A phylogeny of Chinese species in the genus Phrynocephalus (Agamidae) inferred from mitochondrial DNA sequences

We investigated the phylogenetic relationships among most Chinese species of lizards in the genus Phrynocephalus (118 individuals, collected from 56 populations of 14 well-defined species and several unidentified specimens) using four mitochondrial gene fragments (12S rRNA, 16S rRNA, cytochrome b, and ND4-tRNA(LEU)). The partition-homogeneity tests indicated that the combined dataset was homogeneous, and maximum-parsimony (MP), neighbor-joining (NJ), maximum-likelihood (ML) and Bayesian (BI) analyses were performed on this combined dataset (49 haplotypes including outgroups for 2058 bp in total). The maximum-parsimony analysis resulted in 24 equally parsimonious trees, and their strict consensus tree shows that there are two major clades representing the Chinese Phrynocephalus species: the viviparous group (Clade A) and the oviparous group (Clade B). The trees derived from Bayesian, ML. and NJ analyses were topologically identical to the MP analysis except for the position of P. mystaceus. All analyses left the nodes for the oviparous group, the most basal clade within the oviparous group, and P. mystaceus unresolved. The phylogenies further suggest that the monophyly of the viviparous species may have resulted from vicariance, while recent dispersal may have been important in generating the pattern of variation among the oviparous species. (C) 2003 Elsevier Science (USA). All rights reserved.

Phylogenetic analyses of Fringillidae (Aves : Passeriformes) using mitochondrial tRNA gene sequences and secondary structure

Fringillidae is a large and diverse family of Passeriformes. So far, however, Fringillidae relationships deduced from morphological features and by a number of molecular approaches have remained unproven. Recently, much attention has been attracted to mitochondrial tRNA genes, whose sequence and secondary structural characteristics have shown to be useful for Acrodont Lizards and deep-branch phylogenetic studies. In order to identify useful phylogenetic markers and test Fringillidae relationships, we have sequenced three major clusters of mitochondrial tRNA genes from 15 Fringillidae, taxa. A coincident tree, with coturnix as outgroup, was obtained through Maximum-likelihood method using combined dataset of 11 mitochondrial tRNA gene sequences. The result was similar to that through Neighbor-joining but different from Maximum-parsimony methods. Phylogenetic trees constructed with stem-region sequences of 11 genes had many different topologies and lower confidence than with total sequences. On the other hand, some secondary structural characteristics may provide phylogenetic information on relatively short internal branches at under-genus level. In summary, our data indicate that mitochondrial tRNA genes can achieve high confidence on Fringillidae phylogeny at subfamily level, and stem-region sequences may be suitable only at above-family level. Secondary structural characteristics may also be useful to resolve phylogenetic relationship between different genera of Fringillidae with good performance.

沙蜥属部分物种分类性状评价

沙蜥属Phrynocephalus Kaup，1825隶属于爬行纲（Reptilia）有鳞目（Squamata）蜥蜴亚目（Lacertilia）鬣蜥科（Agamidae），是欧亚大陆荒漠和稀疏草原常见蜥蜴。沙蜥属的分类及系统演化关系、地理分布格局与新生代第三纪以来古地中海的变迁、青藏高原的抬升及亚洲内陆干旱荒漠化的过程有密切的关系，长期以来有关沙蜥属的研究一直受到中外学者们的关注。由于沙蜥属地理分布广、形态变异大、体色和斑纹变化复杂，虽然前人使用过许多形态性状来描述和分类沙蜥属物种，但是仍然存在许多问题。性状的分类学意义不明确是造成这些问题的主要原因之一，因此本研究针对沙蜥属常用的鉴别性状进行分类意义的分析，希望能对沙蜥属物种鉴定及分类学其它研究有所裨益。 中国沙蜥属物种主要分布于西北的干旱荒漠区域及青藏高原的大部分地区，大约为18种。 本文研究了中国境内12种沙蜥：青海沙蜥（Phrynocephalus vlangalii）、西藏沙蜥（P. theobaldi）、南疆沙蜥（P. forsythii）、变色沙蜥（P. versicolor）、旱地沙蜥（P. helioscopus）、荒漠沙蜥（P. przewalskii）、乌拉尔沙蜥（P. guttatus）、草原沙蜥（P. frontalis）、叶城沙蜥（P. axillaris）、白稍沙蜥（P. koslowi）、无斑沙蜥（P. immaculatus）和白条沙蜥（P. albolineatus），对它们的65项外部形态性状进行了观察和测量，其中数量性状29项、质量性状36项。评价了这些性状的序级性、间断性和代表性，结论如下： 1. 对于数量性状，得出了适合各级分类的数值区间； 2. 给出了在不同序级上适合分类的质量性状。 并利用各性状评价的结果，给出12种沙蜥的检索表，以及对中国沙蜥物种某些尚存在争议的问题进行了探讨。 详细记录了青海沙蜥红原亚种的骨骼系统，首次发现并命名了肘骨（elbow bone）和垫骨（stepping bone），为沙蜥属系统学研究补充了骨骼方面的证据；解剖了乌拉尔沙蜥、旱地沙蜥、荒漠沙蜥的雌体和雄体的骨骼系统，并在14项骨骼形态性状上对这3种沙蜥进行了比较。 Phrynocephalus （Squamata，Agamidae） is a familiar genus of lizards inhabited desert and sparse steppes in Eurasia. The taxonomics, phylogenetics and distribution pattern of Phrynocephalus are relative intensely to these events: the vicissitudes of the archaic Mediterranean sea since the Cainozoic, the uplift of Qingzang Plateau and the expending arid areas in the inland of Asia. Owing to the wide distribution, the large variability of the morphology and the different colors in Phrynocephalus, it is difficult to identify them. Tough many morphological characters are used to describe and discriminate them，a lot of questions still exist. One of the most important reasons is the confusion in the morphological characters. In this study, we demonstrate the validity and the invalidity of the familiar characters. There are about 18 species of the genus Phrynocephalus in China, which exist in arid desert in Northwest China and Qingzang Plateau. Twelve Chinese species was analyzed in this paper. They are P. vlangalii，P. theobaldi，P. forsythia，P. versicolor，P. helioscopus，P. przewalskii，P. guttatus，P. frontalis，P. axillaris，P. koslowi，P. immaculatus，P. albolineatus. We measure 29 quantitative characters and observe 36 qualitative characters in each individual. Through analyzing these characters, we made some conclusions as follows: 1. to every quantitative character, we get a clear numeric area to discriminate the different operational taxonomic units. 2. we chose the valid qualitative characters in these operational taxonomic units. This paper is the first to describe the “elbow bone”, which is a bone in pectoral appendage equivalent to patella，and “stepping bone”, which is a bone under carpal. A detailed description of the skeletal system of female Phrynocephalus vlangalii hongyuanensis was conducted. We also anatomise the skeletal systems of three species: P. guttatus，P. przewalskii，P. helioscopus, and compare or contrast 14 skeletal characters in them. What’s more，this paper offers some suggestions to the questions of Chinese Phrynocephalus species and keys to 12 species of Phrynocephalus basing on our conclusions on the evaluation of the morphological characters.

黄河上游青海沙蜥种组的系统地理学研究

沙蜥属（Phrynocephalus）的卵胎生类群主要分布在我国青藏高原，包括南疆沙蜥（P. forsythii）、西藏沙蜥（P. theobaldi）、红尾沙蜥（P. erythrurus）、贵德沙蜥（P. putjatia）和青海沙蜥（P. vlangalii）。其卵胎生生殖方式适应了高寒生境，与青藏高原隆升有关。纵观前人的研究，上述几种卵胎生沙蜥的分类、系统发育关系以及生物地理都还存在疑问。本文研究了分布在若尔盖湿地的青海沙蜥红原亚种（P. v hongyuanensis）以及分布在黄河上游其它地区青海沙蜥种组的地理分布格局，并探讨了其形成机制。 青海沙蜥在黄河上游主要分布于若尔盖湿地以及青海湖周边地区。若尔盖湿地青海沙蜥红原亚种的生境由于沼泽的形成被切割成不连续的斑块，通过遗传分析可以推测这种特殊生境对它们遗传结构的影响。其次，贵德沙蜥、青海沙蜥的青海湖周边各居群以及若尔盖湿地居群之间的系统地理格局还未见报道。因此本文以居群为单位，将它们作为一个复合体，通过系统地理研究，可以了解其种群遗传结构，据此分析相关的地质历史事件对其分布的影响。主要结果如下： 1. 若尔盖湿地青海沙蜥红原亚种的种群遗传结构： 共研究了三个地理单元（红原（HY）、辖曼（XM）、玛曲（MQ））的7个采集点的72个个体。所有ND4-tRNALeu序列比对得到785 bp的片断，定义了9种单倍型。结果显示总的核苷酸多样性较低，单倍型多样性较高。分子变异分析（AMOVA）显示3个单元间差异显著（P<0.01），遗传变异主要存在于地理单元间，占62.61%。除MQ单元，XM各居群与HY居群混杂在一起，单倍型网络图没有显示出单倍型和地理位置的对应关系。XM单元单倍型的不配对分布（Mismatch distribution）为明显左移的单峰，且Fu’s Fs test为负值，表明XM单元可能经历了近期种群扩张，有足够的时间积累单倍型的多态性，还不足以大幅提高核苷酸多样性，这是其单倍型多样性较高和核苷酸多样性较低的原因。MQ单元遗传多样性低而与其他单元显著分化，推测这与3万年前黄河在若尔盖玛曲之间贯通有关。近期沼泽的形成对XMb居群的隔离时间短，使得其遗传多样性低但还不足以形成大的遗传差异。无论黄河的贯通还是沼泽的形成其隔离形成的时间都不长，其作用改变了单倍型出现的频率，也出现了一些特有单倍型，但共享单倍型还广泛存在，还不足以使得不同居群之间形成较大的遗传距离。 2. 黄河上游青海沙蜥种组的分布格局与地史过程的关系： 黄河上游青海沙蜥种组包括贵德沙蜥、青海沙蜥指名亚种的青海湖周边各居群、青海沙蜥红原亚种若尔盖湿地居群、以及青海湖以西的部分居群（序列由Genbank下载获得），总计22个居群189个样品。所有ND4-tRNALeu序列比对得到703个位点，定义了39种单倍型。以南疆沙蜥为外群构建的贝叶斯树以及MP法构建的无根树，都分为A、B两大组。其中A包括若尔盖湿地居群以及玛多居群（A1）、青海湖以西的居群和兴海居群（A2）、西藏沙蜥；B包括青海湖以南的居群和天祝居群（B1）、青海湖以东北的居群（B2）。单倍型网络图分别对应了系统发育树上的各支。按照系统发育结果分组进行分子变异分析，得到组间变异占88.63％，各组间差异显著（P=0.000）。种群遗传结构分析得到，A1和B2可能经历了近期的种群扩张，前者扩张时间约为0.105－0.189 Ma B.P.（million years before present），后者为0.057－0.102 Ma B.P.，可能与末次间冰期的气候变暖有关。A2和B1对应的两个地理单元都具有较强的种群遗传结构，较为稳定。 青海沙蜥种组A、B两大支之间遗传距离大，分化明显，分化大约发生在4.29－2.38 Ma B.P.，推测青藏运动的A幕运动后复杂的地形变化可能是它们产生分化的原因。B1和B2分化大约发生在1.73－0.96 Ma B.P.，这与湟水流域构造运动发生的时间相符。在早、中更新世时期，B1支内部各居群可能有交流，中更新世末共和盆地出现的抬升以及河流溯源改道等事件可能是引起这支内部多个单倍型丢失的原因。A1、A2支的分化可能与倒数第三次冰期降临之后气候变冷、阿尼玛卿山的大冰帽有关。 The viviparous group of genus Phrynocephalus is mainly distributed in the Qinghai –Tibetan Plateau, including P. forsythii、P. theobaldi、P. erythrurus、P. putjatia and P. vlangalii. These species are adapted well to the cold clime there, and the origin of this group was the result of a vicariance event associated with the uplifting of the Qinghai -Tibetan Plateau. Although many works have been done, there are still several questions about classification、phylogenetic relationships and the biogeography of this group. The phylogeographic pattern of the P. vlangalii complex on the upper reaches of the Yellow River and the P. v. hongyuanensis in Zoige Wetland were studied in this thesis. On the upper reaches of the Yellow River, P. vlangalii complex are distributed in Zoige Wetland and the southeast and northeast region of Kuku-noor Lake. Because of the forming of the wetland in Zoige, the habitats for sand lizards are divided into many discontinuous ones, and it is necessary to analyze genetic structure in these unique habitats. The phylogeographic patter among P. putjatia、populations of P. vlangalii in the southeast region of Kuku-noor Lake and populations of P. vlangalii in Zoige Wetland hasn’t been studied yet, and the complicated geological events of the Plateau may play an important role in the populations’ diversity and species forming there. So these populations were gathered as a complex, and phylogeographic analysis were used to clarify these doubts. According to the two topics above, this thesis has two parts of results as follows: 1. Three geographic units of P. vlangalii hongyuanensis in Zoige Wetland were defined, and they were Xiaman （XM）、Hongyuan （HY） and Maqu （MQ）. 785bp fragments of the mtDNA ND4-tRNAleu were determined from 72 samples and nine haplotypes were identified. As a whole, the nucleotide diversity was low，but the haplotype diversity was high. Analysis of molecular variance （AMOVA） showed that the three units were distinctly different（P<0.01），and 62.61% of the total genetic diversity was attributable to variation among units. There were 3 haplotypes shared among XM and HY，and no geographic clustering was observed except MQ from the TCS network. The results from the mismatch distribution analysis and Fu’s Fs test implied that there might be a recent population expansion in the XM unit, and this may be the reason why XM had a high haplotype diversity but a low nucleotide diversity. We estimate that the MQ and XMb have lower diversities because of some very recent geographic events, such as the formation of the Yellow river’s upriver and the Zoige Wetland. Although they are distinctly different, not enough time has passed for them to have diverged a great genetic distance. 2. 189 samples in 22 populations of P. vlangalii complex were collected, including P. putjatia、populations of P. vlangalii in the southeast and northeast region of Kuku-noor Lake、 populations of P. vlangalii in Zoige Wetland and the data from Genbank. 703bp ND4-tRNALeu sequences identified 39 haplotypes. P. forsythii was selected as outgroup, and both the Bayesian tree and the MP unrooted tree were divided into two groups（A、B）. A included populations in Zoige Wetland and Xinghai（A1）、populations in the west of Kuku-noor Lake（A2）、P. theobaldi, and B included populations in the southeast of Kuku-noor Lake and Tianzhu（B1）、populations in the northeast of Kuku-noor Lake（B2）. The haplotype network agreed with these groups. AMOVA showed that these five groups were distinctly different（P<0.01）, and 88.63% of the total genetic diversity was attributable to variation among groups. There might be recent population expansion in A1 and A2, which corresponded to the dry climate of the last interglacial period. The expansion times were 0.189-0.105 Ma B.P. and 0.102-0.057 Ma B.P., respectively. A2 and B1 had strong genetic structure. The large genetic distance between A and B showed that they had been separated from each other for a long time（about 4.29-2.38 Ma B.P.）, and it corresponded to the A phase of Qingzang Movement. The diversity between B1 and B2 at 1.73-0.96 Ma B.P. may be caused by the geological event in Huangshui valley. In early Pleistocene, populations in B1 may have gene flow because of geographic linkage, and later the uplift of the Plateau and the change of river route there made a few haplotypes lost. A1 and A2 were divided into two parts by A’nyemaqen Mountains at 0.66-0.37 Ma B.P., which maybe corresponded to glaciations at about 0.7 Ma B.P.