外生菌根真菌生物地理学研究进展

外生菌根真菌对植物矿质营养、生态系统物质循环、物种演化进程等具有十分重要的作用,但其生物地理学研究长期滞后于动植物。扩散和隔离是解释外生菌根真菌生物地理分布格局的重要理论。古地质、古气候和宿主植物是外生菌根真菌地理分布格局形成的重要推动因子。基因组学、生物信息学技术与生物地理学方法相互结合和补充,可以用来研究一些复杂的真菌生物地理学问题。文中详细阐述了外生菌根真菌生物地理学研究的重要过程和现状,如真菌物种界定、常用数据分析方法、起源和演化规律及其在生物多样性保护方面的应用等,并初步探讨了其未来的发展方向。     

土壤微生物生物地理学研究进展

生物地理学是研究生物（包括种群、群落等不同层次）地理分布格局及成因的一门交叉学科。微生物生物地理学的研究长期滞后于宏生物地理学。鉴于土壤微生物在调控生物地球化学过程和维持生态系统功能方面的重要作用,对其空间分布格局及形成机制的认识具有十分重要的理论和实际意义。随着分子生物学技术的发展,对微生物多样性的认知日益深入。越来越多的证据表明,土壤微生物群落结构和多样性具有一定的时空分布格局,从而对微生物全球性随机分布的传统观点提出了挑战。对当前土壤微生物生物地理学研究中的一些概念性问题,如微生物物种的定义、微生物多样性的定量测度、对微生物全球性随机分布的争论等,进行了系统评述;以微生物种-面积关系和距离-衰减关系为例对当前最新的土壤微生物生物地理学研究成果进行总结,并初步探讨了土壤微生物群落的地带性分布问题;在传统生物地理学理论的指导下,提出了一个可用于验证土壤微生物空间分布格局形成和机制维持的简单研究框架。这些对今后土壤微生物生物地理学的研究有一定借鉴和指导意义。     

鸟类分子系统地理学研究进展

分子系统地理学是当代生物地理学的重要分支,是以分子生物学方法重建种内和种上水平的系统发育关系,阐释进化历史,并通过分析近缘生物类群的系统发育关系与其空间和时间分布格局间的相关性构建生物区系历史的研究,是分子生物学与生物地理学结合的产物。中性进化学说和溯祖理论分析的建立,以及线粒体DNA和微卫星标记等分子遗传标记的应用,为分子系统地理学研究的开展提供了理论和实践基础。近年来,分子系统地理方法在鸟类学研究中的应用揭示了许多不同于传统认知的发现,为准确而深入的了解鸟类分子系统地理格局的差异和不同类群的起源中心提供了新颖的证据。目前的研究多从隔离分化说和扩散说的角度对鸟类分子系统地理格局的成因进行分析,而迁徙行为不同对鸟类系统地理格局的影响为成因的解释提供了新的角度。结合区域特点的比较分子系统地理研究,在更广泛的地域和更多类群中开展研究是我国鸟类分子系统地理研究的方向。此外,展望了第二代测序技术对分子生态生物地理研究具有的潜在促进作用。     

历史生物地理学的进展

近年来历史生物地理学的进展主要是隔离分化学派的进展。对隔离分化学派的几个分支学派,特别是分支生物地理学和泛生物地理学在理论和方法方面的进展作了简要回顾和介绍。最近十年来分子手段广泛应用于历史生物地理学研究的各个方面,尤其是谱系生物地理学的快速崛起是历史生物地理学的一个明显特征。对本学科的发展做了初步的展望。     

东南亚生物多样性热点地区的形成与演化

东南亚地处热带,生物多样性极为丰富,可分为4个热点地区:印度-缅甸区的中南半岛、巽他区(含马来半岛、婆罗洲、苏门答腊岛)、菲律宾区(菲律宾群岛)、华莱士区(苏拉威西岛、爪哇岛、马鲁古群岛、小巽他群岛等)。中南半岛在泥盆纪便已是欧亚大陆的一部分,在印度板块撞击欧亚大陆之后受挤压而出;巽他区来自于冈瓦纳古陆和澳洲古陆;菲律宾群岛部分来自于劳亚古陆的碎片向南漂移,部分来自于太平洋西南岛弧的向北迁移;华莱士区则是劳亚古陆碎片、太平洋西南岛弧以及澳洲古陆北侧碎片的组合。巽他区地处赤道,常年温湿;菲律宾区、华莱士区、中南半岛则都受到不同程度的季风气候决定的干湿季变动。地质历史和季风气候影响程度的不同,奠定了东南亚4个生物多样性热点地区的雏形。华莱士区保存有大量的早期被子植物原始类群如睡莲目(Nymphaeales)和木兰藤目(Austrobaileyales),是现代被子植物起源地和冰期避难所之一。巽他区(婆罗洲)和中南半岛是亚洲热带植物的现代分布中心和"进化前沿",是整个东南亚地区重要的种源;而华莱士区的爪哇岛和小巽他群岛主要是物种迁入和中转的种库。这样的物种形成历史与迁移格局,塑造了东南亚4个生物多样性热点地区物种多样性水平与地理范围的基本格局。巽他区和印度-缅甸区曾在冰期通过陆桥相连,使得东南亚成为周边植物扩散交汇的一个"十字路口"。但是,人们对东南亚生物多样性热点地区的物种长距离扩散规律及植物地理学分区仍存在分歧;东南亚与邻近生物多样性热点地区如新几内亚岛、西高止山脉-斯里兰卡、中国横断山区的历史联系,还尚待深入解析。利用现代分子生物学技术,覆盖整个东南亚地区进行全域取样开展代表性类群的物种迁移与生物地理学研究,有望进一步揭示东南亚生物多样性热点地区的形成过程与演化趋势。     

中国鸟类生物地理学研究回顾与展望

本文回顾总结了中国鸟类生物地理学的产生、发展、重要成果和未来的发展趋势。主要论述了以下五个方面:1.中国动物地理学简史及鸟类生物地理学的萌芽;2.鸟类动物地理区划的发展,并重点论述了岛屿鸟类区系调查与生物地理格局、中国台湾岛和海南岛与大陆鸟类区系的联系以及鸟类特有化现象;3.鸟类多样性的格局、形成与维持,并重点归纳了几种重要的科学假说;4.鸟类的谱系生物地理格局、形成原因及影响因素;5.鸟类生物地理学研究的新进展和未来发展趋势,重点阐述谱系生物地理学的发展、"地理格局-适应-基因"的整合分析方法对中国鸟类多样性格局形成机制的深度解析,指出大数据和组学时代是中国乃至世界鸟类生物地理学的发展趋势。     

内蒙古苏崩地点的古新世软食中兽(哺乳纲,中兽目):古新世-始新世界线附近“东方伊甸园”扩散模式的新证据(英文)

记述了发现于内蒙古苏崩晚古新世格沙头期的中兽类软食中兽Hapalodectes属的一个新种。这是软食中兽在中国古新世地层中的首次发现,也是亚洲格沙头期的第二种软食中兽。已有的系统学和生物地层学证据支持软食中兽属和软食中兽科(Hapalodectidae)亚洲起源的观点。软食中兽显然是在古新世-始新世极热事件(PETM)期间通过白令陆桥扩散到北美大陆的,因而符合"东方伊甸园"学说中的生物地理格局。软食中兽有限的(即非欧洲的)地理分布使得我们可以重建该属生物地理学历史。如同软食中兽一样的"东方伊甸园"式的扩散模式,可以看作是大的环境变化事件导致多个支系产生相似的系统学和生物地理学分布格局的生物地理扩散机制。严格地检查了所谓的在古新世-始新世界线上或其附近的与"东方伊甸园"模式相矛盾的大陆间哺乳动物扩散事例,结果发现这些例子都是不可靠的。"东方伊甸园"生物地理学说充分解释了PETM时期哺乳动物群更替以及劳亚古陆哺乳动物地理分布格局的成因。     

历史生物地理学中的BPA分析法Ⅱ :二级BPA

BPA(broks parsimony analysis)是历史生物地理学研究的重要分析方法之一,包括初级BPA和二级BPA。前者主要用于寻找共同格局,后者是对网状进化格局的解释。本文详细介绍了二级BPA的分析方法,并就BPA与其它历史生物地理学／支序学派的研究方法进行了区别。     

植物功能生物地理学的研究进展与展望

功能生物地理学研究性状及其多样性的时空分布变化、生态成因及其对生态系统功能的影响。近十来年,功能生物地理学领域发展迅速,性状数据呈指数增长,基于性状探索物种分布、群落结构和组成以及生态系统功能对环境变化响应的研究取得了重要进展。该文综述了植物功能生物地理学的核心内涵、发展历史、主要研究进展和未来展望。性状是功能生物地理学的研究核心,该文先总结了植物叶、茎、根、花、果实和种子等器官和整株关键性状的地理格局及其与环境间的关系,表明性状变异是植物适应进化和环境筛选的结果;概述了功能多样性的常用指标、地理分布与生态成因;介绍了性状数据的主要来源与性状缺失值的填充方法。随后,综述了植物性状间的关联与权衡,重点介绍了叶经济谱和植物经济谱的发展,指出其反映了植物对关键资源(如碳、养分和水分)的获取与分配策略;概述了基于性状预测物种分布的依据与进展,以及性状多样性与生态系统功能间的关系。在此基础上,提出了功能生物地理学研究所面临的挑战,强调未来研究要关注多性状在种内和种间的协同与权衡关系,将研究精度从物种水平推进到个体水平,采用性状网络等方法定量化性状间的关系及其对环境变化的响应,关注植物跨尺度的适应...     

大数据时代土壤微生物地理学研究综述

土壤蕴含极为丰富的微生物多样性,它们在物质分解、元素生物地球化学循环、植物生产力和生物健康中扮演着关键角色。理解土壤微生物的生物地理分布格局、形成机制与群落构建规则,有助于预测在全球变化背景下土壤微生物组的功能演变及其对陆地生态系统的调控影响。自21世纪以来,土壤微生物生物地理学在各种大型国际微生物计划的推动下逐步形成了分子生物学技术耦合大数据分析的模式,实现了多种尺度上的关联研究。阐述了土壤微生物在分布格局和群落构建规则方面的研究进展,重点介绍了分子生物学技术和大数据分析在土壤微生物生物地理研究中的应用,对土壤微生物生物地理学未来在微生物分类分辨率、模型验证与构建和功能基因地理学的发展方向进行了展望。     

Gondwanan break-up: legacies of a lost world?

Fierce debate surrounds the history of organisms in the southern hemisphere; did Gondwanan break-up produce ocean barriers that imposed distribution patterns on phylogenies (vicariance)? Or have organisms modified their distributions through trans-oceanic dispersal? Recent advances in biogeographical theory suggest that the current focus on vicariance versus dispersal is too narrow because it ignores 'geodispersal' (i.e. expansion of species into areas when geographical barriers disappear), extinction and sampling errors. Geodispersal produces multiple, conflicting vicariance patterns, and extinction and sampling errors destroy vicariance patterns. This perspective suggests that it is more difficult to detect vicariance than trans-oceanic dispersal and that specialized methods must be applied if an unbiased understanding of southern hemisphere biogeography is to be achieved.     

Historical and Ecological Factors in the Evolution, Adaptive Radiation, and Biogeography of Freshwater Mollusks

SYNOPSIS. There are some 36 families that are wholly freshwateror with representative species in freshwater. There are virtuallyno phylogenetic analyses for these families. Zoogeographic analysesof freshwater molluscan faunas are hindered by a lack of significantsystematic studies of these faunas. Such studies are essentialif one hopes to develop hypotheses about phylogeny or biogeography. It is clear from a phylogenetic analysis of the Pomatiopsidaethat phylogenetic, vicariance, dispersal, and ecological factorsall have significant effects on the patterns of distributionof this family. At one stage in history vicariance may be adominant factor while during another stage of history, dispersalmay be a dominant factor. At every stage, ecological considerationsare necessary to understand the phenotypes seen and the spatialrelationships among taxa. In examining the distribution patternsof dominant freshwater families with regard to their biological,ecological, and overall phylogenetic relationships it is evidentthat ecology plays a major role along with dispersal and vicariance.Clearly a synthesis is needed in biogeographical studies thatincorporates vicariance dispersal, ecology, and geology-paleontology.     

Palaeobiogeography of the North Pacific toothed mysticetes (Cetacea,Aetiocetidae): a key to Oligocene cetacean distributional patterns

Biogeographical distributional patterns of cetaceans reflect dispersal events and colonization of the oceans from their ancestral area in the ancient Sea of Tethys ~53 Ma. Likewise, they reveal several vicariance events throughout the evolutionary history of this group. However, our understanding of how these processes took place and what biogeographical scenarios occurred among the different groups of cetaceans through time is limited. Consequently, this work focuses on explaining the distributional patterns of the well‐known North Pacific toothed mysticetes, Aetiocetidae, through the power of retrodiction offered by track analysis (panbiogeography) and cladistic biogeography, using the approach of evolutionary biogeography. Our results show that the distributional patterns of Aetiocetidae explain their endemism in the North Pacific, as well as indicating that their hypothetical ancestor probably colonized the Pacific from the Atlantic Ocean by a dispersal event (founder effect) via the Central American Seaway. Furthermore, their biogeographical history shows that the adaptive radiation (cladogenesis) of Aetiocetidae is result of peripatric speciation followed by sympatric speciation within a heterogeneous environment. Finally, the biogeographical framework of Aetiocetidae further supports the relevant role that the Pacific Ocean has played in the evolution of Oligocene cetaceans as a geographical area that promoted endemism, dispersal and colonization. At more local scales, environmental conditions further promoted increased diversity and disparity amongst Mysticeti.     

Out-of-Africa origin and dispersal-mediated diversification of the butterfly genus Junonia (Nymphalidae: Nymphalinae)

The relative importance of dispersal and vicariance in the diversification of taxa has been much debated. Within butterflies, a few studies published so far have demonstrated vicariant patterns at the global level. We studied the historical biogeography of the genus Junonia (Nymphalidae: Nymphalinae) at the intercontinental level based on a molecular phylogeny. The genus is distributed over all major biogeographical regions of the world except the Palaearctic. We found dispersal to be the dominant process in the diversification of the genus. The genus originated and started diversifying in Africa about 20 Ma and soon after dispersed into Asia possibly through the Arabian Peninsula. From Asia, there were dispersals into Africa and Australasia, all around 5 Ma. The origin of the New World species is ambiguous; the ancestral may have dispersed from Asia via the Beringian Strait or from Africa over the Atlantic, about 3 Ma. We found no evidence for vicariance at the intercontinental scale. We argue that dispersal is as important as vicariance, if not more, in the global diversification of butterflies.     

Biogeography of rotifers

The biogeography of rotifers is discussed in light of general biogeographical concepts. It is argued that, in spite of considerable abilities for passive dispersal, vicariance can develop well in this group. Examples selected from the Branchionidae illustrate the high levels of endemicity found in Australia and South America, while the Indian subcontinent and Africa have a predominantly cosmopolitan fauna. An explanation for these patterns is found in drifting continents and Pleistocene climatic changes.     

历史生物地理学进展

生物地理学研究动植物的地理分布。历史生物地理学重建生物区系历史。分替理论的复兴动摇了散布理论的上百年统治。最近10年主要是分替理论推动了历史生物地理学,出现了多个途径——种系发生物地理学、分支分替生物地理学、特有性的俭吝分析和泛生物地理学。岛屿生物地理学理论有了改进和严格的实验检验;庇所学说产生了新的模型。最后就我国如何发展生物地理学提出了对策措施。     

Quantitative palaeobiogeography: GIS, phylogenetic biogeographical analysis, and conservation insights

Aim  The utility of GIS-based and phylogenetic biogeographical analysis in palaeobiogeography is reviewed with reference to its ability to elucidate patterns of interest for modern conservation biology, specifically the long-term effects of invasive species.
Location  Emphasis is on biogeographical patterns in the Appalachian basin and mid-continent of North America during the Devonian. Global palaeobiogeographical patterns of the Cambrian are also considered.
Methods  Palaeobiogeographical patterns are assessed within a GIS framework, including both direct range reconstruction and niche modelling methods, and within phylogenetic biogeographical analysis. Biogeographical patterns are considered within multiple clades of fossil invertebrates, including trilobites, crustaceans, brachiopods, and bivalves.
Results  GIS-based analysis (including niche modelling methods) of Devonian invertebrates demonstrates a tightly correlated relationship between sea-level rises and range expansion, dispersal events, and species invasions. The predominance of range expansion and species invasions during the Late Devonian reduced opportunities for vicariant speciation during this interval. Comparison of phylogenetic biogeographical patterns between Cambrian and Devonian trilobites allows discernment of the relative roles of tectonics and eustacy in driving biogeographical patterns.
Main conclusions  GIS analysis and phylogenetic biogeography are powerful tools for analysing the coevolution of the Earth and its biota. Analyses can identify episodes of vicariance and geo-dispersal and produce testable hypotheses for further analysis within the fossil record.     

When phylogenetics met biogeography: Willi Hennig,Lars Brundin and the roots of phylogenetic and cladistic biogeography

Willi Hennig's (Beitr. Ent. 1960, 10, 15) Die Dipteren-Fauna von Neuseeland als systematisches und tiergeographisches Problem applied a phylogenetic approach to examine the distributional patterns exhibited by the Diptera of New Zealand. Hennig showed how phylogenetic trees may be used to infer dispersal, based on the progression and deviation rules, and also discussed the existence of vicariance patterns. The most important author who applied Hennig's phylogenetic biogeography was Lars Brundin, when analysing the phylogenetic relationships of two taxa of Chironomidae (Diptera) and using them to examine the biogeographic relationships of Australia, New Zealand, South America and South Africa. The relevance of Brundin's contribution was noted by several authors, as it began the cladistic or vicariance approach to biogeography, that implies the discovery of vicariance events shared by different monophyletic groups. Both phylogenetic and cladistic biogeography have a place in contemporary biogeography, the former for analysing taxon biogeography and the latter when addressing Earth or biota biogeography. The recent use of the term “phylogenetic biogeography” to refer to a posteriori methods of cladistic biogeography is erroneous and should be avoided.     

Critique of parsimony analysis of endemicity as a method of historical biogeography

Aim Assess the value of parsimony analysis of endemism as either an a priori (cladistic) and an a posteriori (phylogenetic) method of historical biogeography. Location World‐wide. Methods Parsimony analysis of endemicity (PAE) and Brooks parsimony analysis (BPA). Results Parsimony analysis of endemicity is capable of finding correct and unambiguous area relationships only under scenarios of vicariance in combination with non‐response to vicariance or extinction. An empirical comparison between PAE and BPA, using the poeciliid fish genera Heterandria and Xiphophorus, demonstrates that PAE fails to document much of the historical complexity in this relatively simple system. Main conclusions The a priori assumptions of PAE are far more restrictive than those made by other a priori methods, limiting its utility as a method of cladistic biogeography. The inability of PAE to detect perfect vicariance or biogeographical histories involving dispersal, renders it unsuitable as a method of phylogenetic biogeography.     

The resurrection of oceanic dispersal in historical biogeography

Geographical distributions of terrestrial or freshwater taxa that are broken up by oceans can be explained by either oceanic dispersal or vicariance in the form of fragmentation of a previously contiguous landmass. The validation of plate-tectonics theory provided a global vicariance mechanism and, along with cladistic arguments for the primacy of vicariance, helped create a view of oceanic dispersal as a rare phenomenon and an explanation of last resort. Here, I describe recent work that suggests that the importance of oceanic dispersal has been strongly underestimated. In particular, molecular dating of lineage divergences favors oceanic dispersal over tectonic vicariance as an explanation for disjunct distributions in a wide variety of taxa, from frogs to beetles to baobab trees. Other evidence, such as substantial gene flow among island populations of Anolis lizards, also indicates unexpectedly high frequencies of oceanic dispersal. The resurrection of oceanic dispersal is the most striking aspect of a major shift in historical biogeography toward a more even balance between vicariance and dispersal explanations. This new view implies that biotas are more dynamic and have more recent origins than had been thought previously. A high frequency of dispersal also suggests that a fundamental methodological assumption of many biogeographical studies--that vicariance is a priori a more probable explanation than dispersal--needs to be re-evaluated and perhaps discarded.