低等金缕梅类的系统学：分子和发育学证据

传统的低等金缕梅类包含7个科，即领春木科（Eupteleaceae）、昆栏树科（Trochodendraceae）、水青树科（Tetracentraceae）、连香树科（Cercidiphyllaceae）、折扇叶科（Myrothamnaceae）、悬铃木科（Platanaceae）和金缕梅科（Hamamelidaceae）。这些科之间的谱系关系以及金缕梅科内部的谱系关系是研究被子植物系统和进化的主要问题之一。本研究的目的在于通过对现有的和本研究中产生的分子和发育学资料的分析来对这些谱系问题进行探讨，希望使我们对这些类群的认识提高到了一个新的水平。 本研究测定了包括连香树科、领春木科、悬铃木科、水青树科和金缕梅科内所有亚科代表共计14个种的rbcL基因，matK基因和18S-26S核核糖体（nrDNA）内转录间隔区（ITS）的序列，并结合原有资料对所有低等金缕梅类（除非洲分布的折扇叶科）及其相近类群进行了分支分析。主要结论包括;传统低等金缕梅类是一个复系类群;金缕梅科也是一个复系类群;ITS序列分析支持将连香树科包含在金缕梅科内，但是，rbcL资料和matK资料不支持将连香树科包含在金缕梅科内。本研究支持金缕梅科内6个亚科的分类系统，即将其分为阿丁枫亚科（Altingioideae）、红花荷亚科（Rhodoleioideae）、马蹄荷亚科（Exbucklandioideae）、壳菜果亚科（Mytilarioideae）、双花木亚科（Disanthoideae）和金缕梅亚科（Hamamelidoideae），但壳菜果亚科的山桐柴属（Chunia）应置于马蹄荷亚科内。 本研究首次描述和报道了金缕梅科5个亚科6个种的花的形态发生。通过对本研究发现的新证据和文献中记载的资料分析表明金缕梅科的花发育的特征无明显的共同式样。从本研究提供的花发育资料得出的值得注意的结论是红花荷属在金缕梅科中的亚科地位得到支持。对牛鼻栓（Fortunearia sinensis Rehd. et Wils.）的花发育研究表明其花性分化在发育晚期才出现。 本文首次对显脉红荷（Rhodoleia henryi Tong）的胚胎学进行了研究。尽管红花荷属是金缕梅科内适应鸟传粉的特化类群，但其胚胎学的特征与金缕梅科其它植物并无明显区别。因此，本研究不支持红花荷属独立成科而支持其在金缕梅科内的亚科地位。

Early - Late Miocene palaeoclimate data and palaefloras of 48 samples from Southern China

Southern China, especially Yunnan, has undergone high tectonic activity caused by the uplift of Himalayan Mountains during the Neogene, which led to a fast changing palaeogeography. Previous study shows that Southern China has been influenced by the Asian Monsoon since at least the Early Miocene. However, it is yet not well understood how intense the Miocene monsoon system was. In the present study, 63 fossil floras of 16 localities from Southern China are compiled and evaluated for obtaining available information concerning floristic composition, stratigraphic age, sedimentology, etc. Based on such reliable information, selected mega- and micro-floras have been analysed with the coexistence approach to obtain quantitative palaeoclimate data. Visualization of climate results in maps shows a distinct spatial differentiation in Southern China during the Miocene. Higher seasonalities of temperature and precipitation occur in the north and south parts of Southern China, respectively. During the Miocene, most regions of Southern China and Europe were both warm and humid. Central Eurasia was likely to be an arid center, which gradually spread westward and eastward. Our data provide information about Miocene climate patterns in Southern China and about the evolution of these patterns throughout the Miocene, and is also crucial to unravel and understand the climatic signals of global cooling and tectonic uplift.

Table 2. Percentage of palynomorphs found in each sample through Longling section

The Longling Coal Mine (W. Yunnan) is situated in an area of substantial geotectonic activity. Its Late Pliocene palynoflora is of considerable interest, since the area represents a centre of biodiversity. Eighty-two palynomorphs belonging to 61 families were recovered from the lignite. The palynoflora is dominated by angiosperms (68.3%), with ferns (24.4%), gymnosperms (4.9%) and algae (2.4%). Comparisons indicate that most of the palynoflora was derived from the Montane Humid Evergreen Broad-leaved Forest, with lesser contributions from the Tsuga dumosa Forest and Evergreen Coniferous Broad-leaved Mixed Forest, as well as the Montane Mossy Evergreen Broad-leaved Forest. This indicates that the Late Pliocene climate was cooler than that of the present. In the course of the accumulation of the lignite, the climate underwent five major phases of warming and cooling.