具有较高的多样性,是重要的分类性状.利用花粉形态特征能较好地区分高级分类群如亚科、族以及亚族,有时也有助于阐明类群之间的相互关系,甚至也能用于区分属、种和阐明其关系.     

国产爵床科鳞花草族1属、穿心莲族2属和爵床族8属植物的花粉形态

报道了中国爵床科Acanthaceae爵床亚科Ruellioideae鳞花草族Lepidagathideae 1属、穿心莲族Andrographideae 2属和爵床族Justicieae 8属共14种植物的花粉形态。根据花粉萌发孔类型和外壁纹饰特征,可将这些植物的花粉归为4个类型: (1)具3孔沟,外壁具网状纹饰。该类型见于色萼花属Chroesthes (采自广西样品)和穿心莲属Andrographis植物。(2)具3孔沟及假沟(肋条带型)类型,外壁具网状纹饰,网眼纵向排列成行,网眼内有细网纹。该类型见于色萼花属(采自云南样品)和鳔冠花属Cystacanthus。(3)具3孔沟,沟两侧各有1条假沟,外壁具网状纹饰。该类型见于瑞丽山壳骨Pseuderanthemum shweliense、狗肝菜属Dicliptera和驳骨草属Gendarussa植物。(4)具2孔沟,沟两侧具斑块。该类型见于山壳骨属Pseuderanthemum 1种、纤穗爵床属Leptostachya、鳄嘴花属Clinacanthus、鸭嘴花属Adhatoda、杜根藤属Calophanoides和野靛棵属Mananthes植物。     

中国蓼属叉分蓼组植物花粉形态的研究

采用光学显微镜和扫描电镜对中国蓼属叉分蓼组20种3变种的花粉形态进行了观察和研究。结果表明其花粉形态大多数为近球形至近长球形,少数为扁球形或长球形;花粉大小为20.4～44.0µm×17.0～34.0µm：从萌发孔看,有3沟、3 孔沟、多沟、散沟;外壁纹饰为微刺—穴状、刺状、粗网状、皱块状。据此,该组花粉可划分为5种类型,即叉分蓼型(Aconogonon-type)、钟花蓼型(Campanulatum-type)、大连线冰岛蓼型(Forrestii-type)、西伯利亚蓼(Sibiricum-type)及多穗蓼型(Polystachyum-type),编制了这些花粉类型检索表。叉分蓼型花粉的主要特征是具3沟,外壁纹饰为微刺-穴状,此种类型的植物有14种2变种。钟花蓼型花粉的主要特征是具6散沟,外壁纹饰为微刺-穴状,此种类型的植物有钟花蓼和绒毛钟花蓼。西伯利亚蓼型花粉的主要特征是具3孔沟,外壁纹饰为皱块状,此种类型的植物有西伯利亚蓼。多穗蓼型花粉的主要特征是具6(~8)多沟,外壁纹饰为粗网状,此种类型的植物有松林蓼及多穗蓼。大连线冰岛蓼型花粉的主要特征是具散沟,外壁纹饰为显著的长刺状,此种类型的植物有大铜钱叶蓼及铜钱叶蓼,结果表明叉分蓼组的花粉形态具有重要的分类学意义,研究结果支持将叉分蓼组上升为属的等级,也支持Knorringia的属的地位,大铜钱叶蓼和铜钱叶蓼应移入Koenigia属中,而松林蓼和多穗蓼仍保留在蓼属中。     

光学显微镜下松柏类和菊科花粉的分类、鉴定要点及生态意义

本文对地层中广泛分布的松柏类和菊科花粉进行初步分类,讨论各类型(属)的鉴定特征及生态意义.以气囊的有无、外壁结构和纹饰、气囊的形态和纹饰、本体与气囊过渡点的特征、帽与帽缘纹理等为鉴定要点,对杉型、柏科型、刺柏型、红豆杉型、落叶松属、铁杉属、罗汉松属、云杉属、雪松属、冷杉属、油杉属和松属(双束松型和单束松型)13个类型的松柏类植物花粉逐步分类.通过总结前人研究和统计分析,讨论落叶松属、铁杉属、罗汉松属、云杉属、雪松属、冷杉属、油杉属和松属,特别是双束松型和单束松型花粉的生态环境指代意义.依据花粉的大小、外壁表面纹饰、外壁光切面中基柱层的结构和发育程度,初步拟将菊科花粉划分为6个类型,即菊苣-蒲公英型、紫菀型、春黄菊型、风毛菊型、蓝刺头型和蒿属,并通过对6个花粉类型植物母体生态环境的归纳总结和统计分析,讨论它们的生态环境指代意义.     

中国菊科植物的系统分类与区系的初步研究

为1993年"菊科植物的系统分类与区系地理的初步探讨"(世界)一文的姊妹篇,重点论述我国菊科的系统分类及其区系地理成分。文中介绍了分布我国的菊科240属隶于2亚科、5超族、11族中的系统位置。论述了我国菊科植物区系地理成分的特点是:1.大洲间共同分布或洲际间断分布的属多,且具明显的热带亲缘;2.与亚洲国家,包括中亚国家或亚洲热带国家共同分布的属多,尤其是成"中亚-青藏高原-喜马拉雅山"地区分布的属多;3.中国特有属多,其中我国西南省区特有属最多。文中还讨论了分布我国菊科各族祖先种的起源、迁移以及我国区系地理热带亲缘和"横断山脉-喜马拉雅山脉(东)森林植物亚区"菊科植物分布的特点。     

蜘蛛抱蛋亚族的花粉形态

本文研究并报道了百合科蜘蛛抱蛋亚族的花粉形态,主要结论如下：1．开口箭属含两种花粉类型即：(1)单槽、椭圆形;(2)无萌发孔、球形。具单槽、椭圆形花粉的种类含单型性核型,花形较小,柱头小而花柱短,雄蕊高于柱头;无萌发孔、球形花粉的种类则为单型性核型,花形较大,柱头常高度膨大,雄蕊常着生在花被筒基部。2．万年青属花粉为椭圆形,具单槽;蜘蛛抱蛋属花粉则为球形,无萌发孔;开口箭属花粉一部分与万年青属相似,另一部分则与蜘蛛抱蛋属雷同。3．蜘蛛抱蛋亚族中最原始的花粉类型为单槽椭圆形,具孔状或网状外壁纹饰。球形,无萌发孔,外壁具皱波状、瘤状或芽孢状纹饰的花粉为派生类型。4．蜘蛛抱蛋亚族种下花粉形状、萌发孔类型和外壁纹饰基本稳定,可作为分种特征。     

新疆千里光族花粉形态研究

在光学显微镜和扫描电镜下,对分布于新疆的菊科千里光族４属２６种植物的花粉进行了观察。根据萌发沟长短和外壁纹饰待征将各属分成二种类型：（１）具长萌发沟：有橐吾属、千里光属和多榔菊属。（２）具短萌发沟：仅有款冬属。由此可看出,款冬是较独立的一类,与其余各属在亲缘关系上相距较远。花粉形态特征为多榔菊属分类地位的探讨提供了资料。同时也为橐吾属两新种的成立提供了孢粉学证据。     

中国大蒜芥族植物花粉形态的研究

对中国大蒜芥族10属14种植物花粉形态分别进行了光镜和扫描电镜下的观察研究。结果表明该族花粉形态可划分为4种类型：（1）具3沟,超长球形,网状纹饰,外壁2层;（2）具3沟,超长球形,细网状纹饰,外壁1层;（3）具3沟（偶4沟）,长球形,网状纹饰,外壁2层;（4）具6沟,长球形,网状纹饰,外壁2层。因此,中国大蒜芥族的花粉形态多样性程度较高,说明了它不是一个自然类群,是一个多系类群,这与前人研究结果相一致。另外,本文首次报道十字花科锥果芥属植物具6沟花粉,具6沟花粉在十字花科中极为特殊,所以作者将锥果芥属提升为族级,另立新族,即锥果芥族（Tribe Berteroelleae F．Z．Li,G．Y．Tang ＆ Z．Y．Sun,trib．nov．）。     

中国沙拐枣属植物花粉形态及其在地层研究中的意义

通过光学显微镜和扫描电镜观察了中国沙拐枣属(Calligonum L.)11种植物的花粉形态。按扫描电镜下的外壁纹饰分类,该属花粉可分为4种类型,即:网纹-穴状具圆形或近圆形网眼、网纹-穴状具多角型网眼、网纹-穿孔和网纹-穿孔或小沟渠。它们的演化趋势是从前面类型依次向后面类型演化。根据花粉内孔的形状,沙拐枣属植物花粉可区别于蓼科其它属植物三孔沟类型花粉。     

中国红豆杉科花粉形态的研究

红豆杉科(Taxaceae),花粉近球形,有时稍扁或稍长。直径为20．8-45．8μm。具远极 薄壁区,或不典型的乳头状突起。外壁两层,内外层厚度相等,有时层次不明显。在光学显微 镜下,外壁表面粗糙,或具微弱的颗粒状纹饰。在穗花杉(Amentotaxus argotaenia)这个种里,有些花粉粒具残存气囊。在扫描电镜下,外壁表面具粗瘤和细瘤两种纹饰类型。透射电镜本科各属代表种观察表明,本科花粉外壁内层具片状结构,外层由单层瘤状纹饰分子构成,有 些种细瘤连接形成覆盖层。根据花粉形态资料,可将本科植物分为2个族： 白豆杉族(仅包括白豆杉一个属)和红豆杉族(包括红豆杉属和榧树属)。 鉴于穗花杉属花粉的特殊性,建议独立上升为穗花杉科Amentotaxaceae。     

Development of the echinate pollen wall inFarfugium japonicum (Compositae: Senecioneae)

Development of the echinate pollen grains inFarfugium (Compositae: Senecioneae) has been studied by a combination of transmission electron microscopy and field emission scanning electron microscopy with a freeze fractured method. The inner surface of the callose wall surrounding each microspore does not possess an echinate pattern before primexine deposition begins. The primexine formation coincides with the initiation of spines. The freeze fractured primexine shows probacula which form transverse rods. The developing exine has an inner spongy substructure. The endexine is formed by the accumulation of the electron dense lamellae with white lines after the dissolution of the callose wall. In the present study, it is confirmed that the developmental process of pollen formation revealed in the field emission scanning electron microscope is consistent with the results obtained using the transmission electron microscope.     

Origin and divergence of Afro-Indian Picrodendraceae: linking pollen morphology,dispersal modes,fossil records,molecular dating and paleogeography

The pantropical Picrodendraceae produce mostly spheroidal to slightly oblate, echinate pollen grains equipped with narrow circular to elliptic pori that can be hard to identify to family level in both extant and fossil material using light microscopy only. Fossil pollen of the family have been described from the Paleogene of America, Antarctica, Australia, New Zealand, and Europe, but until now none have been reported from Afro-India. Extant pollen described here include representatives from all recent Picrodendraceae genera naturally occurring in Africa and/or Madagascar and south India and selected closely related tropical American taxa. Our analyses, using combined light microscopy and scanning electron microscopy, show that pollen of the Afro-Indian genera encompass three morphological types: Type 1, comprising only Hyaenanche; Type 2, including Aristogeitonia, Mischodon, Oldfieldia and Voatamalo; Type 3, comprising the remaining two genera, Androstachys and Stachyandra. Based on the pollen morphology presented here it is evident that some previous light microscopic accounts of spherical and echinate fossil pollen affiliated with Arecaceae, Asteraceae, Malvaceae, and Myristicaceae from the African continent could belong to Picrodendraceae. The pollen morphology of Picrodendraceae, fossil pollen records, a dated intra-familial phylogeny, seed dispersal modes, and the regional Late Cretaceous to early Cenozoic paleogeography, together suggest the family originated in the Americas and dispersed from southern America across Antarctica and into Australasia. A second dispersal route is believed to have occurred from the Americas into continental Africa via the North Atlantic Land Bridge and Europe.     

藜科植物的起源、分化和地理分布

全球藜科植物共约130属1500余种,广泛分布于欧亚大陆、南北美洲、非洲和大洋洲的半干旱及盐碱地区。它基本上是一个温带科,对亚热带和寒温带也有一定的适应性。本文分析了该科包含的1l族的系统位置和分布式样,以及各个属的分布区,提出中亚区是现存藜科植物的分布中心,原始的藜科植物在古地中海的东岸即华夏陆台(或中国的西南部)发生,然后向干旱的古地中海沿岸迁移、分化,产生了环胚亚科主要族的原始类群;起源的时间可能在白垩纪初,冈瓦纳古陆和劳亚古陆进一步解体的时期。文章对其迁移途径及现代分布式样形成的原因进行了讨论。     

POLLEN MORPHOLOGY OF HAPLOPAPPUS AND RELATED GENERA (COMPOSITAE—ASTEREAE)

Pollen grains of Haplopappus and related genera in the subtribe Solidaginae from North and South America were examined by light and scanning electron microscopy. The grains are consistently tricolporate and echinate. Some genera can be distinguished by pollen size, spine length, and number of spine rows between colpi. Based on these characters, the divergence of Benitoa from other members of the subtribe, as indicated by its morphology and secondary chemistry, is supported. Additionally, the recently suggested absence of a close relationship between Pyrrocoma and Oonopsis is indicated by their contrasting pollen types. This study demonstrates the potential of pollen studies in distinguishing some taxonomic groups in the Astereae.     

中国和其他全北界三趾马的头骨和头后骨骼形态比较(英文)

由于地理位置上处于北美和旧大陆西部之间,中国晚中新世的三趾马提供了重要的生物地层与生物地理信息。这些信息反映出晚中新世时期北美和欧亚大陆之间的动物群交流,同时也与当时的古环境变迁相关联。依据面部和牙齿形态以及肢骨比例,将中国的三趾马与欧亚大陆及北美的其他种类进行了对比。中国的三趾马可识别出两个分类类群,其中一个非系统发育意义上的类群包括 Hipparion dermatorhinum,H. weihoense,H. fossatum,H. hippidio-dus 和 H. coelophyes,这一类群与旧大陆西部的三趾马在形态上高度相似; 另一个为本土类群,包括 H. ptychodus,H. platyodus,H. tylodus,H. sefvei 和 H. plocodus,它们与其他地区的种类并无相似之处。前一个类群是中国北方草原型动物群中的典型分子,对欧亚大陆化石地点的生物地层对比相当重要; 后一类群与北美的三趾马( "Cormohipparion"属) 在面部形态上具有相似性,这些本土的三趾马是中国北方森林型动物群的分子。     

Origin,Differentiation, and Geographic Distribution of the Chenopodiaceae

Numbers of species and genera,endemic genera,extant primitive genera,relationship and distribution patterns of presently living Chenopodiaceae(two subfamilies,12 tribes,and 118 genera)are analyzed and compared for eight distributional areas,namely central Asia,Europe,the Mediterranean region,Africa,North America,South America, Australia and East Asia． The Central Asia,where the number of genera and diversity of taxa are greater than in other areas,appears to be the center of distribution of extant Chenopodiaceae．North America and Australia are two secondary centers of distribution． Eurasia has 11 tribes out of the 12,a total of 70 genera of extant chenopodiaceous plants,and it contains the most primitive genera of every tribe． Archiatriplex of Atripliceae,Hablitzia of Hablitzeae,Corispermum of Corispermeae,Camphorosma of Camphorosmaea,Kalidium of Salicornieae,Polecnemum of Polycnemeae,Alexandra of Suaedeae,and Nanophyton of Salsoleae,are all found in Eurasia,The Beteae is an Eurasian endemic tribe,demonstrating the antiquity of the Chenopodiaceae flora of Eurasia．Hence,Eurasia is likely the place of origin of chenopodiaceous plants． The presence of chenopodiaceous plants is correlated with an arid climate．During the Cretaceous Period,most places of the continent of Eurasia were occupied by the ancient precursor to the Mediterranean,the Tethys Sea．At that time the area of the Tethys Sea had a dry and warm climate．Therefore,primitive Chenopodiaceae were likely present on the beaches of this ancient land．This arid climatic condition resulted in differentiation of the tribes Chenopodieae,Atripliceae,Comphorosmeae,Salicornieae,etc．,the main primitive tribes of the subfamily Cyclolobeae. Then following continental drift and the Laurasian and Gondwanan disintegration, the Chenopodiaceae were brought to every continent to propagate and develop, and experience the vicissitudes of climates, forming the main characteristics and distribution patterns of recent continental floras. The tribes Atripliceae, Chenopodieae, Camphorosmeae, and Salicornieae of recent Chenopodiaceae in Eurasia, North America, South America, southern Africa, and Australia all became strongly differentiated. However, Australia and South America, have no genera of Spirolobeae except for a few maritime Suaeda species. The Salsoleae and Suaedeae have not arrived in Australia and South America, which indicates that the subfamily Spirolobeae developed in Eurasia after Australia separated from the ancient South America-Africa continent, and South America had left Africa. The endemic tribe of North America, the tribe Sarcobateae, has a origin different from the tribes Salsoleae and Suaedeae of the subfamily Spirolobeae. Sarcobateae flowers diverged into unisexuality and absence of bractlets. Clearly they originated in North America after North America had left the Eurasian continent. North America and southern Africa have a few species of Salsola, but none of them have become very much differentiated or developed, so they must have arrived through overland migration across ancient continental connections. India has no southern African Chenopodiaceae floristic components except for a few maritime taxa, which shows that when the Indian subcontinent left Africa in the Triassic period, the Chenopodiaceae had not yet developed in Africa. Therefore, the early Cretaceous Period about 120 million years ago, when the ancient Gondwanan and Laurasian continents disintegrated, could have been the time of origin of Chenopodiaceae plants.The Chinese flora of Chenopodiaceae is a part of Chenopodiaceae flora of central Asia. Cornulaca alaschnica was discovered from Gansu, China, showing that the Chinese Chenopodiaceae flora certainly has contact with the Mediterranean Chenopodiaceae flora. The contact of southeastern China with the Australia Chenopodiaceae flora, however, is very weak.     

Comparative pollen morphology of Brachylena, Tarchananthus and two species of Tubulifloridites (Asteraceae) from the Eocene, Knysna Lignite of South Africa

Two fossil taxa Tubulifloridites antipodica and T. viteauensis recovered from the Eocene Knysna Lignite of South Africa were examined with scanning (SEM) and transmission electron microscopy (TEM). The details of their sculpturing and wall structure are similar to the same species of fossil dispersed pollen taxa recovered from southwestern Africa and South America. Fifteen species of the woody South African taxa, Brachylaena (9 species) and Tarchonanthus (6 species) were investigated with SEM and TEM. All of the taxa are tricolporate, spherical to slightly prolate, microechinate to echinate and have a bilayered columellate infrastructure, except B.ilicifolia, which has a single columellate infrastructural level with the “granularization” of the outer portion of the infrastructural layer or the inner layer of the tectum. There is a similar distribution of plesiomorphic and derived pollen characters in a number of aster subfamilies and tribes suggesting a similar evolutionary progression of pollen, and pollen wall character evolution was occurring synchronously in a variety of aster subfamilies during the middle Tertiary and that these unique pollen features may be important to the evolution and diversification of the Asteraceae.     

西藏和北极巴罗地区菊科植物几个属的花粉

对西藏和北极巴罗地区菊科4个属(蒿属、飞蓬属、风毛菊属和千里光属)17个种的花粉形态进行了光学和扫描电子显微镜的观察、比较。结果表明这两个地区菊科4个属的花粉粒大多为球形或近球形,少数是扁球形或长球形。萌发孔的类型均为三孔沟。但在花粉大小、萌发孔形状、外壁厚度以及表面纹饰等方面存在差异。通过对这两个地区菊科植物花粉形态的观察有可能为菊科分化、迁移,以及化石孢粉的研究提供参考资料。