The role of extreme events in evolution

Evolutionists have often had a marked tendency to think that, in the course of time, planetary events were not very different from those occurring during a human life. However, when a ‘non-human’ timescale is used, the history of our planet appears profoundly and frequently disturbed by extreme events. These events, even not always instantaneous, impose – because of their amplitude – a severe sorting, not between individuals of a species, but between species, or even between phyla. In the face of an extreme event, intraspecific diversity counts little: it is the interspecific diversity that makes the difference. As shown by mass extinctions, extreme events open ecological niches and redistribute the cards of life, giving survivors opportunities to radiate. The capacity to cope with extreme ecological conditions favours certain species in ecosystems, not certain individuals in populations. This is not a macroevolutionary process in terms of acquiring new adaptations, but a macroevolutionary process in terms of sorting entire sections of life. The most important is perhaps that the current ‘mediatisation’ of a limited number of mass extinctions dissimulates less important extinctions caused by less extreme and more localized events that were possibly responsible for many changes in the composition and structure of communities throughout the evolution. The term of ‘pre-adaptation’ has been neglected, because it gives an impression of finalism, but it expresses well that, when an unexpected event occurs, a particular species has or has not the ‘right genes’ to continue to sustain viable populations. The role of extreme events in modifying the course of evolution should not be underestimated.     

Beringia as an Ice Age genetic museum

Thousands of Late Pleistocene remains are found in sites throughout Beringia. These specimens comprise an Ice Age genetic museum, and the DNA contained within them provide a means to observe evolutionary processes within populations over geologically significant time scales. Phylogenetic analyses can identify the taxonomic positions of extinct species and provide estimates of speciation dates. Geographic and temporal divisions apparent in the genetic data can be related to ecological change, human impacts, and possible landscape mosaics in Beringia. The application of ancient DNA techniques to traditional paleontological studies provides a new perspective to long-standing questions regarding the paleoenvironment and diversity of Late Pleistocene Beringia.     

Policy mobilities,territorial knowledge dynamics and the role of KIBS: Exploring conceptual synergies of formerly discrete approaches

Although contemporary policy making is substantially affected by consultants, little is known about the interconnection of their role inside policy making networks and their key product – knowledge. This paper matches the approaches on Policy Mobilities (PM) and Territorial Knowledge Dynamics (TKD) to fill this theoretical gap. By exploring the synergies of both concepts, a research agenda is suggested that enables to investigate the multi-facetted entanglements of knowledge and policy making dynamics as well as what stake consultants have in this complex assemblage. Accordingly, this paper claims appreciation of ‘variegated consultocracies’ rather than global homogeneity of consultants’ engagement in policy making processes by explicating better integration of ‘scale, ‘time’, and actors’ embeddedness into PM. The paper thus primarily aims to provide a solid theoretical and methodological basis for exploring the complex dynamics consultants take part in, and how they in turn impact policy making processes.     

Shark and ray faunas in the Middle and Late Eocene of the Fayum Area, Egypt

The Eocene rocks exposed in the Fayum Area, Egypt, are well known for their fossil vertebrates but in recent times the sharks and rays have been largely neglected. Extensive surface collecting, supplemented with bulk samples, has produced large collections from the Midawara, Gehannam, Birket Qarun and Qasr el-Sagha formations, spanning the Bartonian and Priabonian stages and from palaeoenvironments varying from open muddy shelf to very shallow estuarine systems. In total about 90 species of sharks and rays are recorded, many of them previously unrecognised, resulting in some of the most diverse fossil chondrichthyan assemblages known from the Tertiary. Teeth of these species suggest that they occupied a wide range of ecological niches from top predator to tiny benthic invertebrate feeder to planktivore. Many of the species are limited in their stratigraphical range and show potential to be used, at least locally, as biostratigraphical indicators for stratigraphically poorly constrained vertebrate sites elsewhere in North Africa. Distinctly different faunas from different sedimentary environments indicate a strong environmental control on the distribution of many species.     

The evolution of the electronics industry in Johor (Malaysia): Strategic coupling,adaptiveness, adaptation,and the role of agency

Bringing together concepts from the global production networks and evolutionary economic geography literature, this article empirically examines the trajectory of the electrical and electronics industry in Johor (Malaysia). Based on trends in firm entries and exit as well as interviews with companies, we find limited robustness in the industry’s trajectory. While there is evidence of the role of ‘structure’ in this outcome, we argue that human agency – particularly the actions of subnational policy-makers – is key. This is manifest in a preference for fostering regional ‘adaptiveness’ through the often uncritical promotion of a diversity of economic sectors. This compromises the meaningful pursuit of regional ‘adaptation’ in the form of new and more complex branches emerging from existing industries. This arrested development, in turn, hinders an effective strategic coupling between the regional economy and multinational corporations, thus undermining regional resilience.     

Evolution,science and society: Historical reflections on the geographical experiment

Of the many diverse sources of naturalistic thinking in early modern geography, the penetration of Darwinian evolution is conventionally regarded as one of the most influential. In its application to social processes, the term ‘Social Darwinism’, as it is generally designated, has been used to describe almost any evolutionary perspective on human society. In its most common form, ‘Social Darwinism’ (or ‘Business Darwinism’, as some have designated it) has been portrayed as an attempt to provide ‘scientific’ justification for the cut-throat ethics of late nineteenth century capitalism. The main contention of this essay is that the widespread use of the term ‘Social Darwinism’, has obscured the variety of other ways in which biological analogies were applied to society, and that one of the most influential of these was the social model erected on the Lamarckian evolutionary alternative — a version of evolutionary biology widely espoused by geographers in Britain and America. Social Lamarckism, by emphasizing the cumulation of social improvements, repudiated the non-interventionism of ‘Social Darwinism’ and was used by many geographers to underpin their support for numerous educational, eugenic and environmental movements to improve the condition of humanity. And while biologically bankrupt, the Lamarckian social schema continues to be invoked as a viable model of society's evolution.     

Water reform governmentality in Ecuador: Neoliberalism,centralization, and the restraining of polycentric authority and community rule-making

In most Latin American countries, issues concerning water governance and control also reflect broader conflicts over authority and legitimacy between the state and civil society. What lies behind the diverse water policy reforms is not simply a question of governing water affairs but also a drive to control or co-opt water user groups. This paper examines the efforts by the present Ecuadorian government to ‘control water users’ through new forms of ‘governmentality’ (Foucault, 1991). We use the ‘cathedral and bazaar’ metaphor (Lankford and Hepworth, 2010) to illustrate government rationale and practices in water governance shifts in the last decades. We analyze how Rafael Correa’s government sets out to reshape the relations between state, market and society. In its ‘Twenty-first Century Socialism’ project, based on a proclaimed ‘Citizen Revolution’, actual policy reform does not reverse but rather transforms the process of neoliberalizing water governance – creating a hybrid bazaar-cathedral model. We argue that the current water govermentality project implements reforms that do not challenge established market-based water governance foundations. Rather it aims to contain and undermine communities’ autonomy and ‘unruly’ polycentric rule-making, which are the result of both historical and present-day processes of change. Interestingly, water user federations that emerged during the neoliberal wave of the last two decades now claim water control space and search for new forms of democratizing water governance. They act as agents who fiercely – yet selectively and strategically – oppose both elements of the State-centered (cathedral) and market-based (bazaar) water governance models.     

Carboniferous fossil forests

Forests of Carboniferous age, first described in detail in the nineteenth century, are often illustrated in textbooks, but their ecological and evolutionary significance has been largely overlooked or, worse, misrepresented. It has often been thought that the standing fossil forests found rooted in coals represent relicts of the peat-forming vegetation. Recent research has suggested that this is not always the case and that many of the standing trees represent an essentially non-peat-forming wetland ('clastic swamp') vegetation comprising a distinctive set of genera and species of plants. Recent investigation of several famous examples - Weaklaw, Arran and Joggins as well as new examples such as Mary Lee and Table Head - is throwing new light on the ecological and evolutionary significance of these fossil forests.     

Golf and the environmental politics of modernization

In this critical review we reflect on findings from a socio-historical study of golf’s relationship with the environment. We focus especially on the golf industry’s pursuit of modernization from the early 1900s to the present. Golf’s quest to ‘be’ modern, we contend, has specifically constituted three particular ‘turns’: a first turn in the early 1900s involving the scientific rationalization of golf course development and maintenance; a second, ‘exemptionalist’ turn in the post-war years whereby science and technology fueled a perception of immense control over nature; and a third, more recent turn to ecological modernization (EM) whereby science and technology are leveraged toward environmental stewardship – or at least claims thereof. We ultimately argue that the golf industry’s recent adoption of EM principles in their environment-related work has political implications, as it ‘protects’ the industry from more radical environmental alternatives.     

Evolutionary and geological events across the Precambrian–Cambrian boundary

Over the last decade, palaeontologists around the world have been striving to understand one of the most remarkable episodes in the fossil record: the explosive evolution of skeletal fossils around the Precambrian–Cambrian boundary. When examined in the field, the close association of geological and biological events is apparent. An important succession in this respect is the classic Precambrian and Cambrian area of Charnwood–Nuneaton in the English Midlands. Here it can be seen that the boundary also spans a time of major tectonic and oceanographic changes. Could these have contributed to the ‘Cambrian evolutionary explosion’?     

Flow variability and the biophysical vitality of river systems

We illustrate the fundamental importance of fluctuations in natural water flows to the long-term sustainability and productivity of riverine ecosystems and their riparian areas. Natural flows are characterized by temporal and spatial heterogeneity in the magnitude, frequency, duration, timing, rate of change, and predictability of discharge. These characteristics, for a specific river or a collection of rivers within a defined region, shape species life histories over evolutionary (millennial) time scales as well as structure the ecological processes and productivity of aquatic and riparian communities. Extreme events – uncommon floods or droughts – are especially important in that they either reset or alter physical and chemical conditions underpinning the long-term development of biotic communities. We present the theoretical rationale for maintaining flow variability to sustain ecological communities and processes, and illustrate the importance of flow variability in two case studies – one from a semi-arid savanna river in South Africa and the other from a temperate rainforest river in North America. We then discuss the scientific challenges of determining the discharge patterns needed for environmental sustainability in a world where rivers, increasingly harnessed for human uses, are experiencing substantially altered flow characteristics relative to their natural states.     

Biosedimentary record of postglacial coastal dynamics: high‐resolution sequence stratigraphy from the northern Tuscan coast (Italy)

Integrating analysis of the benthic palaeoecological record with multivariate ordination techniques represents a powerful synergy able to provide an improved characterization of coastal depositional facies in a sequence stratigraphical perspective. Through quantitative analysis of benthic foraminifer, ostracod and mollusc associations from the postglacial succession of Core M3 (Arno coastal plain, Tuscany, Italy), and application of detrended correspondence analysis (DCA) to the mollusc sub‐data set, we offer a refined picture of stratigraphical variations in faunal content from a paralic depositional setting, and reconstruct the palaeoenvironmental gradients that account for such variations. Despite distinct ecological behaviours, and taphonomic and sedimentological constraints, a strong ecological control on meio‐ and macrofaunal biofacies and taxa turnover is documented across the study succession. Amongst all possible mechanisms that may play a role in ‘shaping’ fossil distribution, the ecological signal driven by salinity represents the most prominent factor controlling the composition of fossil associations in the cored succession. Molluscs can even provide outstanding quantitative estimates of palaeosalinity along the sampled core. When plotted stratigraphically, the three fossil sub‐data sets show consistent patterns of vertical evolution that enable prompt identification of the key surfaces for sequence stratigraphical interpretation in otherwise lithologically indistinguishable deposits. The concomitant maximum richness of species with strong marine affinity, paralleled by the highest DCA salinity estimates, allows recognition of the maximum flooding zone, dated to ～7.7 cal. ka BP, within a homogeneous succession of outer lagoon clays. These clays are sandwiched between early transgressive, swamp to inner lagoon deposits and overlying prograding coastal?alluvial plain facies.     

On the experimental silicification of microorganisms. III. Implications of the preservation of the green prokaryotic alga prochloron and other coccoids for interpretation of the microbial fossil record

Evidence for Precambrian fossil eukaryotic microorganisms has been based on: (1) the presence of internal ‘spots’ which have been variously interpreted to be remains of nuclei or pyrenoids of photosynthetic plastids or other organelles; (2) tetrahedral tetrad arrangement of cells; (3) trilete scars interpreted to be indicative of meiotic division: (4) large cell diameters; and (5) putative mitotic cell divisions. These features have been reported in fossils preserved in Precambrian cherts. We have studied modern microbial mats, thought to be analogues of Precambrian fossil communities, and found they may be silicified by laboratory procedures. In microbial mats from Baja California we have found many ‘spot cells’ that we could identify as remains of cyanophytes. We have silicified the newly discovered large prokaryotic coccoid green alga Prochloron and have found that it, like many cyanophytes previously silicified, preserves its structure and maintains its initial dimensions. In laboratory-silicified prokaryotic organisms we have found that all of the above criteria, supposedly characteristic of eukaryotes, can be observed. We conclude that there is no compelling morphological evidence for fossil eukaryotic microbes from Precambrian cherts.     

The use of wetland water balances to link hydrogeological processes to ecological effects

A methodology for modelling wetland water levels using the water balance approach was developed for Pulborough Brooks Site of Special Scientific Interest in West Sussex, in the UK. The methodology was applied to assess potential groundwater abstraction impacts on communities and species of ecological importance in the wetland. The modelling methodology links regional hydrogeological processes to wetland hydrology and ecology that is typically influenced by processes that take place at a more reduced spatial scale. To assess impacts, it is necessary to understand the hydrological sources of water that are affected by abstraction as well as to consider how the magnitude of these processes relates to other processes that influence wetland water levels. Water levels are commonly the most important factor determining the presence or absence of species or communities in a wetland and the model predicts wetland water levels and assesses how suitable these water levels are for species of ecological significance. Model results show that typical historic rates of abstraction have not resulted in an adverse effect on the integrity of the Pulborough Brooks relative to a ‘natural’ (no abstraction) scenario.     

Continental sedimentation, soil genesis and marine transgression in the basal beds of the Cretaceous in the east of the Paris Basin

In the eastern Paris Basin, on the boundary of two French ‘départements’, Marne and Meuse, the Cretaceous deposits begin with Wealden facies assigned to the Valanginian. This is overlain by marine Hauterivian and Lower Barremian. Several techniques have been used for studying these deposits: light-microscope, scanning electron microscope, grain-size analysis, chemical and mineralogical analysis. Environmental interpretations of the various facies are based on sedimentological, geochemical and pedological criteria (fossil soils are present). Clay minerals are dominantly illite and kaolinite. In the soil horizons kaolinite is dominant. A mixed-layer illite-smectite appears at the base of the transgression. Under marine influence a more stable illite dominant suite is formed. The Wealden sediments appear to have been deposited in a very mature flood-plain. Part of the sequence was subjected to weathering in situ by soil processes under a warm climate with repeated wetting and drying. Paraconformably above, the marine Hauterivian is the product of a shallow sea that tended to form lagoons. A true marine environment was established in the Lower Barremian, when mixing homogenized the sediments.     

Cleiothyridina obmaxima McChesny的个体发育、生态特征及进化途径

本文通过对Cleiothyridina obmaxima在同一化石点产出的大量个体的统计研究,讨论了该种个体发育的阶段及其种群动力学特征,并做出了相应的解释。同时根据该种个体形态的特征及其在个体发育不同阶段的变化,结合其所赋存的群落及其围岩特征,讨论了其个体生态学及其环境意义,进而探讨了该种的演化途径。     

Hominins without fellow travellers? First appearances and inferred dispersals of Afro-Eurasian large-mammals in the Plio-Pleistocene

Discoveries of fossil Homo outside Africa predating 1.0 Ma have generated much discussion about hominin dispersal routes. However, tool-using bipeds were only one element of the inter-continental mammalian dispersals that occurred during the climatic changes of the Pliocene and Pleistocene. This paper will place hominin movements in the context of those of the wider mammalian fauna, which includes carnivores, bovids and non-human primates. The distribution of these different taxa suggests that species moved individually when the environmental conditions were right for them, rather than in multi-species waves of dispersal, and allows evaluation of the contextual evidence for the newly emerging ‘Out of Asia’ paradigm as well as the established ‘Out of Africa’ model.     

The urban land debate in the global South: New avenues for research

The global ‘land grab’ debate is going urban and needs a specific conceptual framework to analyze the diverse modalities through which land commodification and speculation are transforming cities across the globe. This article identifies new avenues for research on urban land issues by drawing on an extensive body of academic literature and concrete cases of urban land transformations in Asia, Latin America and Africa. These transformations are analyzed by focusing on three types of urban investments – investments in property, investments in public space and public services, and investments in speculation, image building and ‘worlding’ – and the way these investments are intermingled with and enhanced by processes of gentrification and speculative urbanism. Addressing real estate and infrastructure investments, speculation and gentrification through a land-based lens allows us to deepen the discussion on urban land governance in the global South. We argue that urban land acquisition cannot be thoroughly understood in isolation from the workings of urban real estate markets, public policies, and displacement processes. The urban land grab debate needs to consider the dialectic interplay between land use change and general socio-spatial transformations both in central – or recentralized – and peripheral areas. This is why we plea for a kaleidoscopic perspective on urban land governance by uncovering the complex patchwork of urban land acquisitions and their diverse temporalities and spatialities, their hybrid character in terms of actors involved, and the multiple and often unpredicted ways in which urban dwellers try to gain control over and access to urban land.     

海相遗迹化石对显生宙生物大辐射事件的响应*

通过系统梳理前寒武纪和显生宙海相遗迹化石记录及笔者自己的研究,发现在寒武纪生命大爆发、奥陶纪生物大辐射、中生代海洋革命共3次里程碑式的生物大辐射过程中,海相遗迹化石的属级多样性变化和歧异度增减均与生物多样性呈正相关,生物扰动强度和深度明显增加,造迹生物的觅食策略和行为习性多样化明显增多。寒武纪生命大爆发时期,最有代表性的生物行为变化是出现了具有垂向分量的潜穴; 奥陶纪生物大辐射期间,海相遗迹化石的分布逐渐从滨、浅海扩展至半深海和深海,表现为造迹生物群落栖息地的扩张; 中生代海洋革命时期,海相和陆相遗迹化石同步增加,生物对生态空间利用的深度、广度和集约性同步增强,遗迹化石面貌表现为深海雕画迹的多样性和歧异度大幅增加、形态类型多样、多种觅食策略共存。地史时期的海相遗迹化石面貌受环境外因和生物内因控制,表现出形态由简到繁、分布范围由小到大的变化趋势,对生态空间的利用表现为由沉积物表层至浅层再到深层、由二维到三维、由局域(浅水)到广域(浅水和深水以及陆地)的发展,印证了生物获取生态机会的过程。