黑龙江青冈地区晚更新世猛犸象-披毛犀动物群生存的环境背景

更新世晚期大型哺乳动物消亡一直是科学界关注的热点科学问题,其消亡的环境背景和影响机制仍没有形成一致观点。我国东北地区晚更新世地层中保存有丰富的猛犸象-披毛犀动物群(Mammuthus-Coelodonta Fauna)化石记录,是研究更新世晚期大型哺乳动物生存环境及消亡过程的理想区域。黑龙江省青冈地区出土有典型的晚更新世哺乳动物化石种类,如真猛犸象(Mammuthus primigenius)、披毛犀(Coelodonta antiquitatis)等。本文以青冈县英贤村化石出土剖面为研究对象,通过孢粉分析,重建猛犸象-披毛犀动物群的生存环境背景。青冈地区猛犸象-披毛犀动物群出土于湖沼相沉积中,研究发现其生存环境的主要植被成分是蒿属、菊科、禾本科、莎草科和云杉属,指示草甸草原为主,局地生长有针叶林的植被景观。欧亚大陆晚更新世高纬度地区广泛分布的猛犸象草原植被曾延伸到我国东北地区。     

广西扶绥南山洞新发现的人类化石和蒙古野驴化石——末次冰期华南气候变化的哺乳动物化石新证据

广西扶绥县南山洞发现人类化石及哺乳动物化石。人类化石包括2枚智人牙齿化石,分别是左下第三臼齿和右下第二臼齿,其形态特征与广西其他山洞发现的智人化石相似,归入晚期智人。哺乳动物化石多为华南大熊猫———剑齿象动物群成员,时代属更新世晚期。该地点新发现的蒙古野驴化石属华南晚更新世动物群的首次发现。南山洞所有化石发现于洞内浅褐色砂质粘土中,堆积物第二层钙板层的铀系年龄为30—40ka。蒙古野驴的出现暗示中国南方大陆可能在末次冰期出现过干冷的气候环境。     

吉林青山头遗址哺乳动物群及其地质时代

近年来在吉林省前郭县青山头第四纪地层中陆续发现了旧石器时代晚期的人类化石、新时器时代早期的人类遗骸和大量文化遗物及共生的动物群。本文着重讨论该遗址的两个不同哺乳动物群的性质及时代,这将对确定该区更新世与全新世地层界线、探索猛犸象-披毛犀动物群后期的演化提供了新的资料。     

乌尔吉晚更新世动物群和古生态环境

乌尔吉地区晚更新世地层出露广泛,哺乳动物化石常有发现.乌尔吉动物群属于猛犸象—披毛犀动物群,其时代为晚更新世晚期.动物群的生态性质明显反映了当时应为寒温带湿冷草原为主间有疏林和少量灌丛的自然景观.     

陕西洛南龙牙洞动物群的特点、时代及环境

从陕西洛南龙牙洞中采得哺乳动物化石３０多个属种,与之共存的有洛南直立人及其石制品。该动物群中同时具有古北区和东洋区的动物,为华北－华南动物地理区系间的一个过渡性动物群,时代为早更新世晚期,可与公王岭动物群对比。动物群的性质反映了当时洛南地区乃至秦岭东段为一温暖、湿润的森林草原环境,部分属种可能主要因为不适应急剧变化的气候而绝灭。     

山东淄博第四纪裂隙动物群

简要记述产自山东淄博孙家山裂隙群的主要哺乳动物化石,将之分为A、B、C三个动物群。A动物群时代与周口店第18地点相当,为早更新世早期;B动物群时代与周口店第9地点相当,为早更新世晚期;C动物群则可能与周口店第1地点中上部层位的时代相当,为中更新世中晚期。分析不同种类的生态类型并依据最小个体数的统计结果,认为早更新世早期本区为相对温湿的草原环境,附近可能有荒漠化现象;早更新世晚期气候较为温湿,无荒漠化现象;中晚更新世主要为林缘—灌丛环境,气候更为湿润。A动物群是华北地区早更新世早期特有的动物群,略具南北过渡区的特征;B动物群初具现代动物区系的面貌;C动物群基本与现代动物区系一致。     

我国南方第四纪哺乳动物群的划分和演变

到目前为止,通过调查和研究已认识到,在我国南方第四纪存在四个主要的哺乳动物群,即:元谋动物群、柳城巨猿动物群、大熊猫-剑齿象动物群和现代哺乳动物群。本文对这四个主要的哺乳动物群的进一步划分和演变进行讨论。元谋动物群、柳城巨猿动物群、建始高坪动物群和柳州笔架山动物群均属早更新世。元谋组发现的动物群似乎可以分为两个不同的层位:早期以森林中生活的动物为主,其时代似可划归晚上新世;晚期的动物则反映出以森林—疏林草原为主的生态环境。早更新世的元谋动物群以元谋组上部(3—4段)发现者为代表。柳城巨猿动物群中现生种类比元谋动物群中多,似较后者为晚。柳城巨猿动物群和大熊猫-剑齿象动物群有较密切的关系,可以说前者是后者的原始类型。建始高坪动物群和柳州笔架山动物群代表柳城巨猿动物群和大熊猫-剑齿象动物群之间的过渡类型。大熊猫-剑齿象动物群的地质时代为中-晚更新世,根据动物群的组合情况可分为四个不同的发展阶段:(1)含第三纪残留种类或古老种类;(2)含中更新世典型种类;(3)含早期智人化石;(4)含晚期智人化石或相当于这一阶段的人类制造的文化遗物。我国南方现代哺乳动物群奠基于大熊猫-剑齿象动物群,大体上形成于晚更新世后期。在全新世早期可能有个别更新世残留下来的种类,稍后可能还有个别绝灭种或绝灭亚种;而地理分布改变的种类,在全新世较长的时期内还有所残留。我国南方第四纪哺乳动物表现出土生土长的特点。动物群大致经历过三次较大的变化。和华北地区比较,我国南方第四纪哺乳动物群显示出三大特点:(1)古老种类延续时期较长;(2)现生种类出现较早;(3)动物群的变化不及华北那么明显。     

晚更新世大动物群绝灭之谜

乳齿象、大角鹿、剑齿虎,这些哺乳动物曾在地球上构成一道壮观的风景线,类似这些体重大于44公斤的动物群体被称之为大动物群。57万年前,大陆上栖息着的大动物群超过150属,然而到了1万年前,至少已有97属绝灭了。解释这场绝灭有着不同的学说;较占优势的分别有：人类活动影响,环境的变化以及两的相互作用。现今,来自最新的气候学、生态学、考古学、古生物学的证据又是如何解释史前这场对大动物群发动的“政变”呢?     

披毛犀和猛犸象的地理分布、古生态与有关的古气候问题

披毛犀(Coelodonta antiquitatis Blumenbach)和猛犸象(Mammuthus primigenius Blume-nbach),在更新世时曾广泛分布在北半球极为辽阔的地带。它们是在更新世冰期气候影响下,逐步发展起来的类型,是冰期气候的标帜。更新世晚期,披毛犀与猛犸象,在北半球的分布范围,曾明显向南扩展,尤其是披毛犀在中国的西南部与东部,都曾突出地向南伸展到北纬33°左右。这是在第四纪气候多次波动的影响下,冰川一次又一次的扩张,海洋面逐渐降低。气候带南移,北极动物与北方动物向南迁移的具体反映。     

从异地迁入的动物类群是北美西部内陆地区古新世最早期哺乳动物群的重要组成部分吗?(英文)

K/T界线绝灭事件后残存类群的迁入和地方性辐射在北美西部内陆地区的古新世最早期(Puercan期)哺乳动物群的进化中所起的作用存在争议。持续的野外工作和室内研究极大地扩展和提升了我们对北美地区的白垩纪最晚期(北美陆相哺乳动物分期的Lancian期)和Puercan1期(Pu1)的地方动物群组成的认识,也揭示了这些地方动物群生物年代学对比的局限。总的来说,北美西部内陆地区北部的Pu1地方动物群主要由多瘤齿兽类和真兽类组成,而Lancian期存在的有袋类各类群绝灭。大多数的Pu1哺乳动物是由其他地区迁移而来,其中许多类群在K/T界线后不久就迁徙到这个地区。北美洲古纬度高的地区和亚洲太平洋沿岸地区的白垩纪最晚期或者古新世最早期哺乳动物群的缺乏,妨碍了对异地迁移到北美的哺乳动物起源于亚洲这一假说的验证。另一个假说认为,大多数迁入北美西部内陆地区北部的Pu1哺乳动物可能来自北美大陆的其他地区。这一假说得到了越来越多的支持,并且没有证据表明是错误的。     

Isotopes stables (C,N) du collagène des mammouths de Mezhyrich (Epigravettien,Ukraine) : implications paléoécologiques

The mammoth steppe ecosystem was characterized by a high diversity in large mammals species distributed on a vast geographical range. The isotopic analyses of the collagen of the faunal remains from this context testified the niche partitioning among large herbivores with a specialization in the types of consumed plants. In the case of the mammoth (Mammuthus primigenius), systematic higher abundances in ¹⁵N are found for this species compared to those of other grazers in Eurasia and Alaska during the Upper Palaeolithic. This distinct isotopic signature reflects a specific ecological niche. The analyses of mammoth remains at the Epigravettian site of Mezhyrich (15,000–14,300 conv BP) reveal low abundances in ¹⁵N that are equivalent to those of the associated horses. Thus, the mammoth of Mezhyrich experienced a significant change in their environment and diet that probably led to the loss of their ecological niche. A likely direct competition with other large herbivores and the possible predation by wolves and human populations should be considered for the mammoth of the Ukrainian plains, long before their extirpation from the region.     

Dichroplus vittatus (Orthoptera: Acrididae) follows the converse to Bergmann's rule although male morphological variability increases with latitude

Geographic body size variation was analysed in males and females of 19 populations of the South American grasshopper Dichroplus vittatus Bruner spanning 20 degrees of latitude and 2700 m of altitude. Using mean and maximum body length of each sex and factors obtained from principal components analyses of six morphometric linear characters it was shown that D. vittatus followed the converse to Bergmann's rule latitudinally but not altitudinally where no significant trends were observed. For males, variability of body size increased with latitude but not with altitude. Both types of trends were significantly correlated with mean annual temperature and minimum annual temperature (positive correlations), and two estimators of seasonality, the coefficients of variation of mean annual temperature (negative) and mean annual precipitation (positive). Some allometric relationships also showed geographic variation. It is suggested that the observed decrease in size with latitude together with the increase in morphological variability is a consequence of a number of factors: the shortening of the growing season southwards; the increasing seasonality and climatic unpredictability; and the fact that the species exhibits protandry which contributes to smaller and more variable size in males and smaller but more constant body size in females.     

Hypsodonty of Dipodidae (Rodentia) in Correlation with Diet Preferences and Habitats

The evolution of molar teeth from low-crowned (brachyodont) to high-crowned (hypsodont) has traditionally been recognized as a response to increasing tooth wear due to endogenous (e.g., fiber, silica) and/ or exogenous (e.g., dust, grit) properties of ingested food. Recent work indicates that the mean hypsodonty level of large herbivorous land mammalian communities is a strong predictor of precipitation in their habitats. For small mammals, however, the research is still in an early stage. This study performed comparative studies of hypsodonty on 26 extant dipodid species with and without consideration of phylogeny. The results confirm the role of diet in shaping the cheek tooth crown height in Dipodidae. The significant relationship of investigated environmental variables with hypsodonty may be partly due to phylogenetic effects. Nonetheless, the mean hypsodonty of dipodid communities has significant relationship with regional climatic variables. Hence, the hypsodonty of dipodids also has great potential to be a regional climate proxy.     

Mammouth et comportements de subsistance à l’Épigravettien : analyse archéozoologique du secteur de la fosse no 7 associée à l’habitation no 1 de Mezhyrich (Ukraine)

Zooarchaeological analyses were carried on new large mammal bone materials, from the Epigravettian (Late Upper Palaeolithic) site Mezhyrich (Ukraine), in the pit n^o 7 area associated with the mammoth bone dwelling n^o 1. The results exhibit a usage of the pit as a dump area of food and technical remains from mainly mammoth, hare and fox processing, and bone fuels. The information about mammoth procurement by the last Palaeolithic hunter–gatherers in Eastern Europe allows to document the hunting activities on the mammoth populations, which were probably already weakened at the end of the Pleistocene.     

A test of Allen's rule in ectotherms: the case of two south American Melanopline Grasshoppers (Orthoptera: Acrididae) with partially overlapping geographic ranges

We studied the geographic variation of three morphometric characters in relation to body size in two South American grasshoppers (Acrididae), Dichroplus vittatus Bruner and D. pratensis Bruner to test Allen's rule in these ectotherms. Since both species follow the converse to Bergmann's rule owing to latitudinal and/or altitudinal variation in time available for growth and reproduction, geographic variation in body size proportions of protruding parts may obey to differential allometric growth in different geographic areas. Alternatively, it could reflect true Allenian variation related to thermoregulation. Body proportions were studied by correlation/regression analyses with geographic and climatic variables. In D. pratensis, body proportions increased with latitude and decreased with altitude. These results probably obey to the effects of water balance and seasonality on final body size, and on the allometric growth of the three studied characters not being related to thermoregulation. In D. vittatus, a generally non-significant trend towards the decrease of the mean proportions of all three characters with increasing latitude was observed. Nevertheless, also in this species, it is probable that the environmental gradient responds to seasonality factors (although not to water balance) that affect the length of growing season and, in consequence, body size and its allometric relationships. We conclude that the regularities in the geographic distribution of body proportions of D. pratensis and D. vittatus do not follow Allen's rule in the sense of thermoregulation, and result from variables that determine growing season length and the allometric growth of different body parts.     

Subterranean rodents of the genus Ctenomys (Caviomorpha, Ctenomyidae) follow the converse to Bergmann's rule

Aim We analysed body‐size variation in relation to latitude, longitude, elevation and environmental variables in Ctenomys (tuco‐tucos), subterranean rodents in the Ctenomyidae (Caviomorpha). We tested the existence of inter‐ and intraspecific size clines to determine if these rodents follow Bergmann's rule, to compare intra‐ and interspecific size trends and to assess the relevance of the subterranean lifestyle on these trends. Location South America, south of 15° latitude. Methods This paper is based on 719 specimens of tuco‐tucos from 133 localities of Argentina, Bolivia, Chile, Paraguay, Peru and Uruguay, representing 47 named species and 32 undescribed forms. Intraspecific analyses were performed for Ctenomys talarum Thomas, 1898 and the Ctenomys perrensi Thomas, 1896 species complex. Head and body length and weight were used for estimating body size. Geographical independent variables included latitude, longitude and altitude. Environmental independent variables were mean minimal and maximal monthly temperature, mean annual temperature, mean minimal and maximal precipitation, and total annual precipitation. To estimate seasonality, the annual variability of the climatic factors was calculated as their coefficients of variation and the difference between maximum and minimum values. Mean annual actual evapotranspiration (AET), and mean annual, January (summer) and July (winter) potential evapotranspiration (PET) values were also calculated for each locality, as well as annual, summer and winter water balance (WB). Statistical analyses consisted of simple and multiple regression and nonparametric correlation. Results Body size of Ctenomys decreases interspecifically from 15°00′ S to 48°15′ S and from 56°33′ W to 71°46′ W, and is positively correlated with ambient temperature and precipitation. The best predictors of body size according to multiple regression analyses were mean annual temperature, the difference between mean maximum and minimum annual temperatures, annual PET, the difference between summer and winter PET, and annual and winter water balance. These patterns are repeated, but not identically, at a smaller geographical scale within the species C. talarum and the superspecies C. perrensi. Main conclusions Tuco‐tucos follow the converse to Bergmann's rule at the interspecific level. At the intraspecific level some parallel trends were observed, but the smaller scale of these analyses, involving a very reduced variation of environmental factors, necessitates caution in interpreting results. The subterranean lifestyle probably insulates these rodents from the external temperature. The observed latitudinal body‐size gradients are more probably related to seasonality, ambient energy, primary productivity and/or intensity of predation.     

A general view of the lower Palaeolithic of Turkey

Turkey is one of the rich countries in terms of the Lower Palaeolithic period. The favourable climatic and environmental conditions and quality stone raw material resources in the Pleistocene period caused the country to be heavily occupied by the people of the Lower Palaeolithic. Turkey has biface and flake industries of the Lower Palaeolithic period. Biface industries are more common in open-air sites and are often linked to the Acheulean. Biface tools are only found in the deposits of Karain Cave. The eastern and south-eastern parts of Turkey are the densest regions in terms of biface industries. This density decreases towards the west. However, this general appearance may have resulted from the insufficient level of excavations and surveys of Palaeolithic archaeology throughout the country. In this article, we try to draw a general framework of the Lower Palaeolithic period in Turkey, based on the important Lower Palaeolithic settlements in the country.     

THE SHAPE OF CONTENTION: ADAPTATION,HISTORY, AND CONTINGENCY IN UNGULATE MANDIBLES

Mandibles and teeth of ungulates have been extensively studied to discern the functional significance of their design. Grazing ungulates have deeper mandibles, longer coronoid processes, flatter incisor arcades, and more hypsodont molars in comparison to browsers. If the functional significance of both mandible and teeth shapes is well‐established, it remains uncertain to what extent mandible shapes are really adapted to grazing, meaning that they evolved either to serve their current biological function or just as a structural requirement to accommodate higher crowned molars. Here, we address this question by studying the contribution of phylogeny, hypsodonty, and body size to mandibular shape variation. The mandible shape appeared to be significantly influenced by hypsodonty but not by body size. Interestingly, hypsodonty‐related changes influenced the tooth row in artiodactyls and perissodactyls significantly but in the opposite directions, which is ultimately related to their different digestive strategies. Yet, we obtained a strong phylogenetic effect in perissodactyls, suggesting that their mandible shape should be strongly inherited. The strength of this effect was not significant within artiodactyls (where hypsodonty explained much more variance in mandible shape). Digestive strategy is deemed to interplay with hypsodonty to produce different paths of adaptation to particular diets in ungulates.     

Natural selection favors rapid reproductive phenology in Potentilla pulcherrima (Rosaceae) at opposite ends of a subalpine snowmelt gradient

In high altitude plants, flowering quickly ensures reproductive success within a short snow-free period, but limits maturation time and fecundity. Natural selection on prefloration intervals may therefore vary in contrasting snowmelt environments and could influence the outcome of phenological responses to climatic change. This study investigated adaptive differentiation and plasticity of prefloration intervals in the subalpine perennial Potentilla pulcherrima. Three years of in situ field observations were combined with phenotypic selection analyses and a common garden experiment. Plants from high, intermediate, and low altitudes expressed similar prefloration intervals and plasticity when grown at common altitude, indicating no evidence for adaptive differentiation. Selection on the prefloration interval was negative at both low and high altitudes before and after accounting for strong positive selection on size. Environmental differences between high and low altitudes indicated that long, dry seasons and short, wet seasons both favored rapid reproduction. Therefore, quicker reproduction was adaptive in response to late snowmelt, but slower reproduction in response to earlier snowmelt appeared to be maladaptive. Selection differed marginally between late snowmelt years and dry ones. Plastic responses to future precipitation patterns may therefore have positive or negative effects on fitness within a single species, depending upon altitude and year.     

Astronomically forced climate change in the Kenyan Rift Valley 2.7-2.55 Ma: implications for the evolution of early hominin ecosystems

Global climate change, linked to astronomical forcing factors, has been implicated in faunal evolutionary change in equatorial Africa, including the origin and diversification of hominin lineages. Empirical terrestrial data demonstrating that orbital forcing has a significant effect, or is detectable, at early hominin sites in equatorial continental interiors during the Pliocene, however, remain limited. Sedimentation patterns in the Baringo Basin within the Central Kenyan Rift Valley between ca. 2.7 and 2.55 Ma, controlled by climatic factors, provide a detailed paleoenvironmental record spanning 35 fossil vertebrate localities, including three hominin sites. The succession includes a sequence of diatomites that record rhythmic cycling of major freshwater lake systems consistent with approximately 23-kyr Milankovitch precessional periodicity. The temporal framework of shifting precipitation patterns, relative to Pliocene insolation curves, implicate African monsoonal climatic control and indicate that climatic fluctuations in Rift Valley ecosystems were paced by global climatic change documented in marine cores. These data provide direct evidence of orbitally mediated environmental change at Pliocene Rift Valley hominin fossil localities, providing a unique opportunity to assess the evolutionary effect of short-term climatic flux on late Pliocene East African terrestrial communities.