Biotic element analysis of reptiles of China: A test of vicariance model

Size: px
Start display at page:

Download "Biotic element analysis of reptiles of China: A test of vicariance model"

Transcription

1 Current Zoology 59 (4): , 2013 Biotic element analysis of reptiles of China: A test of vicariance model Youhua CHEN * Department of Zoology, University of British Columbia, Vancouver, Canada, V6T 1Z4 Abstract In this contribution, I identify possible biotic elements of reptiles of China using biotic element analysis. I test whether the vicariance model could significantly shape reptilian current distribution patterns. My results show that dispersal is prevailing for reptiles in China. There are four major biotic elements in reptilian distribution, which are East Xizang, Yunnan- Guizhou Plateau, Taiwan and Hainan, respectively. The test of distributional areas is significantly more clustered than expected by chance, while in another test that closely related species are homogeneously distributed across biotic elements cannot be rejected. Therefore I argued that vicariance might be one of the key processes in patterning reptilian distribution in China. In addition, I develop an improved biotic element analysis in biogeographic studies, by performing biotic element analysis in an iterative manner in order to diagnose more geographically restricted elements until no noise components found. The importance of antecedent selection of distributional data for the subsequent analysis is also discussed. Besides, my study indicates that biodiversity hotspots are not fully overlapped with areas of endemism for reptilians in East Asia [Current Zoology 59 (4): , 2013]. Keywords Biotic element analysis, Reptilian fauna, Biogeography, Null model Areas of endemism are defined as areas delimited by the congruent distribution of two or more species of restricted range, which constitute the basal units in historical biogeography (Morrone and Crisci, 1995; Linder, 2002). There are a number of approaches in revealing areas of endemism, biotic elements or basic units of biogeographic areas (Moline and Linder, 2006; Linder, 2002; Hausdorf and Hennig, 2003; Morrone, 1994). Although there are open debates on the just-mentioned terminologies and definitions (Casagranda et al., 2012, 2009), I treated them all as equivalent as the important areas for historical biogeography. The most widely applied method is parsimony analysis of endemicity (Rosen, 1988; Morrone and Crisci, 1995). Biotic element analysis (Hausdorf and Hennig, 2003) is a statistical approach to identify segregated/geographically restricted biotic elements in historical biogeography (Hausdorf, 2002). Biotic elements are defined as the groups of taxa that have similar distributional ranges significantly different from those of other taxa (Hausdorf, 2002; Casagranda et al., 2012). Although its effectiveness of identifying range-similar species clusters has been challenged recently (Casagranda et al., 2012), it is still applied in recent studies (Moline and Linder, 2006; Carvalho et al., 2011; Wronski and Hausdorf, 2008; Cabrero-Sanudo and Lobo, 2009; Hausdorf and Henning, 2010; Nogueira et al., 2011). The basic principle of biotic element analysis is to identify different species groupings through a Gaussian clustering analysis on the results returned by the non-metric multidimensional analysis. However, the groupings could be identified using hierarchical cluster analysis. In this sense, biotic element analysis is similar to cluster analysis with statistical tests (McCoy et al., 1986; Marquez et al., 1997; Baez et al., 2005). In previous studies (Hausdorf and Hennig, 2004, 2006), the widespread biotic element was directly eliminated without reconsideration. It might not be a good choice since there must be some fragmented distributional information within the widespread element, which could be re-determined from iterative analysis after excluding those determined geographically restricted elements. Besides, there must be some noise species (which have broad distributional ranges and could not be used to diagnose biotic elements) that have not been cleared out in the primary analysis. Therefore it is necessary to re-calculate biotic elements analysis using selective data set until all the noise components have been fully excluded. As such, I performed biotic element analysis for multiple times by iteratively analyzing the remaining data set so as to detect all possible geographically restricted biotic elements. Received Sep.16, 2012; accepted Feb. 5, Corresponding author. haydi@126.com 2013 Current Zoology

2 450 Current Zoology Vol. 59 No. 4 Vicariance biogeography is one subdiscipline of biogeography (Hausdorf and Hennig, 2006; and the references therein). The vicariance model commonly has two predictions (Hausdorf and Hennig, 2004, 2006) (both will be presented in detail in the Materials and Methods section). The first prediction, species from different endemic areas should form different biotic elements, could be tested using a Monte Carlo simulation. In the simulation, the null model can generate random range data sets in a way such that the range size distribution, species richness distribution and the spatial autocorrelation pattern are similar to the parameters in the real data set. Biotic elements were then delimited with a model-based Gaussian clustering process while excluding noise components. The second prediction for which closely related species should be classified into different biotic elements could be tested with a chi-squared test using the cross-table matrix after the biotic elements have been determined. There are five physical regions in China, three of which are Eastern monsoon region, northwest drought region and the Qinghai-Tibet Plateau (Zhao, 1995). Eastern monsoon region could be further divided into northeast plain, north plain, and southern hills. On the basis of biodiversity surveying and mapping, southern hills (covering most of the southern part of China, for example, Yunnan-Guizhou Plateau, Hainan and Taiwan Islands, and Zhoushan Archipelago) and Tibetan (or Xizang) highlands would become the focuses due to their high species endemicity (Chen and Bi, 2007; Chen, 2008, 2009a). It has been broadly accepted that there were multiple distinct biogeographical components of vertebrate fauna of China for a long time (Zhang, 1999). However, traditional studies have only paid attention to faunal similarity and biogeographical affinities of different regions, historical factors are hardly considered (Huang et al., 2008). In this study, I will test the importance of vicariance in shaping current reptilian distributional patterns of China and find out the geographically separated biotic elements. 1 Materials and Methods 1.1 Distribution data The distributional data set of 309 reptilian species of China was derived from CSIS ( which has widely collected each species distribution from various multiple resources. The distributional records have been checked and verified using faunal books or literature, including, Zhao (1999), Zhao et al. (1998), Zhang et al. (1998), Chen (2009) and China Wildlife Conservation Association (2002). A database containing species names, taxonomic classification, distributional counties and geographical coordinates was complied then. My study covered the major orders of reptiles as introduced in the Fauna Sinica (Zhao, 1999; Zhao et al., 1998; Zhang et al., 1998), including Squamata, Testudoformes and Crocodiliformes. Each distribution record was checked to find possible new distributional coordinates and was projected into 1 1 geographical units (latitude longitude) to form 510 grid cells in which 309 reptilian species occur. In such a way a matrix was built for further analysis. 1.2 Richness mapping The grid cells that have top 2% richness of species (species count) are regarded as hotspots (Williams et al., 1996). A geographical information system tailored for biodiversity studies DIVA-GIS ( was utilized to perform mapping procedure. Of course, given the condition that no phylogenetic information is available, our study therefore is only limited to specieslevel diversity mapping of reptiles. 1.3 Biogeographical tests of the vicariance models There are two predictions deriving from the vicariance model (Hausdorf, 2002; Hausdorf and Hennig, 2003; Hausdorf and Hennig, 2006): 1) Species that originated in different areas of endemism by vicariance events form distinct biotic elements; and 2) closely related species that originated by vicariance do not occur within the same area of endemism, but distribute homogenously across different areas of endemism and hence belong to different biotic elements. These tests were implemented using the package PRABCLUS developed by Hausdorf and Hennig (2004) under the R environment (R Development Core Team, 2011). I used the program with the default settings and the Kruskal method is applied for performing clustering analysis (Cabrero-Sanudo and Lobo, 2009). 1.4 Determination of biotic elements Biotic elements (clusters of taxa with similar ranges) are determined using model-based Gaussian clustering with noise category (Hausdorf and Hennig, 2003). This method provides decisions about the number of meaningful clusters and the number of points that cannot be assigned adequately to any biotic element (noise category). To reveal all the possible regionally restricted elements, I re-calculated the analysis using reduced data set which discards those areas and species in geogra-

3 CHEN YH: Biotic elements of reptilians 451 phically restricted biotic elements (defined as an element that covers a narrow and small range of the whole study region). This iterative analytical process was stopped until all noise components have been removed. 1.5 Test for distribution of species groups across biotic elements The second prediction of the vicariance model is that closely related species belong to different biotic elements because they originated in different areas of endemism. It can be tested after biotic elements are determined. Following the suggestion of Hausdorf and Hennig (2006), species in a genus that is not divided into different subgenera were considered groups of closely species. The species are classified in such a way that taxonomic groups are rows and biotic elements are columns in the cross-table. Species belonging to the noise category, widespread elements and species without closely related species in the biotic elements are omitted. The vicariance model predicts a uniform distribution of species groups across biotic elements corresponding to the cross-table expected under the null hypothesis of independence of rows and columns (Hausdorf and Hennig, 2006). I used the Chi-squared test for independence of rows and columns of the table to test the second vicariance prediction. 2 Results 2.1 Species richness patterns The richness map is showed in Fig. 1. Ten grid cells with top 2% reptilian richness are marked in dark grey colors. The grid cell with highest richness number (97 species) is located in North Guangxi, followed by south of Hainan Island with 84 species and south of Yunnan with 79 species. The latter two grid cells correspond to two biotic elements respectively as discussed in the latter part of the study. 2.2 Tests for clustering of reptilian distribution areas The test statistic t=0.531, the ratio between the 25% largest and smallest distances (Hennig and Hausdorf, 2004), is significantly smaller than expected by chance for the reptilian species in China (Simulated t=0.603; ranging from to 0.654; P<0.01). The test indicates that the distribution areas of these reptilian taxa are significantly clustered and could be used for biotic element analysis. 2.3 Biotic elements In the primary biotic element analysis of the 309 species, 286 species were assigned to 9 biotic elements, in which only East Xizang element (17 species) and Taiwan element (15 species) are regionally restricted ele- Fig. 1 Top 2% richness hotspots of reptiles in China (red numbers inside the map indicate the species richness and the location of the hotspots) The provinces related to the current study are showed as abbreviations: XZ-Xizang Province, SC-Sichuan Province, YN-Yunnan Province, GZ-Guizhou Province, GX-Guangxi Province, HN-Hainan Province, FJ-Fujian Province, TW-Taiwan Province.

4 452 Current Zoology Vol. 59 No. 4 ments (Fig. 3). Another seven elements are widespread in most of the grid cells. The remaining 23 species (7.4%) are included in the noise component. The partition of the species to clusters is shown in the first two dimensions of a non-metric multidimensional scaling in Fig. 2. After discarding 32 element-related species, 23 noise species, 8 element-related grid cells, and 1 species that didn t occupy any of the retained grid cells, the remaining 253 species and 194 grid cells formed a matrix for the next round of biotic element analysis. MDS2 Fig. 2 Multi-dimensional analysis results of the first biotic element analysis Light blue rectangles indicate the regions where the numeric values inside are extensively overlapped. Fig. 3 The four geographically restricted biotic elements Colors from light blue to deep blue represents the species richness of the cells from low to high.

5 CHEN YH: Biotic elements of reptilians 453 In the second round of biotic element analysis (tests for clustering: P<0.01), 7 elements are identified but only one element (Element 3: Hainan element, with 10 species) is geographically restricted (Fig. 3). 33 species were found as noise species. After wiping off elementrelated species and grid cells, the residual 210 species and 202 areas formed another matrix for the third iterative analysis. In the third analysis (tests for clustering: P<0.01), 9 elements are identified without noise components. Only one element (Element 4: Yunnan-Guizhou plateau element) was diagnosed as geographically restricted (Fig. 3) with 10 supportive species. Since one has reached the fully noise-free results, one could stop the whole analytical procedure. 2.4 Distribution of species across biotic elements For analysis of the distribution of closely related species across biotic elements, the noise category and the species without closely related species in the biotic elements were omitted, resulting into 23 species belonging to 10 genera (Achalinus, Cyrtodactylus, Hydrophis, Japalura, Oligodon, Pareas, Rhabdophis, Scincella, Takydromus and Trimeresurus). A chi-squared test showed that closely related species are not significantly grouped into the same biotic element than expected by random (P=0.999). The null hypothesis that closely related species are homogeneously distributed across biotic elements could not be rejected, 3 Discussion 3.1 Characteristic of biotic elements I only identified four major geographically restricted elements for reptilian fauna. For other noisy elements, due to the geographical limitation, they show a widespread mode and are needed to re-analyze using more comprehensive species information. The elements identified here are also almost congruent with the previous results (Chen and Bi, 2007; Xu, 2005; Huang et al., 2008). 3.1 The east Xizang element This element (element 1 in Fig. 3) was featured with large amounts of endemic species (i.e., Cyrtodactylus medogensis, Ptyctolaemus gularis, Elaphe hodgsoni), of which all the 17 species are geographically endemic. This element belongs to the Qinghai-Xizang Plateau, the highest and largest plateau in China with averaging altitude of m. Considerable attention has been paid to this biotic element due to its high diversity and peculiar fauna (Liang, 2003; Xu, 2005; Chen and Bi, 2007; Huang et al., 2008). The uplift of the Qinghai-Xizang Plateau (three major stages: pre-india-asia collision-100 Ma ago; post-india-asia collision-55 Ma ago; recent abrupt uplift-7 Ma ago) (Wang et al., 2008) is the most important historical event in shaping this element directly. The Kunlun and Qilian Mountains stop the cold air from Siberia in the north, which offers better survival condition for endemic reptilian species. Besides, due to its high elevation characteristic, it is unlikely for gene flow and exchange to happen in the element and other adjacent low-altitude areas. 3.2 The Yunnan-Guizhou Plateau element This element (element 4 in Fig. 3) is located in the Yunan-Guizhou Plateau, the second highest plateau in China. This element has wider distributional boundaries compared to other elements. Hengduan Mountains in the west, Daba Mountains in the north and Wuling Mountains in the east are the major barriers to isolate the element to other areas and the East Xizang element. These barriers are formed around the Yanshan orogenic movement in the Cretaceous period ( Ma) (Wan, 2004). Vicariance model gives a relatively good explanation of the distinct faunal difference between the East Xizang element and the Yunnan-Guizhou Plateau element, which were separated by the various mountainous ranges in southwest of the Yunnan-Guizhou Plateau. Glacial refugia predicted by glacial refugium hypothesis (Holder et al., 1999) were consistent well with this element in terms of ranges. During the Pleistocene ice ages, SW China is located in the southeast of the Xizang-Qinghai Plateau surrounded by Hengduan Mountains and in the south of the Qinling and Daba Mountains. The plateau and mountains form a natural division between the temperate zone and subtropical zone in China. Consequently, SW China was less affected by cold air from Siberia during the glaciations (Shen et al., 2005) and became refuge sites for animals and plants. The Yunnan-Guizhou element corresponds to this refugium zone fully, and the East Xizang element was also fallen into this zone. 3.3 The Taiwan element Apparently Taiwan Strait is a natural obstacle to insulate the fauna of Taiwan from mainland China (Element 2 in Fig. 3). The characteristic species are Calliophis sauteri (Elapidae), Takydromus sauteri (Lacertidae), Achalinus formosanus (Colubridae) and others. Taiwan Mountains in the center part of the island might be the barrier between western and eastern part of the reptilian distribution. When inspecting the distributional of this element

6 454 Current Zoology Vol. 59 No. 4 (one grid cell located in SE mainland China, others in Taiwan Island), I could also find a strong biogeographical affinity between the coastal areas of SE China and Taiwan. The historical formation of this element is rather old. Taiwan is part of mainland China ( Cathaysian Ancient Terrene ) in the eras of Paleozoic and Mesozoic. Vertebrate species could disperse across southeastern part of mainland and Taiwan Island easily. Then due to the crustal movement in the Tertiary, the ingression of seawater made Taiwan Island go up and down the sea level at times. During the time interval between the Pliocene and Pleistocene (5 1.8 Ma), the recent abrupt uplift of the Qinghai-Xizang Plateau ( Ma) (J. Li and Fang, 1998; Wang et al., 2008) caused the main body of Taiwan Island uplift out of sea level fully. At about 0.01 Myr ago (the end of the glacial age in the Quaternary), the worldwide transgression made the internal descended areas between mainland and the island evolve into the current strait. 3.4 The Hainan element (Element 3 in Fig. 3) Qionghai Strait is the first barrier to segregate the reptilian distribution with mainland China, while the high mountainous range in the middle part of the island was the second barrier to isolate the Southeastern and Nothern reptilian distribution ranges within the island. This element has been already discussed for birds and mammals (Chen, 2008, 2009) respectively. Species such as Rhabdophis adleri (Colubridae), Cistoclemmys galbinifrons (Geoemydidae; a threatened species), Ophisaurus hainanensis (Anguidae) support this element. In the uplift period of the Qinghai-Xizang Plateau (could be dated back 100 Ma ago) (Wang et al., 2008), due to the volcano activities, the subsidence between Leizhou Archipelago and Hainan Island formed the primary prototype of Qionghai Strait, which began to isolate Hainan Island from mainland China. However, Hainan Island re-connected to mainland China repetitiously due to the fluctuation of sea level for many times (the reconnection frequency should be high, no literature so far has estimated the reconnection times between Hainan Island and mainland). The current island body was formed ultimately until the end of glacial age of the Quaternary as Taiwan Island due to transgression. This element, together with the Taiwan element are formed later than the Xizang element and the Yunnan- Guizhou Plateau element in geological history (Xu et al., 2003), because the Hainan and Taiwan elements are actually isolated from mainland China in the Quaternary Period. However, the East Xizang and Yunnan-Guizhou Plateau elements were segregated from each other during the Yanshan orogenic movement in Cretaceous period. In sum, from the above illustrations and tests of two vicariance hypothesis, ones can know that the orogenic movements and transgressions have actually contributed to most of the vicariance events of reptilian fauna in China. Vicariance model is prominent in the evolution of the reptilians, but one could not conclude that it plays a full role in shaping reptilian distribution without paying attention to speciation modes. As a matter of fact, the two tests of vicariance model are based on a data matrix without considering a large amount of widespread species and singular occurrence species, which might greatly reduce to the possibility of utilizing speciation models for interpreting reptilian distribution without a detailed examination of some informative distributional data. 3.5 Relation of richness hotspots and biotic elements It is not surprising that there existed partial overlaps between the biotic elements and biodiversity hotspots (Chen and Bi, 2007; Myers et al., 2000; Huang et al., 2008), as shown in Figs. 1 and 3. Two richness hotspots in Hainan are subjected to the Hainan element, and another two hotspots in Yunnan also belong to the Yunnan- Guizhou Plateau element. I hypothesized that the spatially overlapping degree between areas of endemism and biodiversity hotspots is not same for different clades. For those clades in which both widespread and geographically restricted species are abundant, the overlapping degree may not be high. For example, amphibians (Chen and Bi, 2007) and reptiles of my present study at regional level; amphibians, birds, reptiles and mammals at global level (Orme et al., 2005; Lamoreux et al., 2006). However, the overlapping degree between richness hotspots and areas of endemism becomes higher for clades with more geographically restricted species but fewer widespread species, such as aphids (Huang et al., 2008). I believed that most low dispersal-ability insect and plant clades should have similar patterns, although more examinations still need to be done in the future. 3.6 Improvement of biotic element analysis In the case of my study, the primary analysis identified nine elements, which contained two geographically restricted ones. The remaining seven elements were fully widespread, and they provided little information of testing vicariance model, indicating that dispersal is a common biogeographic event for reptiles in the region. In order to detect other geographically restricted biotic elements, I subsequently carried out a second biotic

7 CHEN YH: Biotic elements of reptilians 455 element analysis without considering species and areas that have been identified in the two geographically restricted elements. Consequently, another geographically restricted element-hainan element with 33 noise species emerged. A third round of biotic element analysis was implemented so as to another geographically restricted element-yunnan element with no noise species assigned. As such, the iteration of biotic element analysis could be stopped. The null model cooperating spatial autocorrelation analysis was used in Prabclust package. To make the analysis more robust, one needs an informative data set. For those seldom filled data sets, the null hypothesis would be rejected rarely. The reason is that there are too much geographically restricted species in the data set, which would reduce the clustering degree of distributional areas (Hausdorf and Hennig, 2006). At the meantime, the full filled data sets are needed to avoid as well. This kind of data sets will contain tremendous widespread species across the areas, which will reduce the possibility of generating geographically restricted elements. This could be proven in the primary analysis of my present study, where only 32 species contributing to two geographically restricted elements and others forming widespread elements, making the vicariance analysis becomes less meaningful. In addition, I argue that the criteria for determining neighboring regions in the program are not fully accurate, which make the spatial autocorrelation of the data possibly overestimated. Some regions/grid cells that are actually not adjacent are grouped as neighbors in the function geo2neighbor. It is suggested to use the nearby eight neighboring grid cells in preparing a neighborhood list. This simple method would approach the true area spatial relationships comparing to the simple cut-off criterion in the package. The distance test ratio T between the 25% smallest and largest distance for testing clustering of distributional areas has a pitfall needed to discuss. As stated in Hennig and Hausdorf (Hennig and Hausdorf, 2004) the ratio is the most conservative. It depends on top largest ranges and top smallest ranges, which will reduce the significance of clustering in null model simulation (unpublished results) if the data set is composed of most species with small ranges uniformly or with large ranges uniformly, inasmuch in this matter the ratio T becomes close to the maximal limit (value is 1). 3.7 Implications for further studies My study applied biotic element analysis (Hausdorf and Hennig, 2003, 2004, 2006) to detect biogeographically important areas and might represent the primary studies focused on areas of endemism in East Asia (Liang, 2003; Xu et al., 2003; Xu, 2005; Chen and Bi, 2007; Chen, 2009, 2008; Huang et al., 2008). Although the debate on the discrepancies of the biotic elements and areas of endemism is still open (Casagranda et al., 2012), we still regarded that areas of endemism and biotic elements of species distribution should have some congruent aspects and biotic element analysis has the attempt to identify important areas for historical biogeography and endemism [see the application of biotic element analysis on identifying endemic areas in previous studies: Nogueira et al. (2011); Carvalho et al. (2011); Hausdorf and Hennig (2006); Wronski and Hausdorf (2008) and Hausdorf and Henning (2010)]. There are some questions needed to address in further studies: Does the Yunnan-Guizhou Plateau constitute only one biotic element as showed in my study? The solution might rely on more sufficient distributional data. Besides, are there any more geographically restricted biotic elements in other parts of China? For example, the northwestern xeric ranges, other areas of the vast Qinghai-Tibet Plateau (Huang et al., 2008) and the northeastern cold regions. I believed that there must be other significant elements in these areas. Due to the limitation of the data set, they could not be identified in this contribution but will certainly be uncovered in the near future. At last, from technical perspectives, our current study has some limitations given that we don t have a phylogenetic relationship of species in hand. The definition of closely related species based on taxonomic classification could not accurately reflect the phylogenetic relatedness of species. This is because species within a genus is not a guarantee that they could form a monophyletic group based on DNA sequence information. As such, the application of phylogenetic relationship of species to define closely related species would contribute new insights for evaluating and identifying biotic elements. Acknowledgements This work was partially supported by a UBC scholarship. I thank five reviewers for their constructive comments on the earlier versions of my manuscript, and Axel S. Wang for his polishing the language. References Association CWC, Atlas of Reptiles of China., Zhengzhou: Henan Science and Technology Press. Baez J, Real R, Vargas J, Flores-Moya A, Chorotypes of

8 456 Current Zoology Vol. 59 No. 4 seaweeds from the western Meditterranean Sea and the Adriatic Sea: An analysis based on the genera Audouinella (Rhodophyta), Cystoseira (Phaeophyceae) and Cladophora (Chlorophyta). Phycological Research 53: Cabrero-Sanudo F, Lobo J, Biogeography of Aphodiinae dung beetles based on the regional composition and distribution patterns of genera. Journal of Biogeography 36: Carvalho S, Brito J, Crespo E, Possingham H, Incorporating evolutionary processes into conservation planning using species distribution data: A case study with the western Mediterranean herpetofauna. Diversity and Distributions 17: Casagranda M, Arias J, Goloboff P, Szumik C, Taher LM et al., Proximity, interpenetration, and sympatry networks: A reply to Dos Santos et al.. Systematic Biology 58: Casagranda M, Taher L, Szumik C, Endemicity analysis, parsimony and biotic elements: A formal comparison using hypothetical distributions. Cladistics 28: Chen Y, Bi J, Biogeography and hotspots of amphibian species of China: Implications to reserve selection and conservation. Current Science 92: Chen YH, Avian biogeography and conservation on Hainan Island, China. Zoological Science 25: Chen YH, 2009a. Combining the species-area-habitat relationship and environmental cluster analysis to set conservation priorities: A study in the Zhoushan Archipelago, China. Conservation Biology 23: Chen YH, 2009b. Distribution patterns and faunal characteristic of mammals on Hainan Island of China. Folia Zoologica 58: Hausdorf B, Units in biogeography. Systematic Biology 51: Hausdorf B, Hennig C, Biogeographical tests of the vicariance model in Mediterranean land snails. Journal of Biogeography 33: Hausdorf B, Hennig C, Biotic element analysis in biogeography. Systematic Biology 52: Hausdorf B, Hennig C, Does vicariance shape biotas? Biogeographical tests of the vicariance model in the north-west European land snail fauna. Journal of Biogeography 31: Hausdorf B, Henning C, Species delimitation using dominant and codominant multilocus markers. Systematic Biology 59: Hennig C, Hausdorf B, Distance-based parametric bootstrap tests for clustering of species ranges. Computational Statistics and Data Analysis 45: Holder K, Montgomerie R, Friesen V, A test of the glacial refugium hypothesis using patterns of mitochondrial and nuclear DNA sequence variation in rock ptarmign Lagopus mutus. Evolution 53: Huang X, Lei F, Qiao G, Areas of endemism and patterns of diversity for aphids of the Qinghai-Tibetan Plateau and the Himalayas. Journal of Biogeography 35: Lamoreux J, Morrison J, Ricketts T, Olson D, Dinerstein E et al., Global tests of biodiversity concordance and the importance of endemism. Nature 440: Li J, Fang X, The uplift of the Qinghai-Xizang Plateau and climate change. Chinese Science Bulletin 43: Liang A, Zoogeography of the spittlebug superfamily Cercopoidea (Hemiptera) in Southern Tibet and the nearby areas. Acta Zootaxonomica Sinica 28: Linder H, On areas of endemism, with an example from the African Restionaceae. Systematic Biology 50: Marquez A, Real R, Vargas J, Salvo A, On identifying common distribution patterns and their causal factors: A probabilistic method applied to pteridophytes in the Iberian Peninsula. Journal of Biogeography 24: McCoy E, Bell S, Walters K, Identifying biotic boundaries along environmental gradients. Ecology 67: Moline P, Linder H, Input data, analytical methods and biogeography of Elegia (Restionaceae). Journal of Biogeography 22: Morrone J, On the identification of areas of endemism. Systematic Biology 43: Morrone J, Crisci J, Historical Biogeography: Introduction to methods. Annual Review of Ecology and Systematics 26: Myers N, Mittermeier R, Mittermeier C, Da Fonseca G, Kent J, Biodiversity hotspots for conservation priorities. Nature 403: Nogueira C, Ribeiro S, Costa G, Colli G, Vicariance and endemism in a Neotropical savanna hotspot: Distribution patterns of Cerrado squamate reptiles. Journal of Biogeography 38: Orme C, Davies R, Burgess M, Eigenbrod F, Pickup N et al., Global hotspots of species richness are not congruent with endemism or threat. Nature 436: R Development Core Team, R: A Language and Environment for Statistical Computing, Vienna, Austria. ISBN , URL Rosen B, From fossils to earth history: Applied historical biogeography. In: Myers A, Giller P ed. Analytical Biogeography. Chapman and Hall, London, Shen L, Chen X, Zhang X, Li YY, Fu C et al., Genetic variation of Ginkgo biloba L. (Ginkgoaceae) based on cpdna PCR-RFLPs: Inference of glacial refugia. Heredity 94: Wan T, The Tectonics of China: Data, Maps and Evolution. Beijing, Dordrecht Heidelberg, London and New York: Higher Education Press and Springer. Wang C, Zhao X, Liu Z, Lippert P, Graham S et al., Constraints on the early uplift history of the Tibetan Plateau. Proceedings of the National Academy of Science of the United States of America 105: Williams P, Gibbons D, Margules C, Rebelo A, Humphries C et al., A comparison of richness hotspots, rarity hotspots, and complementary areas for conserving diversity of British birds. Conservation Biology 10: Wronski T, Hausdorf B, Distribution patterns of land snails in Ugandan rain forests support the existence of Pleistocene forest refugia. Journal of Biogeography 35: Xu S, The distribution and area of endemism of Catantopidae grasshopper species endemic to China. Acta Zoologica Sinica 51: Xu S, Zheng Z, Li H, Cladistic biogeography of four grasshopper genera (Catantopidae: Orthoptera) from the South of China. Zoological Research 24:

9 CHEN YH: Biotic elements of reptilians 457 Zhang M, Zong Y, Ma J, Fauna Sinica: Reptilia. Vol. 1: General Accounts of Reptilia, Testudoformes and Crocodiliformes. Beijing: Science Press. Zhang R, Zoogeography of China. Beijing: Science Press. Zhao E, Huang M, Zong Y, Fauna Sinica: Reptilia. Vol. 3. Squamata: Serpentes. Beijing: Science Press. Zhao Ermi, Fauna Sinica: Reptilia. Vol. 2. Squamata: Lacertilia. Beijing: Science Press. Zhao J, Physical Geography of China. Beijing: Advanced Education Press

Biotic Element Analysis in Biogeography

Biotic Element Analysis in Biogeography Syst. Biol. 52(5):717 723, 2003 Copyright c Society of Systematic Biologists ISSN: 1063-5157 print / 1076-836X online DOI: 10.1080/10635150390235584 Biotic Element Analysis in Biogeography BERNHARD HAUSDORF

More information

Geography of Evolution

Geography of Evolution Geography of Evolution Biogeography - the study of the geographic distribution of organisms. The current distribution of organisms can be explained by historical events and current climatic patterns. Darwin

More information

Biogeography. An ecological and evolutionary approach SEVENTH EDITION. C. Barry Cox MA, PhD, DSc and Peter D. Moore PhD

Biogeography. An ecological and evolutionary approach SEVENTH EDITION. C. Barry Cox MA, PhD, DSc and Peter D. Moore PhD Biogeography An ecological and evolutionary approach C. Barry Cox MA, PhD, DSc and Peter D. Moore PhD Division of Life Sciences, King's College London, Fmnklin-Wilkins Building, Stamford Street, London

More information

,...,.,.,,.,...,.,...,...,.,.,...

,...,.,.,,.,...,.,...,...,.,.,... Areas of Endemism The definitions and criteria for areas of endemism are complex issues (Linder 2001; Morrone 1994b; Platnick 1991; Szumik et al. 2002; Viloria 2005). There are severa1 definitions of areas

More information

Fields connected to Phylogeography Microevolutionary disciplines Ethology Demography Population genetics

Fields connected to Phylogeography Microevolutionary disciplines Ethology Demography Population genetics Stephen A. Roussos Fields connected to Phylogeography Microevolutionary disciplines Ethology Demography Population genetics Macrevolutionary disciplines Historical geography Paleontology Phylogenetic biology

More information

GIS Applications to Museum Specimens

GIS Applications to Museum Specimens GIS Applications to Museum Specimens Joseph Grinnell (1877 1939) At this point I wish to emphasize what I believe will ultimately prove to be the greatest value of our museum. This value will not, however,

More information

Spheres of Life. Ecology. Chapter 52. Impact of Ecology as a Science. Ecology. Biotic Factors Competitors Predators / Parasites Food sources

Spheres of Life. Ecology. Chapter 52. Impact of Ecology as a Science. Ecology. Biotic Factors Competitors Predators / Parasites Food sources "Look again at that dot... That's here. That's home. That's us. On it everyone you love, everyone you know, everyone you ever heard of, every human being who ever was, lived out their lives. Ecology Chapter

More information

EFFECTS OF TAXONOMIC GROUPS AND GEOGRAPHIC SCALE ON PATTERNS OF NESTEDNESS

EFFECTS OF TAXONOMIC GROUPS AND GEOGRAPHIC SCALE ON PATTERNS OF NESTEDNESS EFFECTS OF TAXONOMIC GROUPS AND GEOGRAPHIC SCALE ON PATTERNS OF NESTEDNESS SFENTHOURAKIS Spyros, GIOKAS Sinos & LEGAKIS Anastasios Zoological Museum, Department of Biology, University of Athens, Greece

More information

Biogeography expands:

Biogeography expands: Biogeography expands: Phylogeography Ecobiogeography Due to advances in DNA sequencing and fingerprinting methods, historical biogeography has recently begun to integrate relationships of populations within

More information

Biodiversity: Facts and figures (tables from the report)

Biodiversity: Facts and figures (tables from the report) Vascular plant * Country Number Australia 15,638 Brazil 56,215 China 8,200 Colombia 32,200 Congo, Democratic Republic 11,007 Costa Rica 12,119 Ecuador 19,362 India 18,664 Indonesia 29,375 Madagascar 9,505

More information

Conceptually, we define species as evolutionary units :

Conceptually, we define species as evolutionary units : Bio 1M: Speciation 1 How are species defined? S24.1 (2ndEd S26.1) Conceptually, we define species as evolutionary units : Individuals within a species are evolving together Individuals of different species

More information

EXTINCTION CALCULATING RATES OF ORIGINATION AND EXTINCTION. α = origination rate Ω = extinction rate

EXTINCTION CALCULATING RATES OF ORIGINATION AND EXTINCTION. α = origination rate Ω = extinction rate EXTINCTION CALCULATING RATES OF ORIGINATION AND EXTINCTION α = origination rate Ω = extinction rate 1 SPECIES AND GENERA EXTINCTION CURVES INDICATE THAT MOST SPECIES ONLY PERSIST FOR A FEW MILLION YEARS.

More information

Species diversification in space: biogeographic patterns

Species diversification in space: biogeographic patterns Species diversification in space: biogeographic patterns Outline Endemism and cosmopolitanism Disjunctions Biogeographic regions Barriers and interchanges Divergence and convergence Biogeographic patterns

More information

The California Hotspots Project: I.

The California Hotspots Project: I. The California Hotspots Project: I. Identifying regions of rapid diversification of mammals Ed Davis, M. Koo, C. Conroy, J. Patton & C. Moritz Museum of Vertebrate Zoology, UC Berkeley *Funded by Resources

More information

Specific gravity field and deep crustal structure of the Himalayas east structural knot

Specific gravity field and deep crustal structure of the Himalayas east structural knot 49 4 2006 7 CHINESE JOURNAL OF GEOPHYSICS Vol. 49, No. 4 Jul., 2006,,.., 2006, 49 (4) :1045 1052 Teng J W, Wang Q S, Wang GJ, et al. Specific gravity field and deep crustal structure of the Himalayas east

More information

ECOLOGICAL PLANT GEOGRAPHY

ECOLOGICAL PLANT GEOGRAPHY Biology 561 MWF 11:15 12:05 Spring 2018 128 Wilson Hall Robert K. Peet ECOLOGICAL PLANT GEOGRAPHY Objectives: This is a course in the geography of plant biodiversity, vegetation and ecological processes.

More information

A Preliminary Analysis of the Relationship between Precipitation Variation Trends and Altitude in China

A Preliminary Analysis of the Relationship between Precipitation Variation Trends and Altitude in China ATMOSPHERIC AND OCEANIC SCIENCE LETTERS, 2011, VOL. 4, NO. 1, 41 46 A Preliminary Analysis of the Relationship between Precipitation Variation Trends and Altitude in China YANG Qing 1, 2, MA Zhu-Guo 1,

More information

Geographical location and climatic condition of the

Geographical location and climatic condition of the Geographical location and climatic condition of the study sites North eastern region of India is comprised of eight states namely; Arunachal Pradesh, Assam, Manipur, Meghalaya, Mizoram, Nagaland, Sikkim

More information

PCB6675C, BOT6935, ZOO6927 Evolutionary Biogeography Spring 2014

PCB6675C, BOT6935, ZOO6927 Evolutionary Biogeography Spring 2014 PCB6675C, BOT6935, ZOO6927 Evolutionary Biogeography Spring 2014 Credits: 3 Schedule: Wednesdays and Fridays, 4 th & 5 th Period (10:40 am - 12:35 pm) Location: Carr 221 Instructors Dr. Nico Cellinese

More information

World Geography Chapter 3

World Geography Chapter 3 World Geography Chapter 3 Section 1 A. Introduction a. Weather b. Climate c. Both weather and climate are influenced by i. direct sunlight. ii. iii. iv. the features of the earth s surface. B. The Greenhouse

More information

Reconstructing the history of lineages

Reconstructing the history of lineages Reconstructing the history of lineages Class outline Systematics Phylogenetic systematics Phylogenetic trees and maps Class outline Definitions Systematics Phylogenetic systematics/cladistics Systematics

More information

Zoogeographic Regions. Reflective of the general distribution of energy and richness of food chemistry

Zoogeographic Regions. Reflective of the general distribution of energy and richness of food chemistry Terrestrial Flora & Fauna Part II In short, the animal and vegetable lines, diverging widely above, join below in a loop. 1 Asa Gray Zoogeographic Regions Reflective of the general distribution of energy

More information

Earth History. What is the Earth s time scale? Geological time Scale. Pre-Cambrian. FOUR Eras

Earth History. What is the Earth s time scale? Geological time Scale. Pre-Cambrian. FOUR Eras The Earth is 4.6 billion years old! Earth History Mrs. Burkey ESS Cy Creek HS 17-18 If the Earth formed at midnight 6:00 am First life appears 10:00 pm First animals/plants on land 11:59 pm First humans

More information

Class Webpage. Forms of Diversity. biol170/biol170syl.htm

Class Webpage. Forms of Diversity.  biol170/biol170syl.htm Class Webpage http://userwww.sfsu.edu/~efc/classes/ biol170/biol170syl.htm What is an animal? While there are exceptions, five criteria distinguish animals from other life forms. (1)Animals are multicellular,

More information

Biodiversity-Hotspots

Biodiversity-Hotspots GE 2211 Environmental Science and Engineering Unit II Biodiversity-Hotspots M. Subramanian Assistant Professor Department of Chemical Engineering Sri Sivasubramaniya Nadar College of Engineering Kalavakkam

More information

Bryan F.J. Manly and Andrew Merrill Western EcoSystems Technology Inc. Laramie and Cheyenne, Wyoming. Contents. 1. Introduction...

Bryan F.J. Manly and Andrew Merrill Western EcoSystems Technology Inc. Laramie and Cheyenne, Wyoming. Contents. 1. Introduction... Comments on Statistical Aspects of the U.S. Fish and Wildlife Service's Modeling Framework for the Proposed Revision of Critical Habitat for the Northern Spotted Owl. Bryan F.J. Manly and Andrew Merrill

More information

Analysis of the Tourism Locations of Chinese Provinces and Autonomous Regions: An Analysis Based on Cities

Analysis of the Tourism Locations of Chinese Provinces and Autonomous Regions: An Analysis Based on Cities Chinese Journal of Urban and Environmental Studies Vol. 2, No. 1 (2014) 1450004 (9 pages) World Scientific Publishing Company DOI: 10.1142/S2345748114500043 Analysis of the Tourism Locations of Chinese

More information

Study on the feature of surface rupture zone of the west of Kunlunshan pass earthquake ( M S 811) with high spatial resolution satellite images

Study on the feature of surface rupture zone of the west of Kunlunshan pass earthquake ( M S 811) with high spatial resolution satellite images 48 2 2005 3 CHINESE JOURNAL OF GEOPHYSICS Vol. 48, No. 2 Mar., 2005,,. M S 811.,2005,48 (2) :321 326 Shan X J, Li J H, Ma C. Study on the feature of surface rupture zone of the West of Kunlunshan Pass

More information

Development Team. Department of Zoology, University of Delhi. Department of Zoology, University of Delhi

Development Team. Department of Zoology, University of Delhi. Department of Zoology, University of Delhi Paper No. : 12 Module : 18 diversity index, abundance, species richness, vertical and horizontal Development Team Principal Investigator: Co-Principal Investigator: Paper Coordinator: Content Writer: Content

More information

The History of Life on Earth

The History of Life on Earth 8 The History of Life on Earth lesson 1 Geologic Time and Mass Extinctions Grade Seven Science Content Standard. 4.b. Students know the history of life on Earth has been disrupted by major catastrophic

More information

Physical Geography. Ariel view of the Amazon Rainforest. A Look at the Seven Continents

Physical Geography. Ariel view of the Amazon Rainforest. A Look at the Seven Continents Physical Geography In this unit you will learn about general physical geography. The study of the Earth s surface features provides the setting for the human-environmental interactions and for the human

More information

PLATE TECTONICS THEORY

PLATE TECTONICS THEORY PLATE TECTONICS THEORY Continental drift Sea floor spreading CONTINENTAL DRIFT CONTINENTAL DRIFT 1. The fitness of continents and Continental Reconstruction Earth ~200 million years ago 1.1 Geometrical

More information

Plan of Development Mountain Valley Pipeline Project. APPENDIX P Plan for Unanticipated Discovery of Paleontological Resources

Plan of Development Mountain Valley Pipeline Project. APPENDIX P Plan for Unanticipated Discovery of Paleontological Resources APPENDIX P Plan for Unanticipated Discovery of Paleontological Resources Appendix P Plan for Unanticipated Discovery of Paleontological Resources Prepared by: TABLE OF CONTENTS 1.0 INTRODUCTION... 1 1.1

More information

3. The diagram below shows how scientists think some of Earth's continents were joined together in the geologic past.

3. The diagram below shows how scientists think some of Earth's continents were joined together in the geologic past. 1. The map below shows the present-day locations of South America and Africa. Remains of Mesosaurus, an extinct freshwater reptile, have been found in similarly aged bedrock formed from lake sediments

More information

Tropical Rainforests in the Pleistocene

Tropical Rainforests in the Pleistocene Tropical Rainforests in the Pleistocene tropics stable during Pleistocene? 1 C temperature drop based on 1976 CLIMAP study of warm vs. cold loving forams (vs. 10 C in North Atlantic) Paleothermometers

More information

Tropical Rainforests in the Pleistocene

Tropical Rainforests in the Pleistocene Tropical Rainforests in the Pleistocene tropics stable during Pleistocene? 1 C temperature drop based on 1976 CLIMAP study of warm vs. cold loving forams (vs. 10 C in North Atlantic) Pollen analysis of

More information

Name. Ecology & Evolutionary Biology 2245/2245W Exam 2 1 March 2014

Name. Ecology & Evolutionary Biology 2245/2245W Exam 2 1 March 2014 Name 1 Ecology & Evolutionary Biology 2245/2245W Exam 2 1 March 2014 1. Use the following matrix of nucleotide sequence data and the corresponding tree to answer questions a. through h. below. (16 points)

More information

Temperature and precipitation fluctuations since 1600 A.D. provided by the Dunde Ice Cap, China

Temperature and precipitation fluctuations since 1600 A.D. provided by the Dunde Ice Cap, China Gladers-Ocean-Atmosphen! lnl6aaions (Proceedings of the International Symposium held at St Petersburg, September 199). IAHS Publ. no. 28, 1991. Temperature and precipitation fluctuations since 16 A.D.

More information

Speciation. Today s OUTLINE: Mechanisms of Speciation. Mechanisms of Speciation. Geographic Models of speciation. (1) Mechanisms of Speciation

Speciation. Today s OUTLINE: Mechanisms of Speciation. Mechanisms of Speciation. Geographic Models of speciation. (1) Mechanisms of Speciation Speciation Today s OUTLINE: (1) Geographic Mechanisms of Speciation (What circumstances lead to the formation of new species?) (2) Species Concepts (How are Species Defined?) Mechanisms of Speciation Last

More information

Genetic diversity of beech in Greece

Genetic diversity of beech in Greece Genetic diversity of beech in Greece A.C. Papageorgiou (1), I. Tsiripidis (2), S. Hatziskakis (1) Democritus University of Thrace Forest Genetics Laboratory Orestiada, Greece (2) Aristotle University of

More information

Evolution. Darwin s Voyage

Evolution. Darwin s Voyage Evolution Darwin s Voyage Charles Darwin Explorer on an observation trip to the Galapagos Islands. He set sail on the HMS Beagle in 1858 from England on a 5 year trip. He was a naturalist (a person who

More information

UoN, CAS, DBSC BIOL102 lecture notes by: Dr. Mustafa A. Mansi. The Phylogenetic Systematics (Phylogeny and Systematics)

UoN, CAS, DBSC BIOL102 lecture notes by: Dr. Mustafa A. Mansi. The Phylogenetic Systematics (Phylogeny and Systematics) - Phylogeny? - Systematics? The Phylogenetic Systematics (Phylogeny and Systematics) - Phylogenetic systematics? Connection between phylogeny and classification. - Phylogenetic systematics informs the

More information

Chapter 19 Organizing Information About Species: Taxonomy and Cladistics

Chapter 19 Organizing Information About Species: Taxonomy and Cladistics Chapter 19 Organizing Information About Species: Taxonomy and Cladistics An unexpected family tree. What are the evolutionary relationships among a human, a mushroom, and a tulip? Molecular systematics

More information

Chapter 21 Southwest Asia: Harsh & Arid Lands

Chapter 21 Southwest Asia: Harsh & Arid Lands Name Hour Chapter 21 Southwest Asia: Harsh & Arid Lands Essential Question: How has the physical geography of Asia influenced the development of these regions (i.e. history, population distribution, &

More information

Panama and the Great American Interchange. Reading: Marshall et al. 1982

Panama and the Great American Interchange. Reading: Marshall et al. 1982 Panama and the Great American Interchange Reading: Marshall et al. 1982 Lecture 6 Recap Lars Brundin Lars Brundin What about the general suitability of chironomid midges as indicators in biogeography?

More information

What is the Earth s time scale?

What is the Earth s time scale? Earth History What is the Earth s time scale? The Geological time scale is a record of the life forms and geological events in Earth s history. Scientists developed the time scale by fossils world wide.

More information

Historical Biogeography. Historical Biogeography. Systematics

Historical Biogeography. Historical Biogeography. Systematics Historical Biogeography I. Definitions II. Fossils: problems with fossil record why fossils are important III. Phylogeny IV. Phenetics VI. Phylogenetic Classification Disjunctions debunked: Examples VII.

More information

Copyright McGraw-Hill Education. All rights reserved. No reproduction or distribution without the prior written consent of McGraw-Hill Education

Copyright McGraw-Hill Education. All rights reserved. No reproduction or distribution without the prior written consent of McGraw-Hill Education Copyright McGraw-Hill Education. All rights reserved. No reproduction or distribution without the prior written consent of McGraw-Hill Education Tibetan Plateau and Himalaya -southern Asia 11.00.a VE 10X

More information

Speciation. Today s OUTLINE: Mechanisms of Speciation. Mechanisms of Speciation. Geographic Models of speciation. (1) Mechanisms of Speciation

Speciation. Today s OUTLINE: Mechanisms of Speciation. Mechanisms of Speciation. Geographic Models of speciation. (1) Mechanisms of Speciation Speciation Today s OUTLINE: (1) Geographic Mechanisms of Speciation (What circumstances lead to the formation of new species?) (2) Species Concepts (How are Species Defined?) Mechanisms of Speciation Last

More information

1 The spatial component of evolution

1 The spatial component of evolution 1 The spatial component of evolution Molecular studies have documented high levels of geographic structure in most plant and animal groups and this finding has fundamental implications for the science

More information

On a world basis the 58 known Indiana genera are more closely affiliated

On a world basis the 58 known Indiana genera are more closely affiliated '. Biogeography of Indiana Trichoptera R. D. Waltz and W. P. McCafferty Department of Entomology Purdue University, West Lafayette, Indiana 47907 Introduction The caddisflies constitute one of the largest

More information

Speciation. Today s OUTLINE: Mechanisms of Speciation. Mechanisms of Speciation. Geographic Models of speciation. (1) Mechanisms of Speciation

Speciation. Today s OUTLINE: Mechanisms of Speciation. Mechanisms of Speciation. Geographic Models of speciation. (1) Mechanisms of Speciation Speciation Today s OUTLINE: (1) Geographic Mechanisms of Speciation (What circumstances lead to the formation of new species?) (2) Species Concepts (How are Species Defined?) Mechanisms of Speciation Last

More information

Geography. Programmes of study for Key Stages 1-3

Geography. Programmes of study for Key Stages 1-3 Geography Programmes of study for Key Stages 1-3 February 2013 Contents Purpose of study 3 Aims 3 Attainment targets 3 Subject content 4 Key Stage 1 4 Key Stage 2 5 Key Stage 3 6 2 Purpose of study A high-quality

More information

Units in Biogeography

Units in Biogeography 648 SYSTEMATIC BIOLOGY VOL. 51 Syst. Biol. 51(4):648 652, 2002 DOI: 10.1080/10635150290102320 Units in Biogeography BERNHARD HAUSDORF Zoologisches Institut und Zoologisches Museum der Universität Hamburg,

More information

5 Time Marches On. TAKE A LOOK 1. Identify What kinds of organisms formed the fossils in the picture?

5 Time Marches On. TAKE A LOOK 1. Identify What kinds of organisms formed the fossils in the picture? CHAPTER 6 5 Time Marches On SECTION The Rock and Fossil Record BEFORE YOU READ After you read this section, you should be able to answer these questions: How do geologists measure time? How has life changed

More information

The Tempo of Macroevolution: Patterns of Diversification and Extinction

The Tempo of Macroevolution: Patterns of Diversification and Extinction The Tempo of Macroevolution: Patterns of Diversification and Extinction During the semester we have been consider various aspects parameters associated with biodiversity. Current usage stems from 1980's

More information

Phanerozoic Diversity and Mass Extinctions

Phanerozoic Diversity and Mass Extinctions Phanerozoic Diversity and Mass Extinctions Measuring Diversity John Phillips produced the first estimates of Phanerozoic diversity in 1860, based on the British fossil record Intuitively it seems simple

More information

Lecture 11 Friday, October 21, 2011

Lecture 11 Friday, October 21, 2011 Lecture 11 Friday, October 21, 2011 Phylogenetic tree (phylogeny) Darwin and classification: In the Origin, Darwin said that descent from a common ancestral species could explain why the Linnaean system

More information

Department of Forest Ecosystems and Society, Oregon State University

Department of Forest Ecosystems and Society, Oregon State University July 7, 2018 Prof. Christopher Still Department of Forest Ecosystems and Society, Oregon State University 321 Richardson Hall, Corvallis OR 97331-5752 Dear Prof. Christopher Still, We would like to thank

More information

Welcome! Text: Community Ecology by Peter J. Morin, Blackwell Science ISBN (required) Topics covered: Date Topic Reading

Welcome! Text: Community Ecology by Peter J. Morin, Blackwell Science ISBN (required) Topics covered: Date Topic Reading Welcome! Text: Community Ecology by Peter J. Morin, Blackwell Science ISBN 0-86542-350-4 (required) Topics covered: Date Topic Reading 1 Sept Syllabus, project, Ch1, Ch2 Communities 8 Sept Competition

More information

Integrative Biology 200 "PRINCIPLES OF PHYLOGENETICS" Spring 2018 University of California, Berkeley

Integrative Biology 200 PRINCIPLES OF PHYLOGENETICS Spring 2018 University of California, Berkeley Integrative Biology 200 "PRINCIPLES OF PHYLOGENETICS" Spring 2018 University of California, Berkeley B.D. Mishler Feb. 14, 2018. Phylogenetic trees VI: Dating in the 21st century: clocks, & calibrations;

More information

Lecture Outlines PowerPoint. Chapter 12 Earth Science 11e Tarbuck/Lutgens

Lecture Outlines PowerPoint. Chapter 12 Earth Science 11e Tarbuck/Lutgens Lecture Outlines PowerPoint Chapter 12 Earth Science 11e Tarbuck/Lutgens 2006 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors

More information

Range of Opportunities

Range of Opportunities Geograhy Curriculum Cropwell Bishop Primary School Range of Opportunities Year 1 Year 2 Year 3 Year 4 Year 5 Year 6 All Key Stage 1 Key Stage 2 Investigate the countries and capitals of the United Kingdom.

More information

8/23/2014. Phylogeny and the Tree of Life

8/23/2014. Phylogeny and the Tree of Life Phylogeny and the Tree of Life Chapter 26 Objectives Explain the following characteristics of the Linnaean system of classification: a. binomial nomenclature b. hierarchical classification List the major

More information

Major geological events fit into a timeline, beginning with the formation of the Earth

Major geological events fit into a timeline, beginning with the formation of the Earth Chapter 4 Major geological events fit into a timeline, beginning with the formation of the Earth 4.1 The origin and development of life William Smith was a canal engineer who supervised the excavation

More information

IB 200B Phylogenetics 21 April II. Vicariance Biogeography

IB 200B Phylogenetics 21 April II. Vicariance Biogeography II. Vicariance Biogeography The breakthrough in the application of cladistic reasoning to biogeography was led by the ichthyologists Gary Nelson and Donn Rosen at the American Museum of Natural History

More information

Geologic Time. The Cenozoic Era. 7. Mammals evolved after dinosaurs became extinct.

Geologic Time. The Cenozoic Era. 7. Mammals evolved after dinosaurs became extinct. Geologic Time The Cenozoic Era Key Concepts What major geologic events occurred during the Cenozoic era? What does fossil evidence reveal about the Cenozoic era? What do you think? Read the two statements

More information

AP Environmental Science I. Unit 1-2: Biodiversity & Evolution

AP Environmental Science I. Unit 1-2: Biodiversity & Evolution NOTE/STUDY GUIDE: Unit 1-2, Biodiversity & Evolution AP Environmental Science I, Mr. Doc Miller, M.Ed. North Central High School Name: ID#: NORTH CENTRAL HIGH SCHOOL NOTE & STUDY GUIDE AP Environmental

More information

Chapter 19. History of Life on Earth

Chapter 19. History of Life on Earth Chapter 19 History of Life on Earth Adapted from Holt Biology 2008 Chapter 19 Section 3: Evolution of Life Key Vocabulary Terms Adapted from Holt Biology 2008 Cyanobacteria Photosynthetic prokaryotes Adapted

More information

Trends of Tropospheric Ozone over China Based on Satellite Data ( )

Trends of Tropospheric Ozone over China Based on Satellite Data ( ) ADVANCES IN CLIMATE CHANGE RESEARCH 2(1): 43 48, 2011 www.climatechange.cn DOI: 10.3724/SP.J.1248.2011.00043 ARTICLE Trends of Tropospheric Ozone over China Based on Satellite Data (1979 2005) Xiaobin

More information

Evolution Problem Drill 09: The Tree of Life

Evolution Problem Drill 09: The Tree of Life Evolution Problem Drill 09: The Tree of Life Question No. 1 of 10 Question 1. The age of the Earth is estimated to be about 4.0 to 4.5 billion years old. All of the following methods may be used to estimate

More information

Georgia Performance Standards for Urban Watch Restoration Field Trips

Georgia Performance Standards for Urban Watch Restoration Field Trips Georgia Performance Standards for Field Trips 6 th grade S6E3. Students will recognize the significant role of water in earth processes. a. Explain that a large portion of the Earth s surface is water,

More information

Dr. Amira A. AL-Hosary

Dr. Amira A. AL-Hosary Phylogenetic analysis Amira A. AL-Hosary PhD of infectious diseases Department of Animal Medicine (Infectious Diseases) Faculty of Veterinary Medicine Assiut University-Egypt Phylogenetic Basics: Biological

More information

2008 SIVECO Romania. All Rights Reserved. Geography. AeL econtent Catalogue

2008 SIVECO Romania. All Rights Reserved. Geography. AeL econtent Catalogue 2008 SIVECO Romania. All Rights Reserved. Geography AeL econtent Catalogue The Earth's Movements Recommended for two hours of teaching. AeL Code: 352. 2. The Earth Rotation Movement in 24 hours 3. The

More information

Evolution Evidence of Change

Evolution Evidence of Change 6 Evolution Evidence of Change lesson 3 Evolution and Plate Tectonics Grade Seven Science Content Standard. 4.f. Students know how movements of Earth's continental and oceanic plates through time, with

More information

Week: 4 5 Dates: 9/8 9/12 Unit: Plate Tectonics

Week: 4 5 Dates: 9/8 9/12 Unit: Plate Tectonics clementaged.weebly.com Name: ODD Period: Week: 4 5 Dates: 9/8 9/12 Unit: Plate Tectonics Monday Tuesday Wednesday Thursday Friday 7 No School 8 E 9 O *Vocabulary *Frayer Vocab *Continental Drift Notes

More information

Research on the Spatial Distribution Characteristics of b-value in Southwest Yunnan

Research on the Spatial Distribution Characteristics of b-value in Southwest Yunnan International Symposium on Computers & Informatics (ISCI 2015) Research on the Spatial Distribution Characteristics of b-value in Southwest Yunnan XIE ZHUOJUAN1, a, LU YUEJUN1, b 1Institute of Crustal

More information

Spring th Grade

Spring th Grade Spring 2015 8 th Grade The geologic time scale is a record of the major events and diversity of life forms present in Earth s history. The geologic time scale began when Earth was formed and goes on until

More information

East Asia. Mongolia, China, Taiwan, the Koreas, and Japan

East Asia. Mongolia, China, Taiwan, the Koreas, and Japan East Asia Mongolia, China, Taiwan, the Koreas, and Japan Major Geographic Characteristics of East Asia East Asia is the most populous region in the world China is the most populous country, and the oldest

More information

Mount Everest and the Gobi Desert

Mount Everest and the Gobi Desert Mount Everest and the Gobi Desert 1 Mount Everest is part of the mountain chain known as the Himalaya. Adventurers from all over the world come to try to climb it. Mount Everest is the highest mountain

More information

Lecture 11- Populations/Species. Chapters 18 & 19 - Population growth and regulation - Focus on many local/regional examples

Lecture 11- Populations/Species. Chapters 18 & 19 - Population growth and regulation - Focus on many local/regional examples Lecture 11- Populations/Species Chapters 18 & 19 - Population growth and regulation - Focus on many local/regional examples Why Study Birds? From DNT 11-6-2007 Causes of the Decline Temperate? Tropical?

More information

How do we learn about ancient life? Fossil- a trace or imprint of a living thing that is preserved by geological processes.

How do we learn about ancient life? Fossil- a trace or imprint of a living thing that is preserved by geological processes. Unit 1B Lesson 4 History of Life on Earth How do we learn about ancient life? Paleontologists scientists that studies fossils Fossil- a trace or imprint of a living thing that is preserved by geological

More information

Circulation in the South China Sea in summer of 1998

Circulation in the South China Sea in summer of 1998 Circulation in the South China Sea in summer of 1998 LIU Yonggang, YUAN Yaochu, SU Jilan & JIANG Jingzhong Second Institute of Oceanography, State Oceanic Administration (SOA), Hangzhou 310012, China;

More information

South, Southeast, and East Asia. Physical Geography

South, Southeast, and East Asia. Physical Geography South, Southeast, and East Asia Physical Geography Mountains v Mountains are important in Asia because they influence: A. Population patterns B. Movement of people and goods C. Climate Mountains v The

More information

Tropical Moist Rainforest

Tropical Moist Rainforest Tropical or Lowlatitude Climates: Controlled by equatorial tropical air masses Tropical Moist Rainforest Rainfall is heavy in all months - more than 250 cm. (100 in.). Common temperatures of 27 C (80 F)

More information

Mass Extinctions &Their Consequences

Mass Extinctions &Their Consequences Mass Extinctions &Their Consequences Microevolution and macroevolution Microevolution: evolution occurring within populations p Adaptive and neutral changes in allele frequencies Macroevolution: evolution

More information

BIODIVERSITY PROSPECTING

BIODIVERSITY PROSPECTING BIODIVERSITY PROSPECTING LECTURE OUTLINE The topic Biodiversity Prospecting will be divided in three lectures with the following approaches: Biodiversity Prospecting Definitions and Concepts Biodiversity

More information

History of life on Earth Mass Extinctions.

History of life on Earth Mass Extinctions. History of life on Earth Mass Extinctions. Agenda or Summary Layout A summary of the topics discussed 1 2 3 4 Explanation of Mass extinctions The five major mass extinctions Two particular extinctions

More information

Mass Extinctions &Their Consequences

Mass Extinctions &Their Consequences Mass Extinctions &Their Consequences Taxonomic diversity of skeletonized marine animal families during the Phanerozoic Spindle diagram of family diversification/extinction PNAS 1994. 91:6758-6763. Background

More information

Sec$on 1: Geography and Early China. How does China s geography affect the culture?

Sec$on 1: Geography and Early China. How does China s geography affect the culture? Sec$on 1: Geography and Early China How does China s geography affect the culture? Con$nents of the World Label the continents. Where is China located? Where is China located? In your groups, begin filling

More information

Community phylogenetics review/quiz

Community phylogenetics review/quiz Community phylogenetics review/quiz A. This pattern represents and is a consequent of. Most likely to observe this at phylogenetic scales. B. This pattern represents and is a consequent of. Most likely

More information

Jihong Huang 1,2, Bin Chen 1,2,3, Canran Liu 4, Jiangshan Lai 1, Jinlong Zhang 1 and Keping Ma 1 *

Jihong Huang 1,2, Bin Chen 1,2,3, Canran Liu 4, Jiangshan Lai 1, Jinlong Zhang 1 and Keping Ma 1 * Diversity and Distributions, (Diversity Distrib.) (2011) 1 16 A Journal of Conservation Biogeography BIODIVERSITY RESEARCH 1 State Key Laboratory of Vegetation and Environmental Change, Institute of Botany,

More information

GLOBAL CLIMATES FOCUS

GLOBAL CLIMATES FOCUS which you will learn more about in Chapter 6. Refer to the climate map and chart on pages 28-29 as you read the rest of this chapter. FOCUS GLOBAL CLIMATES What are the major influences on climate? Where

More information

DISTRIBUTION AND DIURNAL VARIATION OF WARM-SEASON SHORT-DURATION HEAVY RAINFALL IN RELATION TO THE MCSS IN CHINA

DISTRIBUTION AND DIURNAL VARIATION OF WARM-SEASON SHORT-DURATION HEAVY RAINFALL IN RELATION TO THE MCSS IN CHINA 3 DISTRIBUTION AND DIURNAL VARIATION OF WARM-SEASON SHORT-DURATION HEAVY RAINFALL IN RELATION TO THE MCSS IN CHINA Jiong Chen 1, Yongguang Zheng 1*, Xiaoling Zhang 1, Peijun Zhu 2 1 National Meteorological

More information

COOLING DRYING 19 4 CT WT CT AR. mean global temperature levels of aridity latitudinal stratification have all changed appreciably

COOLING DRYING 19 4 CT WT CT AR. mean global temperature levels of aridity latitudinal stratification have all changed appreciably as we have seen. BIOMES are the biota's adaptive response to earth's climate zones but climate too has a history - - it has evolved through time mean global temperature levels of aridity latitudinal stratification

More information

Chapter 8. Biogeographic Processes. Upon completion of this chapter the student will be able to:

Chapter 8. Biogeographic Processes. Upon completion of this chapter the student will be able to: Chapter 8 Biogeographic Processes Chapter Objectives Upon completion of this chapter the student will be able to: 1. Define the terms ecosystem, habitat, ecological niche, and community. 2. Outline how

More information

Overview. How many species are there? Major patterns of diversity Causes of these patterns Conserving biodiversity

Overview. How many species are there? Major patterns of diversity Causes of these patterns Conserving biodiversity Overview How many species are there? Major patterns of diversity Causes of these patterns Conserving biodiversity Biodiversity The variability among living organisms from all sources, including, inter

More information

Alligator mississippiensis.

Alligator mississippiensis. Alligator mississippiensis http://www.birdsasart.com/bn201.htm Core Case Study: Why Should We Care about the American Alligator? Largest reptile in North America 1930s: Hunters and poachers Importance

More information

Head of College Scholars List Scheme. Summer Studentship. Report Form

Head of College Scholars List Scheme. Summer Studentship. Report Form Head of College Scholars List Scheme Summer Studentship Report Form This report should be completed by the student with his/her project supervisor. It should summarise the work undertaken during the project

More information

2 Georgia: Its Heritage and Its Promise

2 Georgia: Its Heritage and Its Promise TERMS region, erosion, fault, elevation, Fall Line, aquifer, marsh, climate, weather, precipitation, drought, tornado, hurricane, wetland, estuary, barrier island, swamp PLACES Appalachian Mountains, Appalachian

More information