Late Pleistocene beetle faunas of Beringia: where east met west

Aim   To examine the issue of Beringian steppe-tundra from an entomological standpoint, using fossil beetle data collected from late Pleistocene sites.
Location   North-eastern Siberia (Western Beringia), the Bering Land Bridge (Central Beringia), and Alaska and the Yukon Territory (Eastern Beringia).
Methods   Analysis of habitat preferences of beetle species found in fossil assemblages, leading to classification of major habitat types characterized by the faunal assemblages.
Results   Fossil beetle assemblages indicative of steppe-tundra are found mainly in the interior regions of Eastern Beringia, whereas these assemblages dominate nearly all late Pleistocene fossil sites in Western Beringia. Eastern Beringian faunas contain a much larger proportion of mesic to hygrophilous species and very few arid-habitat species. In contrast to this, the habitat requirements of the Western Beringian faunas are more evenly spread across the moisture spectrum.
Main conclusions   The taxonomic patterns of the two sets of fossil assemblages are remarkably different. Eastern Beringian faunal assemblages contain substantial numbers of mesic tundra and riparian rove beetles (Staphylinidae); this element is almost entirely lacking in the Western Beringian fossil assemblages. Taphonomic bias tends to overemphasize moisture-loving species at the expense of dry, upland species in the fossil record. Both Western and Eastern Beringian landscapes undoubtedly contained mosaics of habitats ranging from dry uplands (steppe-tundra) through mesic tundra to bogs and riparian corridors.     

Cuticular anatomy of Sphenobaiera huangii (Ginkgoales) from the Lower Jurassic of Hubei, China

Sphenobaiera huangii (Sze) Hsü is typical Early Mesozoic fossil foliage of Ginkgoales in China. It has been recorded from the Upper Triassic to the Lower Jurassic. The cuticular anatomy is investigated based on material from the type locality, Lower Jurassic Hsiangchi Formation, Zigui County, Hubei Province. The specimens are similar to S. huangii, but contain new information about leaf morphology and cuticular anatomy. Lower and upper cuticle is investigated using light and electron microscopy (LM, SEM, and TEM). Many features are described for the first time, including general structures of lower and upper cuticle, stomata, papillae, and cuticular ultrastructure. At the ultrastructural level, two layers have been distinguished in both lower and upper cuticle, including a homogeneous outer layer with granules and a heterogeneous inner layer with fibrils. Based on a literature comparison between S. huangii and other relevant species of Sphenobaiera, S. huangii may represent the best-known taxon in the genus Sphenobaiera in both leaf morphology and cuticular structures. This study provides the first detailed ultrastructural data on the leaf cuticle of Sphenobaiera, one of the oldest foliage taxa of Ginkgoales, and offers further evidence for potential discussion on the taxonomic relationships of S. huangii with other ginkgoalean taxa.     

Mitochondrial DNA data imply a stepping‐stone colonization of Beringia by arctic warbler Phylloscopus borealis

Arctic warbler Phylloscopus borealis is one of several high‐latitude Passerines which are widely distributed across one northern continent but restricted to the Beringian part of the other. Most species with such asymmetric intercontinental ranges are monomorphic across Beringia, suggesting either recent colonization of the second continent or considerable gene flow across the Bering Strait. Arctic warbler is the only migratory species in this group that has three different subspecies in Beringia: Ph. b. borealis (Scandinavia to western Beringia, south to Mongolia), Ph. b. xanthodryas (Japan, Sakhalin, Kamchatka, western Beringia), and Ph. b. kennicotti (Alaska). This polymorphism may indicate that Arctic warbler has a unique and complex phylogeographic history that differs significantly from other species with similar ranges. Our analyses of complete mtDNA ND2 sequences of 88 Arctic warblers collected across the species range showed that the clade comprised of birds breeding on Sakhalin Island and Kamchatka Peninsula diverged from the Palearctic/Beringian clade by 3.8% in ND2 sequence. Beringian birds formed a recently derived clade embedded within the Palearctic clade. Nucleotide diversity declined sharply eastward from Palearctic to western Beringia and then to eastern Beringia. Our data provided no support for currently recognized subspecies. They suggested that the barrier at the western edge of Beringia was crossed by Arctic warbler earlier than the Bering Strait resulting in a stepping‐stone colonization of Beringia by this species. Gene flow appears to be restricted across the western border of Beringia but not the Bering Strait.     

Bennettitalean leaf cuticle fragments (here Anomozamites and Pterophyllum) can be used interchangeably in stomatal frequency‐based palaeo‐CO2 reconstructions

Abstract: Bennettites are an abundant and frequently well‐preserved component of many Mesozoic fossil floras, often playing an important ecological role in flood plain vegetation communities. During a recent study focusing on stomatal indices of Triassic–Jurassic fossil plants, it became evident that the leaf fragments of two bennettite genera Anomozamites Schimper (1870) emend. Harris (1969) and Pterophyllum Brongniart (1825) display a significant overlap of leaf shape as well as cuticular characters. Owing to the preference of recognition of single taxa (ideally species) for the stomatal method, we use a database of 70 leaf fragments of Anomozamites and Pterophyllum compressions from five isotaphonomic Late Triassic sedimentary beds of Astartekløft in East Greenland to test whether leaf and cuticle fragments of the two genera can be separated using a range of quantitative and qualitative morphological and statistical analyses. None of the observed characters – including stomatal frequencies – could be applied to separate the fragments of the two genera into well‐defined groups. Our results therefore indicate that fragmented material and dispersed cuticles cannot be utilized to distinguish between Anomozamites or Pterophyllum at the genus level, but that instead these cuticle fragments may be used interchangeably as stomatal proxies. Classification of fossil leaves into either of these genera is thus only possible given adequate preservation of macro‐morphology and is not possible based solely on cuticle morphology. We suggest that this large inter‐ and intra‐generic morphological variation in both leaf and cuticle traits within Anomozamites and Pterophyllum may be related to the bennettites’ role as understory plants, experiencing a range of micro‐environmental conditions, perhaps depending mainly on sun exposure. Based on the results obtained in this study, we conclude that Anomozamites and Pterophyllum cuticle fragments can be employed interchangeably in palaeo [CO₂] reconstructions based on the stomatal method, thus potentially annexing a plethora of bennettitalean fossil plant material as CO₂ proxies, including dispersed cuticles.     

The presence of cutan limits the interpretation of cuticular chemistry and structure: Ficus elastica leaf as an example

Plant cuticles have been traditionally classified on the basis of their ultrastructure, with certain chemical composition assumptions. However, the nature of the plant cuticle may be misinterpreted in the prevailing model, which was established more than 150 years ago. Using the adaxial leaf cuticle of Ficus elastica, a study was conducted with the aim of analyzing cuticular ultrastructure, chemical composition and the potential relationship between structure and chemistry. Gradual chemical extractions and diverse analytical and microscopic techniques were performed on isolated leaf cuticles of two different stages of development (i.e. young and mature leaves). Evidence for the presence of cutan in F. elastica leaf cuticles has been gained after chemical treatments and tissue analysis by infrared spectroscopy and electron microscopy. Significant calcium, boron and silicon concentrations were also measured in the cuticle of this species. Such mineral elements which are often found in plant cell walls may play a structural role and their presence in isolated cuticles further supports the interpretation of the cuticle as the most external region of the epidermal cell wall. The complex and heterogeneous nature of the cuticle, and constraints associated with current analytical procedures may limit the chance for establishing a relationship between cuticle chemical composition and structure also in relation to organ ontogeny.     

The relative share of graminoid and forb life-forms in a natural gradient of herb layer productivity

The proportional share of graminoid and forb life-form in the herbaceous layer was investigated along a productivity gradient at Laelatu, western Estonia With an increase in the herbaceous layer standing crop from 43 5 to 723 7 g m⁻² the graminoid life-form became dominant in total above-ground mass and in species number Three hypotheses to better explain competitive ability of graminoids were tested 1) graminoids are able to form higher foliage, 2) they are able to distribute foliage nitrogen in a more beneficial way, 3) they have better nitrogen use efficiency 21 sample plots 50 × 50 cm were harvested All above-ground parts of vascular plants were removed by two canopy layers Vertical separation of layers were made according to the height of half light interception A species list was compiled, total and leaf masses and leaf nitrogen content of both life-forms were measured by layer ANOVA showed that there were no significant differences in vertical distribution of foliage or foliage nitrogen between life-forms in the productivity gradient, and hypotheses 1) and 2) are not supported by our data-set Hypothesis 3) is approved partly as the nitrogen concentration in graminoid foliage was 20% less than in forbs If one supposes that nitrogen retention time is equal in both life-forms then graminoids must have higher nitrogen use efficiency when compared to forbs Although the influence of life-form x productivity interaction on leaf nitrogen concentration was not significant, there was a tendency that difference in leaf mass to nitrogen ratio of the two life-forms increased with increasing incident light Thus, we can hypothesize that graminoid species dominate in high productive plots where the incident light intensity is also higher due to their better nitrogen use efficiency when compared to forb species     

Repeatedly out of Beringia: Cassiope tetragona embraces the Arctic

Aim Eric Hultén hypothesized that most arctic plants initially radiated from Beringia in the Late Tertiary and persisted in this unglaciated area during the Pleistocene glaciations, while their distribution ranges were repeatedly fragmented and reformed elsewhere. Whereas taxonomic and fossil evidence suggest that Cassiope tetragona originated in Beringia and expanded into the circumarctic area before the onset of the glaciations, lack of chloroplast DNA (cpDNA) variation may suggest that colonization was more recent. We address these contradictory scenarios using high‐resolution nuclear markers. Location Circumpolar Arctic. Methods The main analysis was by amplified fragment‐length polymorphism (AFLP), while sequences of chloroplast DNA verified the use of Cassiope mertensiana as an outgroup for C. tetragona. Data were analysed using Bayesian clustering, principal coordinates analyses, parsimony and neighbour‐joining, and measures of diversity and differentiation were calculated. Results The circumpolar C. tetragona ssp. tetragona was well separated from the North American C. tetragona ssp. saximontana. The genetic structure in ssp. tetragona showed a strong east–west trend, with the Beringian populations in an intermediate position. The highest level of diversity was in Beringia, while the strongest differentiation in the data set was found between the populations from the Siberian Arctic west of Beringia and the remainder. Main conclusions The results are consistent with a Beringian origin of the species, but the levels and geographical patterns of differentiation and gene diversity suggest that the latest expansion from Beringia into the circumarctic was recent, possibly during the current interglacial. The results are in accordance with a recent leading‐edge mode of colonization, particularly towards the east throughout Canada/Greenland and across the North Atlantic into Scandinavia and Svalbard. As fossils demonstrate the presence of the species in North Greenland 2.5–2.0 Ma, as well as in the previous interglacial, we conclude that C. tetragona expanded eastwards from Beringia several times and that the earlier emigrants of this woody species became extinct. The last major westward expansion from Beringia seems older, and the data suggest a separate Siberian refugium during at least one glaciation.     

Frenelopsis (Coniferales: Cheirolepidiaceae) And Related Male Organ Genera From The Lower Cretaceous Of Spain

Vegetative plant remains and microsporangiate cones, related to the fossil genera Frenelopsis and Classostrobus respectively, were studied in three localities from the Lower Cretaceous of the Pyrenees and Iberian Ranges (Spain). Sterile remains belong to three different species: F. Rubiesensis Barale, F. Ugnaensis sp. nov. and F. Turolensis sp. nov. The male cones Classostrobus ugnaensis sp. nov. and C. Turolensis sp. nov. are associated with the two latter species respectively, and C. Turolensis is found in connection with F. Turolensis . Internodes of F. Ugnaensis display small hemispherical papillae and long conical hairs covering the entire cuticle surface, while F. Turolensis has a strip of hairs near the leaf margin, in addition to more massive outer stomatal papillae and higher stomatal density. The tiny cones of C. Ugnaensis bear microsporophyll cuticles capped with vermiculate flattened papillae and a fringe of marginal hairs, while C. Turolensis has a central area of microsporophylls covered by long conical hairs. Sedimentological and taphonomic analyses show that the assemblages studied belong to a wide spectrum of habitats. These indicate that Spanish Lower Cretaceous frenelopsids were xeromorphic plants, able to adapt to helophytic and riparian habitats, and grew in brackish coastal marshes and fluvio–lacustrine freshwater environments.     

Cuticular penetration of abscisic acid

Summary Penetration of 2-¹⁴C abscisic acid (ABA) through enzymatically isolated cuticles from tomato fruit and from the upper epidermis of apricot, pear and orange leaves was assessed. Penetration was linear with time, greater as the undissociated than the dissociated ion, and greater through dewaxed than non-dewaxed cuticles. Significantly less (3–6 times) (2-¹⁴C)ABA penetrated the tomato fruit cuticle than NAA or 2,4-D. The leaf cuticles were less permeable than the tomato fruit cuticle. There was no evidence that the ABA was altered during transfer across the cuticle.     

云南腾冲上新统芒棒组植物分散角质层研究

在云南腾冲上新统芒棒组中发现保存较好的植物分散角质层,共识别出7种:Reticutissolida,Reticutis tylotis,Fundicutis verriculis,Lusaticutis arizelis,Piliparicutis anfracta,Discrepoparicutis elongata,Enormicutis torquata,可归于6属,4亚类,4类,1个大类,表现出上叶角质层类型和下叶角质层类型的组合特征及上叶角质层类型的优先保存情况。从表皮细胞形态及气孔器等微观特征上看,具气孔的4种之间有着明显的差别,表明它们可能分别来自不同的母体植物;其中3种角质层的母体植物极有可能为被子植物,并处于优势地位。滇西当时温暖湿润的热带-亚热带、暖温带气候,为分散角质层的母体植物提供了良好的生存条件。而该区植物分散角质层的发现为分析其母体植物和重建古环境提供微体植物化石证据。     

The importance of leaf cuticle for carbon economy and mechanical strength

Cuticle thickness of leaves varies >?100 times across species, yet its dry mass cost and ecological benefits are poorly understood. It has been repeatedly demonstrated that thicker cuticle is not superior as a water barrier, implying that other functions must be important. Here, we measured the mechanical properties, dry mass and density of isolated cuticle from 13 evergreen woody species of Australian forests. Summed adaxial and abaxial cuticle membrane mass per unit leaf area (CMA) varied from 2.95 to 27.4?g m(-2) across species, and accounted for 6.7-24% of lamina dry mass. Density of cuticle varied only from 1.04 to 1.24?g?cm(-3) ; thus variation in CMA was mostly due to variation in cuticle thickness. Thicker cuticle was more resistant to tearing. Tensile strength and modulus of elasticity of cuticle were much higher than those of leaf laminas, with significant differences between adaxial and abaxial cuticles. While cuticle membranes were thin, they could account for a significant fraction of leaf dry mass due to their high density. The substantial cost of thicker cuticle is probably offset by increased mechanical resistance which might confer longer leaf lifespans among evergreen species.     

The value of leaf cuticle characteristics in the identification and classification of Iberian Mediterranean members of the genus Pinus

This study reports the value of leaf cuticle characteristics in the identification and classification of Iberian Mediterranean species of the genus Pinus (P. nigra subsp. salzmannii, P. pinaster, P. pinea and P. halepensis), with the aim of using these characters to identify isolated cuticles and stomata in palynology slides. Preparations were made of the cuticles of pine needles belonging to one natural Iberian population of each of the above species. A number of epidermal morphological characteristics were then recorded with the aim of distinguishing these species from one another. The structure of the stomatal complex (the shape and arrangement of the subsidiary cells) was different in each species. The aperture of the epistomatal chamber was significantly smaller in P. pinea than in the other species examined, and the variables recorded for the thickening of the guard cells provided relationships that clearly distinguished all four taxa. The width and length of the stomata and the upper woody lamellae, the central distance between the external limits of the medial lamellae borders and the length of the stem were the most useful variables in this respect. The present results contribute to the ongoing discussion regarding the taxonomic classification of the members of Pinus, and provide valuable clues for the identification of Iberian Mediterranean pine species from small pine needle fragments or isolated stomata. After validation of the present results for multiple populations, these results could also be used to help identify fossil leaf macroremains and the scattered/isolated stomata commonly observed in palaeopalynological samples. © 2009 The Linnean Society of London, Botanical Journal of the Linnean Society, 2009, 161 , 436–448.     

Ultrastructural studies of fossil plant cuticles: Ticoa harrisii from the early Cretaceous of Argentina

ARCHANGELSKY, S., TAYLOR, T. N. & KURMANN, M. H., 1985. Ultrastructural studies of fossil plant cuticles: Ticoa harrisii from the early Cretaceous of Argentina. The fine structure of fossil plant cuticles of Cretaceous age demonstrates well preserved layers that are topographically equivalent to those in some extant plants. Cuticle stratification on specialized structures (stomatal apparatus and trichomes) is presented, together with an account of the fine structure of both the upper and lower cuticular membrane. Levels of cuticle stratification are compared with those of extant plants.     

中国植物化石角质层研究综述

总结近30年来中国大陆植物化石角质层研究的进展,介绍角质层分析的3个主要研究方向:植物化石表皮微细构造研究、植物化石气孔参数与大气CO2和气候变化研究以及植物化石角质层地球化学特征研究.举出众多典型实例,提出植物化石角质层分析的研究展望.     

Molecular genetic evidence for the post-Pleistocene divergence of populations of the arctic-alpine ground beetle Amara alpina (Paykull) (Coleoptera: Carabidae)

Aim This study examines the hypothesis that the biogeographic history of a species is reflected in the distribution of molecular genetic diversity and the phylogenies of extant populations. Location Populations of arctic-alpine ground beetle Amara alpina were analysed from Beringia (Alaska and northernmost British Columbia), the Hudson Bay region, the northern Appalachian Mountains, and the central Rocky Mountains of North America. Methods Mitochondrial restriction site variation of specimens from twenty-two populations were assayed by using radioactively labelled mtDNA to probe Southern membranes containing restriction enzyme digested total DNA. Restriction sites were mapped and genetic distances were calculated by pairwise comparison of presence and absence of restriction sites. Genetic distances were used in a molecular analysis of variance and to construct a minimal spanning tree. Parsimony methods were used to investigate the phylogenetic relationships between the haplotypes. These results were compared to an existing model for postglacial dispersal based on fossil and modern occurrences of arctic-alpine beetles. Results Among the twenty-two populations, fifteen haplotypes were detected. Genetic variation within each of the four regions corresponded to that expected from the palaeontologically based model. Beringian populations were the most genetically diverse. In contrast, no restriction site variation was observed in populations from the Hudson Bay region. Intermediate amounts of variation were observed in alpine populations of the Rocky and Appalachian Mountains. Maximum parsimony and cluster analysis provide evidence that at least two ancestral haplotypes existed in the Southern refugium from which the Rocky and the Appalachian Mountains populations were founded. Main conclusions The genetic results are generally consistent with the palaeontologically based model. The diversity of Beringian populations is consistent with this region having been continuously inhabited by Amara alpina throughout the Pleistocene. The Hudson Bay region was not deglaciated until about 6000 years, and its populations have no restriction site variation. The molecular genetic data support the interpretation that the Hudson Bay region was colonized from Beringia based on the occurrence of the same haplotype in both regions.     

Surface Printing of Plant Leaves for Phylogenetic Studies

A solution of plastic consisting of toluene, 720 ml; methanol, 180 ml; ethyl cellulose (Ethocel, standard 7 CPS), 250 gm; and Dow resin 276 V-2, 75 gm is applied to a leaf surface which has been dampened with toluene. The plastic is spread to a thin film with the edge of a card and allowed to dry. After drying, the plastic may be peeled from the leaf surface and either stored dry in a small envelope or mounted permanently on a microscope slide. Permanent mounts are prepared by placing a small section of the peel from the upper and lower surfaces of the leaf on a microscope slide and covering with a No. 1 cover glass. A small spot of balsam on each corner of the cover glass secures the glass in position. This air mount has proved to be superior to water, glycerol or balsam mounts. Fresh leaves are washed with a mild detergent before application of the plastic. Herbarium specimens are soaked in water overnight to restore the leaf to a semiturgid condition. Five species of different plant families have been illustrated to show the diagnostic features of the surface of the cuticle. An isolated layer of epidermal cells obtained by chemical maceration permitted cell and imprint comparison. The remarkable amount of detail shown by the prints is an aid for phylogenetic studies and may make the recognition of fossil cuticles possible.     

Primary and diagenetic microstructures in trilobites

McAllister, John E. & Brand, Uwe 1989 01 15: Primary and diagenetic microstructures in trilobites. Lethaia , Vol. 22, pp. 101–111. Oslo. ISSN 0024–1164.
Ordovician and Devonian trilobites were studied by scanning electron microscopy (SEM) to define primary and diagenetic microstructures. Primary structures such as Osmólska cavities and hexagonal surface openings are present in samples obtained from both shale and limestone lenses in shales. Generally, samples with primary microstructures are also geochemically well preserved. Diagenetic microstructures were found in samples from shales and limestones, but those from limestones are the most geochemically and microstructurally altered. 'Dendritic' patterns and fused matrices were found in the altered cuticles of trilobites of different species and ages and are therefore considered a normal feature of the diagenetic alteration of cuticular calcite. Primary and diagenetic microstructures of trilobite cuticles are independent of size, species and age of the specimens, but are largely controlled by lithology and thus diagenesis. * Trilobita, primary-, diagenetic microstructures, fossil diagenesis .     

Erratum

A solution of plastic consisting of toluene, 720 ml; methanol, 180 ml; ethyl cellulose (Ethocel, standard 7 CPS), 250 gm; and Dow resin 276 V-2, 75 gm is applied to a leaf surface which has been dampened with toluene. The plastic is spread to a thin film with the edge of a card and allowed to dry. After drying, the plastic may be peeled from the leaf surface and either stored dry in a small envelope or mounted permanently on a microscope slide. Permanent mounts are prepared by placing a small section of the peel from the upper and lower surfaces of the leaf on a microscope slide and covering with a No. 1 cover glass. A small spot of balsam on each corner of the cover glass secures the glass in position. This air mount has proved to be superior to water, glycerol or balsam mounts. Fresh leaves are washed with a mild detergent before application of the plastic. Herbarium specimens are soaked in water overnight to restore the leaf to a semiturgid condition. Five species of different plant families have been illustrated to show the diagnostic features of the surface of the cuticle. An isolated layer of epidermal cells obtained by chemical maceration permitted cell and imprint comparison. The remarkable amount of detail shown by the prints is an aid for phylogenetic studies and may make the recognition of fossil cuticles possible.