Alternating aeolian,sabkha and shallow-lake deposits from the Middle Triassic Gipsdalen Formation,Scoresby Land,East Greenland

Gypsum-bearing deposits of the Gipsdalen Formation (Anisian ? Ladinian ?) are described and interpreted on the basis of lithology, sedimentary structures and sequential pattern.The basal Kolledalen Member consists in the northwestern part of the area of coarse-grained alluvial-fan deposits overlain by cross-bedded aeolian sandstones and finer-grained sabkha or shallow desert-lake deposits. The overlying Kap Seaforth Member displays wel;-developed cyclic sedimentation. In the southeastern part of the area the ideal cycle consists of, from bottom to top: cross-bedded aeolian sandstone, structureless or wave-rippled sandstone of sabkha flat—marginal desert-lake origin, thin wave-rippled sandstone and irregularly bedded mudstone of marginal desert-lake origin and horizontally laminated mudstone deposited in an expanded desert lake.Foreset dips of the cross-bedded aeolian sandstones suggest alternating periods of north-northeast and south-southeast palaeowinds. It is concluded that the aeolian deposits of the Gipsdalen Formation were deposited at low palaeolatitudes in the northern hemisphere. In the Middle Triassic summer seasons the Intertropical Convergence Zone probably lay north of the Jameson Land Basin, which was reached by south-southeast trade winds. During the rest of the year the zone was situated to the south and the area came under the influence of north-northeast trade winds.     

Anomalous Westerlies, El Niño, and the Colonization of Polynesia

The west to east migration of the Polynesians and their Lapita predecessors was not accomplished by tacking against the prevailing southeast trade winds, but by using periodic westerly wind reversals to sail eastward. Data on equatorial westerlies and associated ocean current effects, including those gathered during recent El Niño events, are presented to indicate how these canoe voyagers were able to migrate so far into the Pacific.     

Factors controlling macrophyte distribution in large shallow Lake Võrtsjärv

We investigated the dependence of macrophyte parameters (distribution depth, width of the reed belt, density and length of shoots) on a number of abiotic factors (wind patterns, nutrient loading, slope of the littoral, granulometric sediment composition) in a large, shallow, and eutrophic Lake Võrtsjärv (270 km², average depth 2.8 m) in Estonia in 1997. The macrophytes colonized 19% of the lake area, whilst 95% was potentially suitable by depth. The most affected were the floating-leaved plants that colonized the smallest percentage (6%) of areas suitable for them with regard to depth. Factor analysis revealed a strong polarisation of the lake's vegetation both in west–east and north–south direction caused by (1) dominating westerly and south-westerly winds, (2) the shape of the lake narrowing down from north to south, and (3) concentration of bigger inflows at the west and south shores of the lake. The eutrophication process caused the disappearance of several species, on one hand, and the extension of the distribution areas of other species, on the other hand. Myriophyllum spicatum L. has become the dominating species among the submerged plants, replacing the earlier dominant, Potamogeton perfoliatus L.     

Nest-site selection by crossbills Loxia spp. in ancient native pinewoods at Abernethy Forest,Strathspey, Highland

Capsule Birds preferred stands with a particular density of trees, perhaps to avoid predation, and they selected aspects sheltered from prevailing winds.

Aim To describe the nesting habitat and tree selection by crossbills in a restricted pinewood habitat in Scotland.

Methods Scots Pines used by nesting crossbills were described and compared with randomly selected pines. Nest aspect was related to wind strength and direction.

Results The crossbills selected trees at a density of 50–60 trees/ha. Such stands may be sufficiently dense to provide cover, yet occur at a low enough density to minimize being visited by potential arboreal predators, such as Red Squirrels and Pine Martens. Crossbills tended to nest on lateral branches on the northeast side of crowns. Tree crown development was not asymmetric, so the birds may choose the northeast side to shelter from the prevailing southerly to westerly winds.

Conclusion Stands of pines at a low density need to be maintained for the benefit of crossbills.     

The Neovolcanic Axis Is a Barrier to Gene Flow among Aedes aegypti Populations in Mexico That Differ in Vector Competence for Dengue 2 Virus

Background

Aedes aegypti is the main mosquito vector of the four serotypes of dengue virus (DENV). Previous population genetic and vector competence studies have demonstrated substantial genetic structure and major differences in the ability to transmit dengue viruses in Ae. aegypti populations in Mexico.

Methodology/Principal Findings

Population genetic studies revealed that the intersection of the Neovolcanic axis (NVA) with the Gulf of Mexico coast in the state of Veracruz acts as a discrete barrier to gene flow among Ae. aegypti populations north and south of the NVA. The mosquito populations north and south of the NVA also differed in their vector competence (VC) for dengue serotype 2 virus (DENV2). The average VC rate for Ae. aegypti mosquitoes from populations from north of the NVA was 0.55; in contrast the average VC rate for mosquitoes from populations from south of the NVA was 0.20. Most of this variation was attributable to a midgut infection and escape barriers. In Ae. aegypti north of the NVA 21.5% failed to develop midgut infections and 30.3% of those with an infected midgut failed to develop a disseminated infection. In contrast, south of the NVA 45.2% failed to develop midgut infections and 62.8% of those with an infected midgut failed to develop a disseminated infection.

Conclusions

Barriers to gene flow in vector populations may also impact the frequency of genes that condition continuous and epidemiologically relevant traits such as vector competence. Further studies are warranted to determine why the NVA is a barrier to gene flow and to determine whether the differences in vector competence seen north and south of the NVA are stable and epidemiologically significant.     

Upper Cretaceous paleogeography of the Central Southern Pyrenean Basins (Catalonia, Spain) from microfacies analysis and charophyte biostratigraphy

The most extensive latest Cretaceous deposits of the Pyrenees are non-marine facies traditionally called “Garumnian”, which represent the first continentalization of the Pyrenean Foreland Basins. The age and paleogeography of the basal Garumnian facies in the different parts of the Pyrenean Basin has been a matter of debate. Charophyte biostratigraphy and microfacies analysis suggest that the continentalization was diachronous in the Central Southern Pyrenean basins, i.e., between the Àger and Tremp basins, and the emersion progressed from south to north. In the Àger Basin, to the south, the first Upper Cretaceous non-marine rocks are represented by the La Maçana Formation. This unit is mainly formed by freshwater lacustrine limestones organized into hundreds of shallowing-upwards sequences ranging from deeper lacustrine facies, through marginal, well-illuminated environments dominated by characean meadows, and finishing with lakeshores dominated by clavatoracean meadows. The charophyte assemblage from the La Maçana Fm is mainly formed by Peckichara cancellata, P. sertulata, Microchara cristata, M. parazensis, Platychara caudata, and Clavator brachycerus, which belong to the Peckichara cancellata charophyte biozone (Late Campanian). In contrast, in the Tremp Basin, located to the north, the beginning of the non-marine sedimentation is organized into a few cycles of the well-known La Posa Fm. These cycles begin with brackish deposits formed by thick marls with euryhaline molluscs at the base, followed by lignite and brackish to freshwater limestones. The brackish facies are dominated by porocharaceans. The charophyte assemblage of the La Posa Formation is formed by Feistiella malladae, Peckichara sertulata, Microchara cristata, and Clavator brachycerus, which belong to the Septorella ultima charophyte biozone (Early Maastrichtian).     

The Relationship Between Spatial Distribution and Diet of Arctic Charr, Salvelinus Alpinus, In Loch Ness, U.K.

The pelagic fish community of Loch Ness, U.K., is dominated by Arctic charr, Salvelinus alpinus. Previous studies have shown that the distribution of zooplankton along the south-west to north-east axis of this elongate loch is very dynamic and determined largely by prevailing winds, but Arctic charr are consistently more abundant in the southern half of the loch. In July 1993, the diet compositions of 161 Arctic charr from 53 to 330mm in length were determined and related to their spatial distribution and those of microcrustacean zooplankton and pelagic chironomid larvae and pupae. Diets were dominated by chironomid larvae, with chironomid pupae, Bythotrephes longimanus, Bosmina coregoni and Daphnia hyalina also frequently taken. Over the whole study period, B. longimanus were more important in the diet of fish from the northern half of the loch, while chironomid larvae were more important for fish from the southern half. As a result, per capita prey weight of fish from the south was greater than that of fish from the north. However, wind-induced changes in the distribution of zooplankton along the loch were accompanied by a change in the diet composition of Arctic charr from the south.     

Early Cretaceous calcareous algae from central Iran (Taft Formation, south of Aliabad, near Yazd)

A rich association of calcareous algae is described from the Lower Cretaceous (Barremian–? Lower Aptian) deposits of the Taft Formation, located south of Aliabad (in the vicinity of Yazd, central Iran). The association mainly consists of dasycladaleans and bryopsidales (udoteaceans and gymnocodiaceans); additionally, rare “solenoporaceans” and cyanophyceans are present. Three new species are described: two are dasycladaleans (Pseudoactinoporella? iranica and Holosporella farsica) and one is an udoteacean (Boueina minima). Many of the described and illustrated algae are mentioned for the first time from Iran.     

Topography controlling the wind regime on the karstic coast: late Pleistocene coastal calcareous sands of eastern mid-Adriatic,Croatia

Aeolian dunes controlled by regional climate have been formed in many coastal areas of the Mediterranean Sea during the Quaternary. Generally, they are formed under a landward-blowing wind, and comprise numerous reworked penecontemporaneous shallow-marine carbonate grains. Along the eastern mid-Adriatic Sea, late Pleistocene aeolian and alluvial sands occur as isolated patches in karstic depressions on several islands and the Pelje?ac Peninsula. At most localities, the sands consist of a mixture of mostly carbonate rock fragments and siliciclastic material. A higher proportion of shallow-marine bioclasts was found only at one locality. The terrestrial material was transported to the coastal area by at least two rivers: paleo-Cetina and paleo-Neretva River, and was subsequently reworked and transported by wind, resulting in aeolian deposition. Sandy units of various thicknesses exhibiting sharp erosional bedding planes and cross-bedding are interpreted as representing aeolian dunes and sand sheets controlled by a complex wind regime. The mineralogical composition at almost all localities indicates near-river flood plains as the main sand source. Although the area was affected by strong winds blowing landward and parallel to the coast, they significantly deviated due to the local topography produced by the tectonically deformed and karstified carbonate basement. In this way, the late Pleistocene aeolian deposits on the mid-Adriatic islands differ from deposits from most Quaternary Mediterranean coastal aeolian belts, as they contain very small quantities of penecontemporaneous shallow-marine carbonate grains and were deposited by winds blowing in varying directions instead of prevailing landward-blowing winds.     

Ecophysiological characteristics of Porphyra spp. (Bangiophyceae,Rhodophyta): seasonal and latitudinal variations in northern-central Chile

The red macroalga Porphyra C. Agardh is one of the most ecologically successful genera that lives in the upper intertidal zone. Biochemical, physiological, and morphological acclimation strategies allow their growth and distribution as well as a quick recuperation between tidal regimens. Studies of Porphyra are poorly developed in Chile, and management and exploitation proposals need to be supported by biological and ecophysiological approaches. This study evaluated seasonal and latitudinal physiological performances of Porphyra spp. via maximum quantum yield (F _v?/?F _m), pigments, proteins, phenolic compounds, and antioxidant activity in order to describe how algae can acclimate to their environment and to provide insights to their management and use. Sampling was done at three costal sites in Chile between 25°S and 34°S between winters 2010 and 2011. A total of four different morphotypes were identified (one in the north, one in the center, and two in the south locations) and evaluated separately. Results showed seasonal and latitudinal patterns for all ecophysiological variables studied, with a general tendency of decrease in F _v?/?F _m, pigments, and soluble proteins during spring–summer seasons accompanied by an increase in the antioxidant capacity. Latitudinal differences were observed with a tendency of higher values for ecophysiological traits in central and southern morphotypes. Phenology patterns were different between an annual population in the north location and a perennial one for central-south populations. The taxonomic clarity should be evaluated in order to better understand if there exists intraspecific (dependent on morphology) or interspecific variation.     

Genetic Differentiation Among Populations of the Roseate Spoonbill (Platalea ajaja; Aves: Pelecaniformes) in Three Brazilian Wetlands

Effective population size, levels of genetic diversity, gene flow, and genetic structuring were assessed in 205 colonial Roseate spoonbills from 11 breeding colonies from north, central west, and south Brazil. Colonies and regions exhibited similar moderate levels of diversity at five microsatellite loci (mean expected heterozygosity range 0.50–0.62; allelic richness range 3.17–3.21). The central west region had the highest Ne (59). F _ST values revealed low but significant genetic structuring among colonies within the north and within the south regions. Significant global genetic structuring was found between the northern and central western populations as well as between the northern and southern populations. An individual-based Bayesian clustering method inferred three population clusters. Assignment tests correctly allocated up to 64% of individuals to their source regions. Collectively, results revealed complex demographic dynamics, with ongoing gene flow on a local scale, but genetic differentiation on a broader scale. Populations in the three regions may all be conserved, but special concern should be given to central western ones, which can significantly contribute to the species’ gene pool in Brazil.     

Plant community patterns in Moroccan temporary ponds along latitudinal and anthropogenic disturbance gradients

Background: Temporary ponds, an abundant habitat in the Maghreb region and notably in Morocco, have a high conservation value. However, they are mainly known from the north of the country.

Aims: The aim of this work was to characterise the vegetation of Moroccan temporary ponds along a combined gradient of latitude and anthropogenic pressure.

Methods: Eighty-five ponds distributed along a north–south gradient of 750 km were sampled. For each pond, all vegetation was surveyed (flooded and dry parts) and the local abiotic characteristics were measured during two successive hydrological cycles. The prevailing anthropogenic pressures were also identified and were attributed an impact score.

Results: Eighty-one characteristic pond species (including 17 rare species) were recorded, with several new distribution data in the southern part of the latitudinal gradient. Plant communities were related to climatic and anthropogenic factors, but mostly to local factors, such as maximum water depth and soil pH. The northern ponds (wettest macroclimate) were rich in characteristic species and rare species, while the southern (driest macroclimate) ponds were more species poor.

Conclusions: In addition to the direct impact of increasing human activity, a further reduction of the floristic richness of temporary ponds is expected due to climatic changes. This is particularly the case for characteristic species which have a high conservation value.     

Ecological Niche Conservatism in Doucs (Genus Pygathrix)

The impressive diversity and unique distribution of primate taxa in Southeast Asia creates a region of interesting biogeography and evolutionary history that remains poorly understood. The three species in the Asian colobine genus Pygathrix (P. cinerea, P. nemaeus, and P. nigripes) appear to follow the unique distribution pattern, replacing one another along the north–south axis. However, the evolutionary history and taxonomic status within Pygathrix is currently debated. We constructed climate-based ecological niche models (ENMs) for the three species, using six environmental variables, to confirm that the bioclimate envelopes of Pygathrix cinerea, P. nemaeus, and P. nigripes follow the north–south gradient. We also used the ENMs to test whether the three species lack ecological exchangeability, meaning differentiation among factors that define the fundamental niche, and whether they exhibit ecological niche conservatism, or the tendency for related species to differ less ecologically than might be expected by the climate available to each species. Our ENMs for Pygathrix followed a north–south gradient as expected, with P. nemaeus extending from ca. 14°N to 21°N, P. cinerea from 14°N to 16°N, and P. nigripes from 11°N to 13.5°N. This study presents the first use of ENMs for doucs that yield significant predictive ability based only on climatic variables. The models are significantly different for all three species, supporting a lack of ecological exchangeability between them, as well as the recent elevation of Pygathrix cinerea to species status. Importantly, Pygathrix cinerea and P. nemaeus show evidence of ecological niche conservatism, which lends support to the occurrence of an allopatric speciation event. This result also suggests that the current overlapping distribution of Pygathrix cinerea and P. nemaeus is the result of secondary contact. The north–south distribution gradient, which exists in similar form among other groups of sister taxa in the region, may be attributed to a zoogeographic barrier, vicariance, or current or historical climatic shifts.     

Factors affecting prevailing population levels of <Emphasis Type="Italic">Brevipalpus yothersi</Emphasis> (Acari: Tenuipalpidae) in citrus areas affected by citrus leprosis in the State of Sao Paulo,Brazil

Brevipalpus yothersi Baker (Acari: Tenuipalpidae) was recently confirmed as one of the main vectors of citrus leprosis. Knowledge about this mite’s biology is essential to understand its population dynamics, in order to solve management issues in citrus orchards and explain why citrus leprosis is more severe in some regions. This paper aimed to study biological factors affecting prevailing population levels of B. yothersi and incidence of citrus leprosis. Mites were sampled from orchards in the south, north and northwestern regions of São Paulo State, Brazil. We assessed duration of the developmental stages, oviposition, incubation period, egg viability, longevity, net reproductive rate (R_o), mean generation time (T), intrinsic rate of increase (r_m) and finite rate of increase (λ). There were small differences in parameter values between the three populations. Our results indicated that the various measures adopted in the control of the three populations did not lead to major biological differences between populations for the evaluated parameters.     

The first occurrence of a lingulid brachiopod from the Cretaceous of Sergipe,Brazil, with a restudy of ‘<Emphasis Type="Italic">Lingula</Emphasis>’ <Emphasis Type="Italic">bagualensis</Emphasis> Wilckens, 1905 from southern Patagonia

The lingulid brachiopod Lingularia? notialis sp. nov. is described from the upper Turonian (Cretaceous) of the Sergipe Basin in northeastern Brazil. The rare but well-preserved new material shows morphological characters such as muscle scars, mantle canals and a baculate shell structure. In a preliminary note L.? notialis was referred to Lingularia? bagualensis (Wilckens, 1905) from the uppermost Cretaceous of southern Patagonia, a species restudied here and referred conditionally to Credolingula Smirnova in Smirnova and Ushatinskaya, 2001.     

Synoptic weather conditions inducing long-distance immigration of planthoppers, Sogatella furcifera Horvath and Nilaparvata lugens Stal

• 1 Adults and nymphs of Sogatella furcifera and Nilaparvata lugens are serious pests of growing rice in Japan. They appear in June and July but their origin was unknown. Inflow of warm and humid air from the south was shown to favour the appearance of planthoppers. The air inflow was associated with the passage of depressions along the frontal zone, called Bai-u in the Far East.
• 2 Immigrations were categorized as mass or minor according to the density of immigrants surveyed by various traps. The mass immigrations were induced by the passage of depressions which emerged in the central part of the Chinese continent between 25 °N and 35 °N and proceeded eastwards between the observation point and about 600 km north. Warm and humid south west winds blew, on average, for 19.3 h at an average wind speed of 32.9 km/h. When the route digressed a little north or south, minor immigrations, with only S.furcifera in half the cases, occurred.
• 3 Minor immigration types were categorized into a long-lasting type which appeared in the final stage of the rainy season, a mass immigration typemodified by the location of a typhoon in the south, and a minor type near the frontal line occurring without the passage of recognizable depressions.
• 4 The greatest aerial densities of immigrants were estimated as three to seven per 10³m³ in S.furcifera and one to two per 10³ m³ in N.Iugens. Female immigrants were mostly unmated.
• 5 All the depressions that appeared in June and July 1967–72 were analysed and twenty-nine (76.3%) out of thirty-eight originating in the central part of the Chinese continent, caused immigrations. Yearly fluctuations of planthopper infestations in Japan were shown to depend on the yearly fluctuations of the route of depressions associated with the migration of the planthoppers.

     

Ecological trends in travertine colonisation by pioneer algae and plant communities

The distribution and amount of biological colonisation on the “Lungotevere” walls (Rome) were analysed to assess the ecological role of the main environmental parameters (solar irradiation, rain winds, prevailing winds) and of the nearby tree covering. The floral data indicate a close similarity of species in the stations examined and a dominance of Chroococcus lithophilus Ercegovic among the cyanobacteria and of Erigeron karvinskianus DC among the vascular plants. In these very hard conditions the exposure and amount of the water input do not seem to influence the flora qualitatively as much as it does quantitatively. The low value of microflora, as found in areas characterised by the presence of trees, can be referred to as resulting from the “umbrella” effect of the plants. The macroflora is less influenced by such effects due to the greater capacity of these plants to derive moisture through their roots.     

Do cyclones and forest fragmentation have synergistic effects? A before–after study of rainforest vegetation structure at multiple sites

Abstract Ecological degradation within areas of remnant forest may be amplified if the effects of fragmentation interact with the effects of other environmental disturbances such as wind storms. We used before–after comparisons to assess the effects of Tropical Cyclone Larry on remnant and continuous rainforest in the Wet Tropics uplands of north‐eastern Australia. Vegetation structure was measured 3 years before the cyclone and 6 months afterwards, at eight continuous forest sites and eight remnants (6–37 ha), within 20 km of the cyclone's track. The cyclone caused extensive defoliation, felling and breakage of stems and branches (greatest among the trees >100 cm diameter which had around 50% stem loss), and increased litter and woody debris. Cyclone effects were strongly influenced by a site's spatial position (P = 0.005, 0.001 in multivariate analyses of overall damage). Maximum damage occurred 10–15 km south of the cyclone track, perhaps because of the additive effects of the west‐moving air at the southern eyewall combined with the cyclone's own rapid westward movement. Most fragments were south of the cyclone track, as a consequence of spatially selective deforestation practices, and therefore, showed greatest damage. However, once the effects of spatial position were considered, the independent differences in cyclone effects between fragments and continuous forest were lost (P = 0.23, 0.41 when north‐south distance was included as a covariate in analyses). The expected protection afforded by a continuous forest canopy seems to have disappeared in the face of extremely strong cyclonic winds and down‐draughts. Nevertheless, an interaction between fragmentation and disturbance may yet occur, during the period of post‐cyclone recovery, owing to the effects of landscape context on plant recruitment. For example, there was a higher diversity of exotic seedling germination in fragments, independent of the extent of cyclone damage.     

Morphofunctional analysis of Svobodaina species (Brachiopoda,Heterorthidae) from south‐western Europe

Geometric morphometric methods applied to the ventral muscle field outline of the various species of Svobodaina from south‐western Europe identify criteria for discriminating among this key cluster of brachiopod species. These data indicate the close relationship between the patterns of the ventral muscle field in the Svobodaina species and the environmental conditions where each inhabited; the fields are better developed in species related to high‐energy environments. For example, S. armoricana, with the smallest diductor scars, would have inhabited the quiet marine environments of the lower offshore or within protected lagoonal settings. S. feisti would have inhabited the upper offshore, a more energetic environment than S. armoricana. Finally, S. havliceki, with the largest diductor scars, would have thrived in the most energetic environments among all the south‐western European Svobodaina species, living just above the fair‐weather wave base in the lower shoreface. The palaeoecological results suggest a distribution of Svobodaina species during the Late Ordovician along an onshore–offshore transect across the shallow marine platforms of the Mediterranean margin of Gondwana. On the other hand, the occurrence in some localities of several species with overlapping ranges or within the same assemblage indicates that the biostratigraphical efficacy of the genus is restricted. Thus, the previously defined taxon‐range biozones characterized by Svobodaina species of the north Gondwanan margin are in need of reassessment. The morphology of Svobodaina may be a considerable aid to environmental analyses rather than to precise biostratigraphical correlations.