Geographical distribution patterns of Metaeuchromius in Asia and description of a new species from China (Lepidoptera,Crambidae)

The geographical distribution patterns of Asian Metaeuchromius are analysed with MaxEnt and ArcGIS based on known localities and nineteen environmental variables. The results suggest that the most highly suitable area of the genus located in southeastern China. Precipitation of the warmest quarter (Bio18) and temperature seasonality (Bio4) are the most significant variables affecting geographical distribution Metaeuchromius. Furthermore, a new species from Jiangxi Province, southeast China is added to the genus, Metaeuchromius grandispinata Li, sp. nov. Its habitus, tympanic organs and genitalia are illustrated, and two maps showing geographical distribution patterns of Metaeuchromius in Asia are provided.     

Early Cambrian organophosphatic brachiopods from the Xinji Formation,at Shuiyu section,Shanxi Province,North China

Abundant and diverse small shelly fossils have been reported from Cambrian Series 2 in North China, but the co-occurring brachiopods are still poorly known. Herein, we describe seven genera, five species and two undetermined species of organophosphatic brachiopods including one new genus and new species from the lower Cambrian Xinji Formation at Shuiyu section, located on the southern margin of North China Platform. The brachiopod assemblage comprises one mickwitziid (stem group brachiopoda), Paramickwitzia boreussinaensis n. gen. n. sp., a paterinide, Askepasma toddense Laurie, 1986, an acrotretoid, Eohadrotreta cf. zhenbaensis Li and Holmer, 2004, a botsfordiid, Schizopholis yorkensis (Holmer and Ushatinskaya in Gravestock et al., 2001) and three linguloids, Spinobolus sp., Eodicellomus cf. elkaniiformis Holmer and Ushatinskaya in Gravestock et al., 2001 and Eoobolus sp. This brachiopod assemblage suggests a late Age 3 to early Age 4 for the Xinji Formation and reveals a remarkably strong connection with coeval faunas from East Gondwana, particularly the Hawker Group in South Australia. The high degree of similarity (even at species level) further supports a close palaeogeographic position between the North China Platform and Australian East Gondwana during the early Cambrian as indicated by small shelly fossil data.     

Stromatolite-dominated microbialites at the Permian–Triassic boundary of the Xikou section on South Qinling Block,China

Permian–Triassic boundary microbialites (PTBMs) are organosedimentary carbonates formed immediately after the end-Permian mass extinction. All those reported PTBMs constrained by convincing conodont biozones are present stratigraphycally not higher than the Hindeodus parvus zone and most of them are dominated by thrombolites. This paper provides the first record of a brief, but spectacular development of stromatolite-dominated PTBMs within the basal Isarcicella isarcica conodont zone of the earliest Triassic from the Xikou section of South Qinling Block that was at the margin of the North China Block during the Permian–Triassic transition and was geographically separated from the major occurrence of post-extinction microbialites in the South China Block. This stromatolite cap overlies a 3.7-m-thick oolitic limestone and is composed of a lower 0.2-m-thick bed and an upper 0.5-m-thick bed, separated by a 0.2-m-thick greyish green siliciclastic mudstone. These two stromatolite beds mainly consist of columnar stromatolites with subordinate domal stromatolites. The intercolumn and interstitial spaces within the stromatolites are filled with oolitic grainstones. At the microscopic scale, laminoid structures in stromatolites comprise wavy, millimetric-domical and tangled laminae. The increased grain and fossil contents and/or bioturbation in the domical and tangled laminae indicate that the formation of these laminae is likely related to an increase in the populations and the disruptions by benthic metazoans, as well as an influx of sediment grains. The δ¹³C_carb values fluctuate between 2‰ and 3‰ in the uppermost Permian strata; a distinct negative shift of 1.9‰ occurs at the topmost oolitic grainstone, just below the lower stromatolite bed, and the lowest value of −0.1‰ is located at the base of the upper stromatolite bed. The stratigraphic succession from stromatolites to thrombolites of the PTBMs may represent a transgressive succession and/or a transient ecosystem recovery immediately after the end-Permian mass extinction. The thrombolites-dominated PTBMs mainly developed in near-equator shallow marine geographic locations, and stromatolite-dominated PTBMs mainly developed at higher latitude settings, which probably indicates that a relatively lower diversity and abundance of marine benthic metazoans existed at higher latitudes after the end-Permian mass extinction.     

古DNA捕获新技术与中国南方早期人群遗传研究新格局

古DNA捕获技术目前已获得极大的发展,能够从骨骼和环境沉积物等多种材料中获取到目的DNA片段,而且对于保存环境较差的低纬度地区,同样能够获取有效的内源DNA片段,极大地丰富了古DNA研究的材料来源。本文围绕这一新技术开展总结和讨论,主要分为两个方面：1）总结并介绍该技术应用前景;2）应用这一技术打开了中国南方早期人群研究的新局面,梳理该新技术的应用对史前中国南方人群古基因组研究所获得的新认识,并对中国南方早期人群古基因组深入分析;另外,利用古DNA捕获技术成功获取云南3446~3180 BP的大阴洞遗址4例高质量线粒体基因组信息,并开展了人群遗传历史的研究。     

中国苦苣苔科植物新资料——小花线柱苣苔

该文报道了产自中国西藏自治区墨脱县境内的线柱苣苔属(Rhynchotechum Blume)中国分布新记录——小花线柱苣苔(R. parviflorum Blume)。该新记录种常生长在林中溪流附近的崖壁以及次生林下阴湿生境中,主要辨别特征为叶基本对生,花萼裂片被绢毛,花梗被黄褐色绒毛,花冠筒较小,子房具短柔毛,果无毛至微柔毛。印度学者于2020年记载为印度新分布,而原始文献中记录的凭证标本采集点位于中国西藏自治区墨脱县境内,故对原文记述的产地信息提出质疑。同时,在前人的研究中部分馆藏的线柱苣苔属植物标本被认定为该新记录种,在此一并提出该新记录种在中国的分布地理信息和详细描述。     

中国造礁石珊瑚分类厘定

造礁石珊瑚是珊瑚礁框架建造者, 具有维持珊瑚礁生态系统功能和稳定性的重要作用, 其分类对于造礁石珊瑚和珊瑚礁的研究与保护至关重要。目前, 随着分子系统学的不断发展, 造礁石珊瑚的分类体系发生改变, 伴随着出现大量同物异名。近年来也出现许多无中文学名的中国造礁石珊瑚新记录种, 这些都给物种认定和命名带来困难, 阻碍了中国造礁石珊瑚的研究与保护工作。为此, 本文收集了中国造礁石珊瑚物种记录文献资料, 采用最新的造礁石珊瑚分类体系, 确认同物异名, 形成中国造礁石珊瑚物种名录, 并对中国造礁石珊瑚物种的中文名进行统一的规范和命名。结果表明, 中国共有造礁石珊瑚2个类群16科77属445种。与《中国动物志·腔肠动物门·珊瑚虫纲·石珊瑚目·造礁石珊瑚》相比, 科级分类阶元新增7个科, 变更5个科; 属级分类阶元新增26属, 变更1属, 合并3属; 种级分类阶元新增291种, 变更13种, 合并20种, 新命名305个物种的中文名。并且筛选出187个同物异名。此外, 由于造礁石珊瑚分类体系现仍有部分争议, 文章也进行了讨论说明。     

中国地衣的濒危等级评估

地衣是大型真菌的重要组成部分, 是中国大型真菌红色名录评估的主要对象之一。本次评估的地衣共2,164种, 其中子囊菌地衣2,145种, 担子菌地衣19种, 分属于2门9纲34目92科352属。评估结果显示, 地衣受威胁物种共28种, 占被评估地衣物种总数的1.29%, 其中极危3种, 濒危7种, 易危18种; 近危6种, 无危657种, 而数据不足的物种达1,473种。这类因为缺乏足够的数据资料而未能进一步评估其生存状态和红色名录等级的物种占评估地衣总数的68.07%, 凸显了我国地衣学研究的严峻形势及对地衣分类学人才的迫切需要。对受威胁物种的分析表明, 地衣由于自身生长缓慢和对环境污染敏感, 并且绝大多数分布区域狭窄, 种群数量少, 对生境退化的适应和恢复生长的能力弱, 人类活动和气候变化导致的栖息地破坏和碎片化使得这些地衣的生存受到严重威胁。值得注意的是, 评为易危的一些地衣, 因具有较大的食药用价值而被过度采挖利用, 如不采取有效保护措施, 其受威胁程度将进一步加剧。     

长毛孜然芹,中国伞形科一新记录种

报道了中国伞形科（Apiaceae）孜然芹属一新记录种：长毛孜然芹[Cuminum borszczowii（Regel et Schmalh.）Koso-Pol.]。该物种在形态上与孜然芹（C.cyminum）相近,与后者的区别在于总苞宽披针形具较宽的膜质边缘,不反折,比伞辐短;果实密被长毛。提供了该种详细的形态学描述及图版。凭证标本保存在新疆农业大学标本馆（XJA）和中国科学院新疆生态与地理研究所标本馆（XJBI）。     

中越带唇兰, 中国带唇兰属(兰科)一新记录

报道了中国兰科（Orchidaceae）植物一新记录种：中越带唇兰（Tainia acuminata Averyanov）,并提供形态描述及彩色图片。该种与心叶带唇兰（T.cordifolia Hook.f.）相近,不同在于萼片与花瓣均为狭披针形,唇瓣无侧裂片,阔披针形,渐尖,唇瓣边缘在中上部波状卷曲,唇盘具3条不明显的脊。     

Genetic diversity and population structure of Quercus fabri Hance in China revealed by genotyping‐by‐sequencing

Analysis of genetic diversity and population structure among Quercus fabri populations is essential for the conservation and utilization of Q. fabri resources. Here, the genetic diversity and structure of 158 individuals from 13 natural populations of Quercus fabri in China were analyzed using genotyping‐by‐sequencing (GBS). A total of 459,564 high‐quality single nucleotide polymorphisms (SNPs) were obtained after filtration for subsequent analysis. Genetic structure analysis revealed that these individuals can be clustered into two groups and the structure can be explained mainly by the geographic barrier, showed gene introgression from coastal to inland areas and high mountains could significantly hinder the mutual introgression of genes. Genetic diversity analysis indicated that the individual differences within groups are greater than the differences between the two groups. These results will help us better understand the genetic backgrounds of Q. fabri.