Evidence for a phylogenetic position of button quails (Turnicidae: Aves) among the Gruiformes

The phylogenetic position of the Turnicidae (Aves) was unresolved. Historically, they were classified as members of the Struthioniformes, Galliformes, Charadriiformes, Columbiformes or the Gruiformes. In these classifications they had taxonomic rank of order 'Turniciformes' or family 'Turnicidae'. However, most of these studies followed phenetic methodology and used morphological similarity of taxa and plesiomorphic characters to classify Turnix . Recent phylogenetic studies on the basis of morphological character analyses or phenetic comparisons based on DNA-DNA hybridization experiments failed to clarify the phylogenetic realtionship of Turnix and suggested a position as 'incerte sedis', either among the Gruiformes or as the parvclass 'Turnicac'as a sistergroup to the 'Neoaves'.
We studied skeletal and myological material of Turnix to resolve its phylogenetic position. Further, we considered all characters that were previously discussed in literature to classify Turnix and tested them for their potential use in phylogenetic analysis. We added several yet unemployed morphological characters of phylogenetic significance to the analysis. The Struthioniformes, 'Galloanseres', and Columbiformes are each characterized by a clear set of autapomorpies. Only one autapomorphy in known for the Gruiformes but this character is of satisfying consistency and can be found in all families of the Gruiformes (Gruidae, Psophiidae, Aramidae. Rallidae) and Turnix. Turnix and the Rallidae share four complex morphological characters implying a close phylogenetic relationship. The data presented in this paper support the hypothesis that Turnix is a member of the Gruiformes with close relationships to the Rallidae. No evidence was found that would support a parvclass 'Turnicae'as sistergroup to the 'Neoaves'.     

‘On being the right size’ – Do aliens follow the rules?

Aim

To assess whether mammalian species introduced onto islands across the globe have evolved to exhibit body size patterns consistent with the ‘island rule,’, and to test an ecological explanation for body size evolution of insular mammals.

Location

Islands worldwide.

Methods

We assembled data on body mass, geographical characteristics (latitude, maximum elevation) and ecological communities (number of mammalian competitors, predators and prey) for 385 introduced populations across 285 islands, comprising 56 species of extant, non‐volant mammals. We used linear regression, ANCOVA and regression tree analyses to test whether introduced populations of mammals exhibit the island rule pattern, whether the degree of body size change increased with time in isolation and whether residual variation about the general trend can be attributed to the geographical and ecological characteristics of the islands.

Results

Introduced populations follow the predicted island rule trend, with body size shifts more pronounced for populations with greater residence times on the islands. Small mammals evolved to larger body sizes in lower latitudes and on islands with limited topographic relief. Consistent with our hypothesis on the ecology of evolution, body size of insular introduced populations was influenced by co‐occurring species of mammalian competitors, predators and prey.

Conclusion

The island rule is a pervasive pattern, exhibited across a broad span of geographical regions, taxa, time periods and, as evidenced here, for introduced as well as native mammals. Time in isolation impacts body size evolution profoundly. Body size shift of introduced mammals was much more pronounced with increasing residence times, yet far less than that exhibited by native, palaeo‐insular mammals (residence times > 10,000 years). Given the antiquity of many species introductions, it appears that much of what we view as the natural character and ecological dynamics of recent insular communities may have been rendered artefacts of ancient colonizations by humans and commensals.     

Phylogenetic Autocorrelation Analysis of Extinction Risks and the Loss of Evolutionary History in Felidae (Carnivora: Mammalia)

Phylogeny provides a natural measurement of biodiversity by allowing the computation of indexes that express the amount of phylogenetic diversity that are, in principle, independent of species counts and provides an objective measurement to evaluate the amount of biodiversity lost under the ongoing extinction crisis. In this note, we analyzed patterns of phylogenetic autocorrelation in extinction risks in Felidae (Mammalia: Carnivora) and estimated, using simulation procedures, the amount of phylogenetic diversity loss if k species are preserved in this clade. The simulations showed that loss of phylogenetic diversity based on the IUCN list for extinction threats in Felidae is within the expected values based on the simulated random model, a result also confirmed by the absence of phylogenetic autocorrelation in extinction risks, indicating that extinction threats are randomly distributed across the phylogeny. So, we confirm that loosing species will not necessarily generate a direct proportional loss of phylogenetic information and, consequently, that alternative measures of biodiversity could be used to establish conservation priorities under the common restriction of resources.     

Systematics Agenda 2000: an historical perspective

The publication of Systematics Agenda 2000 in February, 1994 represented an historic event in the collaboration of the systematic biology community designed to set a research agenda for a twenty five year period across the areas of basic and applied systematics. How the community came to take the initiative to produce such a consensus is outlined. Of special interest is the emergence of the Systematics Agenda 2000 initiative from a North American perspective to a truly global enterprise.     

奥陶纪苔藓动物的多样性演变——兼论苔藓动物的起源

苔藓动物是一类多为海生、滤食性的群体生物。奥陶纪是苔藓动物发生、演化辐射和灭绝的重要时期,也是苔虫礁形成的最早时期。已知最老的化石苔藓动物发现于中国特马豆克晚期。构成苔藓动物基本分类框架的狭唇纲(包括变口目、隐口目、泡孔目和管孔目)和宽唇纲(包括窗孔目和栉口目)也都是在奥陶纪时期逐步形成的,其中,变口目出现于特马豆克期Tr2时间段,在弗洛期和大坪期,多样性较低,但从达瑞威尔期开始,经桑比期至凯迪期,多样性不断增高,并出现辐射。隐口目(特别是\"双叶类隐口目苔虫\")也经历了与变口目相类似的发展过程,但它首次出现的时间要相对略迟于变口目。这两个目在整个奥陶纪苔藓动物群中一直占据主导地位。泡孔目、管孔目和窗孔目,先后首次出现在弗洛期Fl2时间段、大坪期Dp1和Dp2时间段,但它们在整个奥陶纪期间一直处于低多样性态势。至于栉口目,它首次出现的时间可能更迟,在凯迪期Ka4时间段,犹如昙花一现。苔藓动物的演化在接近奥陶纪末时呈两幕式灭绝,一次发生在凯迪期Ka2时间段(可能相当于塔凯和安斯蒂的\"拉夫塞伊灭绝\"),另一次发生在赫南特期Hi2时间段(可能相当于塔凯和安斯蒂的\"赫南特灭绝\")。分子生物学和形态学证据表明,苔藓动物属原口动物,而不是以前长期认为的后口动物,或介于原口动物和后口动物之间的过渡类型;而且,苔藓动物与腕足动物、帚形动物之间没有直接的亲缘关系。苔藓动物可能起源于一种叫原内肛动物的生物,它们的目一级分类单元之间的系统发育关系目前尚未形成共识,本文绘制的谱系图还有待于化石记录的不断补充和分子生物学研究的逐步介入以使其日趋完善。     

Investigating age‐dependency of species extinction rates using dynamic survivorship analysis

Survivorship curves with taxon lifespans normalised to variations in the real‐time extinction rate (the ‘Corrected Survivorship Score’ technique) are plotted for various fossil groups. Of five groups tested at the ‘species level’ (strictly speaking, Linnean morphospecies), only the calcareous nannoplankton are found to have had a constant extinction probability with respect to morphospecies age. The planktonic foraminifer, trilobite, conodont and graptolite data all show a significant age‐dependent effect (convexity of survivorship curves), which reveals in each case a progressively increasing extinction probability as morphospecies became older. This effect is found to be much reduced for trilobite genera and absent for ammonoid families, suggesting that age‐dependency of extinction probability is primarily a characteristic of the species level in some, but not all groups. However, the pattern may be partly an artefact of taxonomic methodology. Morphospecies range data, which are gathered primarily for biostratigraphic purposes, are far from ideal for the purpose of survivorship analysis. Therefore, survivorship curves for a specially‐developed lineage phylogeny of Palaeogene planktonic foraminifera are also presented. These do not indicate a similar age‐dependency to the extinction probability with respect to either the terminal or non‐terminal lineages.     

Early Holocene chronology and environment of Ampasambazimba,A Malagasy subfossil lemur site

According to a traditional but hitherto untested reconstruction of Madagascar’s Holocene environment, continuous forest preceded the monotonous grassland formations that now cover most of the island’s interior. Preliminary analyses of pollen samples collected near¹⁴C-dated horizons at Ampasambazimba (central Madagascar) indicate that a mosaic of woodlands, bushlands, and savanna existed close to this important vertebrate subfossil site around 7000–8000 BP. Although most members of Madagascar’s recently extinct “subfossil” fauna are thought to have been forest dwellers, several may have preferred a more open habitat like the one inferred for the region of Ampasambazimba. Dry savanna-woodland burns more readily than does dense forest and may have been more severely affected by the forces which transformed the Malagasy environment during the later Holocene. If so, the loss of savanna-woodland, not dense forest, may have been an important factor in the subfossil extinctions.