New mammal remains from the Late Cretaceous Bostobe Formation (Northeast Aral Sea Region,Kazakhstan)

Four recently collected mammal specimens from the Upper Cretaceous (Santonian–?Campanian) Bostobe Formation in the northeastern Aral Sea Region, Kazakhstan are attributed to Asioryctitheria indet. (an edentulous dentary fragment) and the zhelestid Parazhelestes sp. cf. P. mynbulakensis (a maxillary fragment with a double-rooted canine, an M1, and a dentary fragment including m3). These new records double the known mammal fauna from this formation, which previously included the zhelestid Zhalmouzia bazhanovi and Zhelestidae indet. The taxonomic and ecological structure of the mammal assemblage from the Bostobe Formation can, on present evidence, be considered close to the other eutherian dominated Late Cretaceous mammal assemblages of Central Asia. This region is important in particular in the search for Late Cretaceous ancestors of crown-group eutherian mammal clades (Placentalia).     

Cretaceous Therian Tarsals and the Metatherian-Eutherian Dichotomy

Diverse metatherian and eutherian tarsal remains from the Late Cretaceous (middle-late Turonian) Bissekty Formation, Kyzylkum Desert, Uzbekistan (ca 90 MYA) are described. Their functional and taxonomic properties, along with those of other tarsal evidence, led to a reassessment of polarity hypotheses of therian, metatherian, and eutherian cruropedal attributes, and the consequences of this for phylogeny of taxa. There are calcaneal remains of several types of marsupials, and a single astragalus that probably belongs to one of these. This represents greater taxonomic diversity than the dental record suggests. Exceptionally large and distally extending peroneal processes, and small and steeply angled calcaneocuboid articulations facing mediodistally, as seen in the Early Cretaceous Sinodelphys and other Cretaceous and Paleogene taxa, attest not only to the metatherian status of these specimens, but also to the retention of many ancestral therian features, even more so than in both the Tiupampa and Itaboraí marsupials of the South American Paleocene (both the calcanea and the astragalus suggest therian traits that are decidedly unlike those of symmetrodonts). Calcanea allocated to the deltatherioid species at Bissekty testify unequivocally to their metatherian affinity. The morphology of the best represented sample of eutherian calcanea from Bissekty, presumably of a number of zhelestid species, appears to be more derived than that of the Late Cretaceous/Paleocene Protungulatum in having a much more reduced peroneal process and a calcaneocuboid articulation that faces distally, oriented nearly at a 90° angle to the long axis of the calcaneus. In fact, this distally facing facet, common in later eutherians (except for lineages in the Paleogene record, and various Carnivora), may not be diagnostic of either the protoeutherian, or even of the protoplacentalian, in spite of its presence in Eomaia. Many putatively “basal” lineages have derived characters, hence such outgroups should not be considered the unequivocal repositories of only ancestral character states.     

About some aporrhaid and strombid gastropods from the Late Cretaceous

Sixteen species of the Stromboidea (Gastropoda) from the Late Cretaceous are described in this study. One species belongs to the Strombidae, the others to eight genera and subgenera of the Aporrhaidae. Eight species are new. They have been found in the Cenomanian of Kassenberg in western Germany, the Coniacian of the Mungo River in Cameroon, the Santonian of the Eastern Cape Province of South Africa, the Santonian/Campanian of the Ariyalur area in southern India, the Campanian of northern Spain, and the Maastrichtian of the Western Desert in Egypt. Two species ofDrepanocheilus from South Africa are considered stem-group representatives of the aporrhaids which inhabited the Weddellian Province in the early Tertiary. One new species of the strombid genusHippocrenes is regarded as an early species of the evolutionary lineage leading to the Seraphsidae. The new species areLatiala? ponsi, Drepanocheilus herberti, Drepanocheilus triliratus, Drepanocheilus (Tulochilus) jouberti, Graciliala quaasi, Kaunhowenia catalanica, Kaunhowenia punctata andHippocrenes kussi.     

基因组学时代的真菌分类学:机遇与挑战

真菌物种的形态特征有限,加之形态滞后和形态可塑性,仅靠外部形态、内部结构及生理生化指标,很难把握真菌的系统亲缘。应用DNA测序、基因组测序、比较基因组学及生物信息学等技术,研究人员可以快速识别真菌演化中出现的数量众多的单系支系,为建立各分类等级的新分类单元提供有力证据,为真菌分类学研究带来了新的希望和活力。自2000年以来,在真菌界至少发表了1新亚界、4新门、7新亚门、19新纲、9新亚纲、40余新目等高级分类单元。近3年来,我国发表了20余个真菌新属,其中绝大多数属的建立都有分子证据支持。可以预见,大量的新种、新属、新科乃至更高级分类单元将会在今后10年内持续发现和建立。这必将大大促进真菌分类学的发展,完善现有的真菌分类系统。我们应该顺势而上,利用我国丰富的真菌资源,为真菌分类学的发展做出应有贡献。与此同时,真菌分类学也面临着十分严峻的挑战。挑战主要来自3个方面,一是研究变得越来越综合,不但需要有相应的研究经费支持,而且要求从事该领域的研究人员技术更全面、知识更广博及知识更新速度更快捷;二是新物种描述进度偏慢,远远不能满足人们对物种认识和利用的日益增长的需要;三是研究人员亟需创新研究模式,以新技术、新思路、新机制来构建新的真菌分类学,加速新物种的发现和描述进度,最终为社会进步和科学发展服务。     

Infrasectional systematics of the genus Sideritis L. section Sideritis (Lamiaceae)

RIVERA NUÑEZ, D., OBON DE CASTRO, C., TOMAS-LORENTE, F., FERRERES, F. & TOMAS-BARBERAN, F. A., 1990. Infrasectional systematics of the genus Sideritis L. section Sideritis (Lamiaceae). A new taxonomic division of the section Sideritis is proposed on the basis of morphological, cytological and chemical characters. The following subsections art-recognized: Grandiflora, Ovata, Camarae, Linearifolia, Gymnocarpae, Stachydioides, Lacaitae, Hirsuta, Chamaedryfolia, Arborescens, Flavovirens, Leucantha, Angustifolia, Serrata and Scordioides . Possible evolutionary pathways are discussed.     

The spatio-temporal colonization and diversification across the Indo-Pacific by a ‘great speciator’ (Aves,Erythropitta erythrogaster)

The Indo-Pacific region has arguably been the most important area for the formulation of theories about biogeography and speciation, but modern studies of the tempo, mode and magnitude of diversification across this region are scarce. We study the biogeographic history and characterize levels of diversification in the wide-ranging passerine bird Erythropitta erythrogaster using molecular, phylogeographic and population genetics methods, as well as morphometric and plumage analyses. Our results suggest that E. erythrogaster colonized the Indo-Pacific during the Pleistocene in an eastward direction following a stepping stone pathway, and that sea-level fluctuations during the Pleistocene may have promoted gene flow only locally. A molecular species delimitation test suggests that several allopatric island populations of E. erythrogaster may be regarded as species. Most of these putative new species are further characterized by diagnostic differences in plumage. Our study reconfirms the E. erythrogaster complex as a ‘great speciator’: it represents a complex of up to 17 allopatrically distributed, reciprocally monophyletic and/or morphologically diagnosable species that originated during the Pleistocene. Our results support the view that observed latitudinal gradients of genetic divergence among avian sister species may have been affected by incomplete knowledge of taxonomic limits in tropical bird species.     

中国白垩纪蜂窝蛋化石的分类订正

重新系统描述了蜂窝蛋科蜂窝蛋属的模式蛋种宁夏蜂窝蛋(Faveoloolithus ningxiaensis)和杨氏蛋属的模式蛋种夏馆杨氏蛋(Youngoolithus xiaguanensis),并记述了产自浙江天台的蜂窝蛋科新材料,建立一个新的蛋属———副蜂窝蛋属(Parafaveoloolithus),及3个新的蛋种———Parafaveoloolithus microporus,P.macroporus和P.tiansicunensis。根据赵资奎1994年提出的恐龙蛋分类中具有鉴定意义的几个特征,重新讨论了现有蜂窝蛋的分类地位,提出杨氏蛋属应当提升为科一级的分类单元,总结了蜂窝蛋科内属级和种级分类单元的主要鉴定特征以及蜂窝蛋类的鉴定方法。