A refined ammonite biostratigraphy for the Middleand Upper Carixian (Ibex and Davoei Zones,Lower Jurassic) in North-West Europe and stratigraphical details of the Carixian-Domerian boundary

A refined biostratigraphical scheme is described forthe Ibex and Davoei Zones (Carixian Substage, Lower Jurassic) in NW Europe, and the biostratigraphical details of the Carixian — Domerian boundary are outlined. It is based on detailed stratigraphical collections of ammonites from the major Pliensbachian localities in Britain, France and Germany, with supplementary data from Portugal. The zones and subzones, which are largely unchanged from the well-established scheme described by Dean & alii (1961), are further divided into zonules which can be recognised throughout NW Europe. These zonules, nine for the Ibex Zone and seven for the Davoei Zone, probably represent the greatest biostratigraphical resolution readily obtainable using ammonite faunas. The problems inherent in the precise recognition of the chronostratigraphical Carixian-Domerian boundary, owing to slightly discordant species ranges, are discussed.     

Size changes in Jurassic liparoceratid ammonites and their stratigraphical and ecological significance

Over 50 species of liparoceratid ammonites have previously been recognized from the Ibex and Davoei Zones (Lower Pliensbachian, Lower Jurassic) of England alone. Such a high specific diversity is an artifact caused by their stratigraphical importance and the complex nature of their shells. Simple bivariate analysis indicates that Aegoceras species are arbitrary subdivisions of an allometric growth trend. Principal component multivariate analysis shows that Liparoceras and Androgynoceras (sensu Callomon) are quite distinct from Aegoceras , and they display a more random pattern of variation. The existence of stratigraphically useful size changes in liparoceratids mirrors precisely size increases in benthic molluscan taxa, such as the bivalve 'Astarte' platymorpha and the archaeogastropod Eucyclus subimbricata. The ammonite size changes, at least, probably result from phenotypic variation analogous to that observed in the living cephalopod Sepia officinalis. This evidence taken in conjunction with the fact that kosmoceratid ammonite size changes correspond somewhat with benthic faunal changes suggests that ammonites maybe less useful for stratigraphy than is believed.     

Evidence for the longest stratigraphic range of a post-Triassic Ichthyosaur: a Leptonectes tenuirostris from the Pliensbachian (Lower Jurassic) of Switzerland

A three-dimensional well-preserved ichthyosaur skull and parts of the postcranial skeleton are attributed to the species Leptonectes tenuirostris (Conybeare, 1822). It was found vertically embedded in Pliensbachian deposits representing three successive biozones (ibex to margaritatus Zone). The find is dated as early Late Pliensbachian (margaritatus Zone) by a rich ammonite and ostracod fauna. It is the first record of the genus Leptonectes from Switzerland and from the Late Pliensbachian. It is so far the best preserved and most complete ichthyosaur from this time interval worldwide. With diagnostic specimens known from the Rhaetian (Late Keuper) up to the early Late Pliensbachian (Middle Liassic), L. tenuirostris (Conybeare, 1822) has the most extensive stratigraphic range documented for any post-Triassic ichthyosaur so far.     

Biodiversity and biogeography of middle–late liassic ammonoids: implications for the early Toarcian mass extinction

In Western Tethyan areas, the Toarcian stage begins with two important evolutionary events in ammonite faunas: (1) the disruption of Tethyan–Boreal provinciality; (2) a biological crisis linked with the oceanic anoxic event OAE. The analysis of these events has been addressed by constructing curves of ammonoid diversity (species richness, origination and extinction rates) in the Late Pliensbachian (= Domerian)–Early Toarcian interval in selected localities. Two diversity drops are recognized. The first one is recorded at the end of the Dactylioceras mirabile subzone and reflects the disruption of Tethyan–Boreal provinciality, through the progressive extinction of the Boreal endemic family Amaltheidae that occupied the north-western European seas during the whole Pliensbachian on the one hand, and the extinction of Late Domerian Ammonitina endemic to the Mediterranean areas on the other hand. The Early Toarcian homogeneization of Mediterranean and north-western European ammonoid faunas was reached via elimination of both Boreal and Mediterranean endemics with differential rates of extinction in the two palaeogeographic domains and the subsequent geographical expansion of Tethyan-derived ammonoids. The second, dramatic drop in ammonite diversity in the upper part of the Dactylioceras semicelatum subzone coincided with the onset of OAE. It also affected epioceanic ammonoid clades like Phyllocerataceae and Lytocerataceae. These two drops are interpreted as two distinct extinctions and not as episodes of a single, stepwise event. Complex relations between ammonoid diversity and sea-level changes are suggested by trends in endemism, which may be reversed during either a single transgression or a single regression.     

Global radiolarian zonation for the Pliensbachian, Toarcian and Aalenian

Jurassic radiolarians from 220 samples in Queen Charlotte Islands, B.C., Williston Lake, B.C., east-central Oregon, Baja California Sur, southern Spain, Austria, Slovenia, Turkey, Oman, Japan and Argentina were studied in order to construct global zonation for the Pliensbachian, Toarcian and Aalenian stages. Well-preserved faunas from continuous stratigraphic sections in Queen Charlotte Islands provide the most detailed record for this time interval, and all collections are tied to North American ammonite zones or assemblages. Collections from nearly all other areas lack independent dating except for early Toarcian carbon-isotope dating in Slovenia and late Aalenian ammonites in Spain.A database of 197 widely distributed updated taxonomic species was used to construct a Unitary Association (UA) zonation for the interval. A global sequence of 41 UAs was obtained for the top of the Sinemurian to the base of the Bajocian. The first and the last UAs represent the Late Sinemurian and the Early Bajocian respectively. The remaining 39 UAs were merged into nine zones (four Early Pliensbachian, one Late Pliensbachian, one Early Toarcian, one Middle-Late Toarcian, and two Aalenian) according to prominent radiolarian faunal breaks and ammonite data. The new zones are the Canutus tipperi - Katroma clara Zone (latest Sinemurian/earliest Pliensbachian); Zartus mostleri - Pseudoristola megaglobosa, Hsuum mulleri - Trillus elkhornensis and Gigi fustis - Lantus sixi zones (Early Pliensbachian); Eucyrtidiellum nagaiae - Praeparvicingula tlellensis Zone (Late Pliensbachian); Napora relica - Eucyrtidiellum disparile Zone (Early Toarcian); Elodium pessagnoi - Hexasaturnalis hexagonus Zone (Middle and Late Toarcian); Higumastra transversa - Napora nipponica Zone (early Aalenian); and Mirifusus proavus - Transhsuum hisuikyoense Zone (late Aalenian). These zones can be correlated worldwide and link previously established UA zonations for the Hettangian-Sinemurian and the Middle to Upper Jurassic. The new zonation allows high-resolution dating in the studied interval and provides a solid basis for analyzing faunal turnovers and the paleobiogeography of Jurassic radiolarians.     

Upper Sinemurian and Lower Pliensbachian ammonite faunas from Herford-Diebrock area (NW Germany)

At Herford-Diebrock a section from the Upper Sinemurian (Raricostatum to Aplanatum Subzone) to the Lower Pliensbachian (Polymorphus Subzone) is studied in respect of its ammonite faunas. Precise correlations in terms of faunal horizons are carried out between Yorkshire and SW Germany through Hessische Straße. Special emphasis is given to the taxonomical position ofEoderoceras armatum (Sowerby).Eoderoceras miles (Simpson) is now placed in synonymy withSowerby’s species. The section does not fulfill the requirements for the GSSP of the Sinemurian/Pliensbachian boundary.     

Distribution of clay minerals in Early Jurassic Peritethyan seas: Palaeoclimatic significance inferred from multiproxy comparisons

A set of published, unpublished, and new clay mineral data from 60 European and Mediterranean localities allows us to test the reliability of clay minerals as palaeoclimatic proxies for the Pliensbachian–Toarcian period (Early Jurassic) by reconstructing spatial and temporal variations of detrital fluxes at the ammonite biochronozone resolution. In order to discuss their palaeoclimatic meaning, a compilation of low-latitude belemnite δ¹⁸O, δ¹³C, Mg/Ca, and ⁸⁷Sr/⁸⁶Sr values is presented for the first time for the whole Pliensbachian–Toarcian period. Once diagenetic and authigenic biases have been identified and ruled out, kaolinite content variation is considered as a reliable palaeoclimatic proxy for the Early Jurassic. Major kaolinite enrichments occur during times of low δ¹⁸O, high Mg/Ca, and increasing ⁸⁷Sr/⁸⁶Sr, implying warm climates and efficient runoffs during the Davoei, Falciferum and Bifrons Zones. Conversely, cooler and drier times such as the Late Pliensbachian or the Late Toarcian are characterized by low hydrolysis of landmasses, and correspond to kaolinite depleted intervals. Secondary factors as modifications of sources or hydrothermalism may sporadically disturb the palaeoclimatic signal (e.g., in the Bakony area during the Late Pliensbachian). In addition, a spatial comparison of clay assemblages displays significant kaolinite enrichments towards northern parts of the Peritethyan Realm, probably related to the latitudinal zonation of hydrolyzing conditions. This implies enhanced runoffs on northern continental landmasses that reworked kaolinite-rich sediments from subtropical soils and/or Palaeozoic substrata.     

Deep-time phylogenetic clustering of extinctions in an evolutionarily dynamic clade (Early Jurassic ammonites)

Conservation biologists and palaeontologists are increasingly investigating the phylogenetic distribution of extinctions and its evolutionary consequences. However, the dearth of palaeontological studies on that subject and the lack of methodological consensus hamper our understanding of that major evolutionary phenomenon. Here we address this issue by (i) reviewing the approaches used to quantify the phylogenetic selectivity of extinctions and extinction risks; (ii) investigating with a high-resolution dataset whether extinctions and survivals were phylogenetically clustered among early Pliensbachian (Early Jurassic) ammonites; (iii) exploring the phylogenetic and temporal maintenance of this signal. We found that ammonite extinctions were significantly clumped phylogenetically, a pattern that prevailed throughout the 6.6 Myr-long early Pliensbachian interval. Such a phylogenetic conservatism did not alter--or may even have promoted--the evolutionary success of this major cephalopod clade. However, the comparison of phylogenetic autocorrelation among studies remains problematic because the notion of phylogenetic conservatism is scale-dependent and the intensity of the signal is sensitive to temporal resolution. We recommend a combined use of Moran's I, Pearson's ? and Fritz and Purvis' D statistics because they highlight different facets of the phylogenetic pattern of extinctions and/or survivals.     

Pliensbachian (Early Jurassic) calcareous nannofossils from the Peniche section (Lusitanian Basin,Portugal): A clue for palaeoenvironmental reconstructions

Quantitative analysis of Early Jurassic calcareous nannofossil assemblages from the Peniche section in Portugal have been performed in order to interpret palaeoenvironmental changes occurring in the Lusitanian Basin during the Late Pliensbachian Davoei, Margaritatus and Spinatum Ammonite Zones. Nannofossil data are compared to already published carbon and oxygen stable isotope data, organic matter content (wt.%Total Organic Carbon, TOC), and biomarker analysis. A significant change in calcareous nannofossil assemblages and species diversity at the transition between the Margaritatus and Spinatum Ammonite Zones matches with the pattern shown by geochemical data. This suggests that a profound change in environmental conditions occurred at that time. In the Davoei and Margaritatus Ammonite Zones, in a context of general sea-level rise, the Lusitanian Basin was characterized by water column stratification that favoured the sedimentation and preservation of organic matter. Biomarkers and oxygen isotope trends suggest that stratification of water masses occurred because of low salinity in surface waters. The shallowest part of the water column, characterized by oligotrophic conditions, was inhabited by the (probable) calcareous dinocyst Schizosphaerella spp., while the deep-dweller Crepidolithus crassus flourished in the lower photic-zone layers. In the Spinatum Ammonite Zone, a regressive trend occurred and a salinity increase is inferred on the basis of oxygen isotope values. Water masses were probably less stratified at that time. The upper photic-zone nannofossil assemblages were still dominated by Schizosphaerella spp. whilst, in the deep photic-zone, Mitrolithus jansae (a Mediterranean taxon) replaced C. crassus (a taxon with NW-European affinity). This pattern may indicate a change in palaeoceanographic conditions related to surface current circulation. The sea-level fall occurring during the Spinatum Ammonite Zone may have resulted in the partial isolation of the Lusitanian Basin from the NW-Europe basins because of the creation of a threshold. Alternatively, tectonic drowning of North African carbonate platforms in the Late Pliensbachian may have promoted better exchanges of nannoplankton between the Lusitanian Basin and the Mediterranean Tethys via the creation of new seaway connections.     

Reinvestigation on species richness and environmental correlates of bryophytes at a regional scale in China

Aims The aim of this article is 4-fold: (i) to update species richness of bryophytes for each of the Chinese provinces based on the most current knowledge on distributions of bryophytes in China, (ii) to provide a set of analyses based on the updated species richness data and the environmental variables used in a recent article on species richness of bryophytes in China, (iii) to expand the analysis presented in the recent article by relating species richness of bryophytes to over 15 additional climatic variables and (iv) to determine the degree to which the relationships between bryophyte species richness and environmental variables that were reported in the recent article might have been biased.Methods Over 180 literatures with national, provincial and local species lists of bryophytes in China were used in this study. Taxonomy and nomenclature of bryophytes in China were standardized according to The Plant List. Correlation and regression analyses were used to examine the relationships between species richness or species density of bryophytes in Chinese provinces and environmental variables.Important findings On average, each Chinese province possesses 700.6 species of bryophytes, which is 112.1 species more than previously reported. With the updated species richness data reported in this study, stronger relationships between species richness of bryophytes and environmental variables have been found, compared with those found in a recently published study for China. When single environmental variables were considered, precipitation-related variables were, on average, more strongly correlated with species richness and species density than were temperature-related variables. Environmental variables were on average correlated more strongly with species density than with species richness of bryophytes at the regional scale in China. Our study showed that measures quantifying the average and variation of environmental conditions within each Chinese province explained 82.7% and 71.1% of the variation in species richness of liverworts and mosses, respectively, and explained 86.5% and 70.7% of the variation in species density of liverworts and mosses, respectively.     

两个入侵烟粉虱隐种MEAM1与MED对番茄黄曲叶病毒水平传播能力的比较

【目的】烟粉虱 Bemisia tabaci 是番茄黄曲叶病毒（Tomato yellow leaf curl virus, TYLCV）在自然界的唯一传播媒介,除了可以直接取食获取TYLCV,烟粉虱还可以通过交配获取此植物病毒。虽然前人研究证明了烟粉虱Middle East-Asia Minor 1 （MEAM1）和Mediterranean （MED）隐种都可以通过交配在两性个体之间水平传播TYLCV,但有关MEAM1与MED隐种水平传播TYLCV的能力是否存在差异,不同研究的结果却并不一致。另外,目前尚无关于烟粉虱的水平传播行为是否有助于TYLCV在田间扩散的相关研究。【方法】从浙江、广东、云南和河南4个省份的田间采集MEAM1和MED隐种烟粉虱种群,在室内应用分子标记对各种群所属隐种鉴定后分别建立7个供试种群,然后观察每个种群内带毒成虫与不带毒成虫通过交配在不同性别个体之间水平传播TYLCV的能力,并选用采自广东的MEAM1隐种烟粉虱模拟群体交配实验探究通过交配获毒的烟粉虱个体是否具有传播TYLCV致健康番茄植株发病的能力。【结果】4个省内的MEAM1和MED隐种烟粉虱都可通过交配对TYLCV进行水平传播,但传播频率一般在10%以下。不同省份的MEAM1隐种种群之间在水平传播TYLCV的能力上无显著差异,不同省份的MED隐种种群之间也不存在显著差异。另外,同一省份的MEAM1隐种与MED隐种之间在水平传播TYLCV的能力上也不存在显著差异,而且在两个隐种中,带毒雄虫将病毒水平传播给不带毒雌虫与带毒雌虫将病毒水平传播给不带毒雄虫的频率没有显著差异。研究还表明,采自广东的MEAM1隐种烟粉虱个体通过交配水平获毒后不能致健康番茄植株发病。【结论】综合以上结果,我们推测TYLCV在中国境内两个入侵烟粉虱隐种MEAM1和MED各自种群内个体之间的水平传播概率较低,对该病毒在田间的扩散可能没有作用或作用不大。     

Extinction pattern of marine Ostracoda across the Pliensbachian-Toarcian boundary in the Cordillera Ibérica, NE Spain: Causes and consequences

This paper discusses the extinction pattern of the Pliensbachian-Toarcian boundary (PTB) ostracod assemblages at the Almonacid de la Cuba section (Cordillera Ibérica, NE Spain), which has been recently proposed as auxiliary boundary stratotype for the PTB. The ostracod record shows that the main Early Jurassic ostracod extinction event occurred not at the end of the Pliensbachian, but near the top of the Mirabile ammonite Subzone, Tenuicostatum ammonite Zone (Early Toarcian). On the basis of the evaluation of PTB ostracod record, a new causal explanation for the Early Toarcian ostracod turnover is proposed. This paper suggests that a reorganization of surface and deep-water circulations caused by the opening of the Hispanic Corridor could have generated a mild cooling episode, finally affecting the survival of healdioid ostracods.     

Spatial distribution of Late Pliensbachian (Early Jurassic) calcareous nannofossils within the Lusitanian basin (Portugal)

Quantitative analyses of Pliensbachian calcareous nannofossils have been carried out on a proximal-distal transect in the Lusitanian Basin (Portugal). The studied sections Vale Venteiro near Tomar and Peniche represent proximal and distal environments with respect to the emerged land of the Iberian Meseta (to the East). The upper portion of the Vale das Fontes Fm (Davoei and Margaritatus ammonite Zones) is studied in both sections and correlated by means of ammonite and nannofossil integrated biostratigraphy. A careful analysis of the preservation state of nannofossils is performed. Preservation state is moderate to good in the two settings; changes in nannofossil assemblages are therefore considered as primary. Samples were analysed for nannofossil absolute and relative abundances, species diversity and wt%CaCO₃. The analysis of calcareous nannofossils (absolute abundance, percentage, average abundance) shows changes in the community structure in space (i.e., from proximal to distal), and vertically within the water column. This pattern suggests a partitioning of habitats within the photic zone, and with respect to emerged lands. Proximal environments within the Lusitanian Basin were probably more eutrophic, because of the proximity of emerged lands to the East (Iberian Meseta). This was the source area for nutrients delivered into the basin by river transport. Distal environments were likely characterized by a greater water depth and by a deeper light penetration leading to a relatively more expanded photic zone. The assemblages recorded in the proximal setting exhibit high mean relative abundance of placolith-bearing coccolithophorids (Lotharingius spp., Biscutum spp. and Similiscutum spp.) and of Schizosphaerella spp., while distal assemblages are dominated by Crepidolithus crassus and Schizospharella spp. Crepidolithus crassus is interpreted as a deep-dweller coccolithophorid, inhabiting preferentially distal and deeper settings in the Lusitanian Basin. Placolith-bearing coccolithophorids were more abundant in proximal settings with respect to emerged lands, under relatively elevated trophic conditions. The probable calcareous dinocyst Schizospharella spp. proliferated in surface waters of both proximal and distal environments.     

Latitudinal gradient of taxonomic richness of ammonites in the Kimmeridgian-Volgian in the Northern Hemisphere

The latitudinal gradient of taxonomic richness (LGTR) of Kimmeridgian and Volgian ammonite genera of the Northern Hemisphere is evaluated, and the LGTR evaluation methods and factors influencing LGTR are discussed. In the Kimmeridgian-Volgian the LGTR values for ammonites were largely influenced by the paleogeography of the Middle Russian Sea, which was directly connected with the Neotethys and, to a lesser extent, by the exchange through the connection between the Arctic and Pacific oceans. The Middle Russian Sea is considered to have been a major source of immigrant taxa to the Arctic basins. The highest latitude ammonite faunas were influenced by the Pacific faunas, and due to the permanent presence of oceanic phylloceratids and lytoceratids, ammonite taxonomic richness was relatively high compared to some mid-latitudinal sites. The gradual decrease in taxonomic richness that occurred from the end of the Kimmeridgian to the end of the Volgian in all Subboreal basins probably resulted from the eventual isolation from the Neotethys. Subboreal ammonite associations from the ecotone between the two superrealms (Panboreal and Tethys-Panthalassa) were affected by short-term climatic oscillations, which led to rapid changes in the ammonite assemblages.     

Provinciality of the Mediterranean lower Jurassic brachiopod fauna: Causes and plate-tectonic implications

The composition of 23 “NW European” and “Mediterranean” Lower Jurassic (Pliensbachian) brachiopod faunas is compared at the species level. On the basis of this quantitative approach, the two “provinces” can be delimited more sharply than by earlier qualitative studies. In the author's opinion the most reasonable cause of the provinciality is as follows: in the Middle Triassic a segment of the European shelf became rifted, detached and drifted toward the open Tethys ocean. Being isolated, the brachiopods of this province could produce evolutionary lineages different from the European ones. If the presence of this contiguous and separate Triassic—Jurassic microcontinent characterized by Mediterranean brachiopod faunas is assumed, this factor should be borne in mind in the reconstructions concerning the closure of the Tethys (= Alpine orogeny).     

Les faunes d’ammonites du Pliensbachien inférieur des séries dauphinoises de la Durance (Jurassique inférieur, Barrage de Serre-Ponçon, Hautes-Alpes, France)

The Liassic ammonite faunas and especially those of the Early Pliensbachian are of major importance for the understanding of the stratigraphic framework of the “Dauphiné” zone of the southern subalpine ranges (“dôme de Remollon”). Until now, only listed by the authors, these faunas are, for the first time, described and illustrated in the present paper. With about twenty species, these faunas cover the whole of the Early Pliensbachian. There are poorly diversified and of clearly Euroboreal affinities. Nearly all of the species are abundant and common in most of the NW European fossiliferous localities. Despite of a paleogeographical location fairly close to the Alpine zones (Southern Alps and Austroalpine units) with rather diversified faunas of mainly Mediterranean affinities, none Mediterranean taxa are present in the studied area. Unfortunately, the current stratigraphic and paleogeographic knowledge do not allow to ascertain if this reflects a separation due to paleoenvironmental or true paleogeographic barriers. In this latter case, the general geologic implications would be remarkable.     

中国蚂蚁丰富度地理分布格局及其与环境因子的关系

物种丰富度分布格局及其形成机制的研究对于生物多样性保护具有重要意义。为了了解中国蚂蚁物种丰富度分布格局,利用中国省级尺度蚂蚁物种分布数据和环境信息,结合GIS和数理统计方法,探讨蚂蚁物种丰富度的地理分布格局与环境因子之间的关系。研究结果表明:(1)蚂蚁丰富度随纬度增加呈逐渐递减趋势,但缺乏显著的经度梯度。丰富度最高的地区主要集中在南方省份,我国北方、西北干旱区和青藏高原北部地区丰富度较低;(2)简单线性回归分析表明,能量、水分和季节性因素中,影响蚂蚁物种丰富度最强的因子分别为最冷月均温(TEMmin)(R2adj=0.532)、年均降水量(PREC)(R2adj=0.376)和年温度变化范围(TEMvar)(R2adj=0.539),而单个生境异质性因子对蚂蚁物种丰富度的影响均不显著;(3)最优模型由年均温(TEM)、海拔变化范围(ELErange)和年温度变化范围(TEMvar)组成,能够解释68.4%的蚂蚁丰富度地理分异。鉴于海拔变化范围更多地反映与温度相关的生境异质性,因此温度是限制中国蚂蚁分布的最重要因素。另外,分析结果还表明,海南、贵州、江西、四川、安徽和山西等6省蚂蚁区系调查最不充分,是未来发现蚂蚁新分布的热点地区。     

Reproducibility and reliability of the Pliensbachian calcareous nannofossil biohorizons from the Basque-Cantabrian Basin (Northern Spain)

Based on calcareous nannofossil assemblages identified in four expanded and well-dated sections from the Basque-Cantabrian Basin, the main objective of this paper is to improve the knowledge of the Pliensbachian calcareous nannofossil events, and to calibrate these events to the ammonite zones established for this area. The semiquantitative analysis of more than 140 smear slides from the Tudanca and Santotis sections, and the re-analysis of more than 200 smear slides from the Camino and San Andrés sections, have been carried out in order to describe the succession of calcareous nannofossil assemblages. Related to their composition changes, we have recognized and calibrated to the ammonite zones two main events: the first occurrences (FOs) of Similiscutum cruciulus and Lotharingius hauffii, and six secondary events: the FOs of Biscutum novum, Biscutum grande, Biscutum finchii, Lotharingius barozii and the FCOs (first common occurrences) of Calcivascularis jansae and L. hauffii. In the Camino and San Andrés sections, we also identify the FOs of Biscutum dubium, Bussonius prinsii and Lotharingius sigillatus. The obtained data allow us to assess the degree of reproducibility of the Pliensbachian calcareous nannofossil events in the studied area. The biohorizon succession recognized in the Basque-Cantabrian Basin are compared to those proposed for NW Europe, Lusitanian Basin, Italy and Southern France.     

Species richness,endemism and conservation of Mexican gymnosperms

An analysis of the distribution patterns of 124 Mexican gymnosperm species was undertaken, in order to detect the Mexican areas with high species richness and endemism, and with this information to propose areas for conservation. Our study includes an analysis of species richness, endemism and distributional patterns of Mexican species of gymnosperms based on three different area units (states, biogeographic provinces and grid-cells of 1° × 1° latitude/longitude). The richest areas in species and endemism do not coincide; in this way, the Sierra Madre Oriental province, the state of Veracruz and a grid-cell located in the state of Oaxaca were the areas with the highest number of species, whereas the Golfo de México province, the state of Chiapas and a grid-cell located in this state were the richest areas in endemic species. A weighted endemism and corrected weighted endemism indices were calculated, and those grid-cells with high values in both indices and with high species richness were considered as hotspots; these grid-cells are mainly located in Southern and Central Mexico.