Depositional environments and facies development of the Cenomanian–Turonian Galala and Maghra el Hadida formations of the Southern Galala Plateau (Upper Cretaceous,Eastern Desert,Egypt)

The Cenomanian–Turonian (Upper Cretaceous) Galala and Maghra el Hadida formations of the Southern Galala Plateau in Wadi Araba (northern Eastern Desert, Egypt) represent marine depositional systems developing in response to the early Late Cretaceous transgression at the southern margin of the Neotethyan Ocean in tropical paleolatitudes. A facies analysis (litho-, bio- and microfacies) of these successions shows the presence of 22 facies types (FTs, six are related to the Galala Formation, while the Maghra el Hadida Formation is represented by 16 FTs). The Galala Formation was deposited in a fully marine lagoonal environment developing in response to a latest Middle to early Late Cenomanian transgression. The rich suspension- and deposit-feeding macrobenthos of the Galala Formation indicate meso- to eutrophic (i.e., green water) conditions. The facies types of the uppermost Cenomanian–Turonian Maghra el Hadida Formation suggest deposition on a homoclinal carbonate ramp with sub-environments ranging from deep-subtidal basin to intertidal back-ramp. Major and rapid shifts in depositional environments, related to (relative) sea-level changes, occurred in the mid-Late Cenomanian, the Early–Middle Turonian boundary interval, the middle part of the Middle Turonian and the Middle–Late Turonian boundary interval.     

Biostratigraphy and Paleobiogeographic implications of the Cenomanian–Early Turonian Ostracods of Egypt

The present study deals with the Cenomanian–early Turonian ostracods in the southern Sinai, Egypt. The investigated sequence includes the Raha and Abu Qada formations. The Raha Formation consists of distinctive Cenomanian taxa such as Cytherella aegyptiensis, Veeniacythereis maghrebensis, V. jezzineensis, V. streblolophata streblolophata, Monoceratina trituberculata, and Glenocythere reticulata. Based on the ostracod species, four local biozones are recognized, including Veeniacythereis jezzineensis – Metacythereopteron berbericum, Cytherella eosulcata – Xestoleberis derorimensis, Amphicytherura ziregensis and Perissocytheridea istriana – Cythereis fahrioni. The paleobiogeography of the considered ostracods suggests that there are two bioprovinces, the first of which is the North African province and includes Egypt, Tunisia and Algeria. The second bioprovince represents the Middle East province and includes Lebanon, Oman and Iran. The strong resemblance between the two bioprovince indicates a relatively good communication along the margin of Southern Tethys during the Cenomanian and improved marine ostracod exchange.     

Gradualistic characean lineages in the Upper Cretaceous–Palaeocene of southern Europe

Two charophyte lineages from the Upper Cretaceous–Palaeocene of southern Europe are described here, constituting a useful biostratigraphic tool for correlating non-marine stratigraphic sequences. The Peckichara pectinata lineage, ranging from the middle Campanian to the middle–upper Maastrichtian, consists of four successive gyrogonite morphotypes that displayed progressively more complex gyrogonite ornamentation and increasingly smaller gyrogonites with time. The Peckichara sertulata lineage, ranging from the middle Campanian to the Danian, consists of three morphotypes that followed a more common evolutionary trend, developing progressively larger gyrogonites without any changes in ornamentation. Intermediate forms between the successive morphotypes suggest that they corresponded to anagenetic varieties of the same evolutionary species rather than to separate species. The different trends observed appear to be palaeoenvironmentally controlled. The grades of the P. pectinata lineage first occurred in permanent lakes that later shifted to fluvial influenced floodplain ponds, this shift accounting for the reduction in gyrogonite size. By contrast, the P. sertulata lineage mainly occurred in permanent lakes, where stable palaeoenvironmental conditions enabled a steady rise in gyrogonite size to increase the space available for the zygote.     

Bottom-Water Conditions in a Marine Basin after the Cretaceous–Paleogene Impact Event: Timing the Recovery of Oxygen Levels and Productivity

An ultra-high-resolution analysis of major and trace element contents from the Cretaceous–Paleogene boundary interval in the Caravaca section, southeast Spain, reveals a quick recovery of depositional conditions after the impact event. Enrichment/depletion profiles of redox sensitive elements indicate significant geochemical anomalies just within the boundary ejecta layer, supporting an instantaneous recovery –some 10² years– of pre-impact conditions in terms of oxygenation. Geochemical redox proxies point to oxygen levels comparable to those at the end of the Cretaceous shortly after impact, which is further evidenced by the contemporary macrobenthic colonization of opportunistic tracemakers. Recovery of the oxygen conditions was therefore several orders shorter than traditional proposals (10⁴–10⁵ years), suggesting a probable rapid recovery of deep-sea ecosystems at bottom and in intermediate waters.     

Vegetation coverage,species richness,and dune stability in the southern part of Gurbantünggüt Desert

This study investigated the relationship between vegetation coverage, species richness, and environmental factors, and also analyzed the relationship between vegetation coverage, species richness, and dune stability in different terrains, in the southern part of Gurbantünggüt Desert in China. The results showed that the order of vegetation coverage and species richness was greatest in middle areas, followed by the eastern areas, with the western areas being sparse. On a large scale, precipitation from April to June determined the amount of vegetation coverage. On a small scale, vegetation coverage was influenced by the type of terrain and the water and salt content in soils. Species richness of vegetation was determined by soil water and salt content on both the large and small scales. There were also remarkable differences in relative wind erosion among the different terrains and their order was: crest, slope, and inter-dune in descending order. The correlations between wind erosion and vegetation coverage and species richness were influenced by the type of terrain. Furthermore, there were significant correlations between wind erosion and vegetation coverage and species richness in dune slopes and crests. There was, however, no significant correlation between wind erosion and vegetation coverage and species richness in inter-dune sites. Vegetation coverage was the dominant factor influencing wind erosion in both slopes and crests. Species richness may have an impact on wind erosion through vegetation coverage in both slopes and crests. These results suggest that the effect of terrain type should be fully considered during the establishment of vegetation cover in the desert.     

Morphologic variation of two key biostratigraphical proteaceous-like pollen taxa across the Cretaceous–Paleogene boundary in northern South America

Echitriporites trianguliformis and E. suescae comb. nov. are two species of proteaceous-like triaperturate pollen that have been widely reported in several sedimentary sequences from northern South America, especially in Colombia and Venezuela. Despite their biostratigraphic significance and because of their morphological similarity, distinction between the two species has been difficult, leading to a biased understanding of their chronostratigraphic ranges. In this study, we compare 75 pollen grains spanning the Maastrichtian–Danian time interval through traditional and geometric morphometrics, and a newly proposed Procrustes-based method (index of pollen curvature). Traditional assessments show subtle variation between specimens; however, geometric morphometrics and the curvature index allow quantifying morphological differences in the degree of concavity-convexity through time. Therefore, geometric morphometrics and curvature index results enable us to constrain the stratigraphic ranges of both taxa. We suggest a coetaneous range for E. trianguliformis and E. suescae comb. nov. during the Late Cretaceous, but the presence of only E. trianguliformis after the Cretaceous–Paleogene boundary event. In addition, we propose a threshold value of 1.5 µm for the curvature index as a tool for distinguishing between these two taxa. We conclude that the combination of geometric morphometrics and the curvature index provides a powerful tool to distinguish between morphological closely-related pollen taxa that are difficult to distinguish through both light microscope visual comparisons and statistical analysis of morphometric measurements.     

Land-use history of the Axlarp area in the Småland uplands,southern Sweden: palaeoecological and archaeological investigations

The results of pollen analysis, magnetic measurements (SIRM), and archaeological and historical investigations, in the Axlarp area are presented. With respect to natural conditions and the distribution of prehistoric features, this area is typical of the higher parts of the Småland uplands, which, agriculturally, is a marginal region of southern Sweden. The study shows that farming in the Axlarp area began at ca. 700 B.C. (dates in calibrated/calendar years). The period 700 B.C.-A.D. 500 was characterized by shifting cultivation of Hordeum and Triticum and much pasture. Between A.D. 500 and A.D. 1200 farming declined but some pasturage was still practised, possibly on a seasonal basis. Two farms were established in the Middle Ages, probably between A.D. 1200–1300. Cereals were sown in stone-cleared fields and pastoral farming and hay making was carried out. One farm was deserted during the 15th or early 16th century and the other developed into the hamlet Axlarp whose farmers practised a three-course cropping system. Land-use history as recorded in the pollen diagram can be related to activities associated with these farms. Cereals grown after A.D. 1200 included Hordeum and Avena, and possibly Triticum and Secale. There are no indications of slash-and-burn cultivation in the area.     

Horizontal mesoscale distribution of phytoplankton in the Tvärminne sea area,southern Finland

Horizontal distribution of phytoplankton was studied by sampling two grids, both having 16 sampling points. The distance between sampling points was 10 m. Phytoplankton species were enumerated by inverted microscopy and the observed distribution patterns were compared with a random distribution. Contagious distribution was common among the species studied. Both actively moving and passively drifting species showed significant contagiousness in their distribution. Actively moving and passively drifting species showed different distribution patterns. The effects of horizontal heterogeneity on phytoplankton sampling are discussed.     

Paleoenvironmental and paleoclimatic changes during the Late Cretaceous and Cretaceous–Paleogene (K/Pg) boundary transition in Tattofte,External Rif,northwestern Morocco: implications from dinoflagellate cysts and palynofacies

This paper presents a quantitative study of dinoflagellate cysts (dinocysts) and palynofacies of the Campanian–Danian marly succession at the village of Tattofte (western External Rif, northwestern Morocco). The paleoenvironmental and paleoclimatic interpretations, inferred from this palynologic analysis, are compared to coeval sequences of other areas in the Northern Hemisphere. Changes in the relative abundances of dinocyst taxa, which are paleoenvironmental indicators, throughout the section suggest a deposition in a marine inner to outer neritic setting. The upper Campanian dinocyst assemblage is characterized by the presence of outer neritic-oceanic and low productivity indicator taxa (e.g., Spiniferites spp., Odontochitina spp.) and cold-water taxa (e.g., Manumiella spp., Chantangiella spp., Laciniadinium spp.), whereas, the lower Maastrichtian assemblage is characterized by inner neritic, high productivity and warm-water indicator taxa (e.g., Palaeocystodinium spp., Andalusiella spp.). The upper Maastrichtian dinocyst assemblage displays a return to an outer neritic environment under a transgressive regime, but with a cooling pulse and a moderate productivity. However, the Cretaceous–Paleogene (K/Pg) boundary interval records remarkable changes in the relative abundances of dinocyst taxa, indicating an inner neritic (coastal) setting, which is the most proximal in the study section; such changes reflect instable paleoenvironmental conditions which may be related to global cooling periods, likely caused by the Deccan volcanism in India and/or the Chicxulub asteroid impact in Mexico at the K/Pg boundary. In the Danian, the dinocyst relative abundances indicate a gradual return to stable environmental conditions.A quantitative analysis of the kerogen plots (palynomorphs, phytoclasts and amorphous organic matter (AOM)) reveals five types of palynofacies, generally indicating oxic to suboxic marine environments. The upper Campanian and upper Maastrichtian (lowermost part) strata are characterized by a playnofacies (V), indicating a distal shelf, while the lower Maastrichtian and lower Danian (uppermost part) strata record a playnofacies (III), reflecting an intermediate inner-outer neritic environment. However, the K/Pg boundary transition is characterized by playnofacies types (I) and (II), indicating a proximal (coastal) environment.     

The composition,structure, and dynamics of the nekton of the upper epipelagic layer in the Aleutian and Commander basins,western Bering Sea,in the fall seasons of 2002–2013

The data on the composition and abundance of nekton species and their interannual variations within the upper epipelagic layer (0–50 m) in the Aleutian and Commander basins in the western Bering Sea that are considered in the article were collected during complex surveys that were conducted by the Pacific Research Fisheries Center in September and October of 2002–2013. The core species structures of the nekton communities in these two areas were similar: the chum salmon Oncorhynchus keta and the boreopacific gonate squid Boreoteuthis borealis were the most abundant species. Simpson’s dominance index varied synchronously in both areas, with higher values in the Aleutian Basin, until 2009. In the subsequent years, the values of the index for the studied areas became equal and varied asynchronously. An analysis of abundance showed that two types of species structure most often prevailed (with the dominance of either chum salmon or squid); in some years the species structure differed from that in other years. Species of the low-boreal and low-boreal-subtropical complexes were more abundant in the Commander Basin, reaching particularly high proportions in 2006, 2008, and 2012. Certain species showed similarity in the year-to-year dynamics of their abundance; however, these coincidences were frequently accidental. After the climate regime shift in 2006–2007, the total biomass of nekton in the Aleutian Basin decreased from 3241 to 1736 kg/km² (46%); in the Komandorskiye Basin it decreased from 2459 to 1976 kg/km² (20%).     

Investigation of EEG abnormalities in the early stage of Parkinson’s disease

The objective of the present study was to investigate brain activity abnormalities in the early stage of Parkinson’s disease (PD). To achieve this goal, eyes-closed resting state electroencephalography (EEG) signals were recorded from 15 early-stage PD patients and 15 age-matched healthy controls. The AR Burg method and the wavelet packet entropy (WPE) method were used to characterize EEG signals in different frequency bands between the groups, respectively. In the case of the AR Burg method, an increase of relative powers in the δ- and θ-band, and a decrease of relative powers in the α- and β-band were observed for patients compared with controls. For the WPE method, EEG signals from patients showed significant higher entropy over the global frequency domain. Furthermore, WPE in the γ-band of patients was higher than that of controls, while WPE in the δ-, θ-, α- and β-band were all lower. All of these changes in EEG dynamics may represent early signs of cortical dysfunction, which have potential use as biomarkers of PD in the early stage. Our findings may be further used for early intervention and early diagnosis of PD.     

Factor analysis of the impact of the environment on microbial communities in the tvärminne area, southern coast of Finland

Data already examined by regression analysis were subjected to factor analysis to scrutinize the effects of environmental factors on microbial populations in the brackish waters of the Tv?rminne archipelago on the southern coast of Finland. Water samples were collected from 1.0-m depth at one point in Tv?rminne Storfj?rd, 71 times over about 2 years. Twenty-six parameters were determined on each sample, 10 of environmental and 16 of microbiological type. The correlations between the parameters were factorized using the principal axis solution, and eight factors chosen for further consideration were rotated by the varimax method. The major part of the variance (about 90% of the total communality) of the microbiological parameters was covered by five factors, interpreted as phytoplankton blooms, the periods before and after the blooms, freshwater outflows, and water temperature. Wind variables were components in the factors interpreted as freshwater outflows. Rainfall played a minor part in the total variance of the microbial community, but it washed yeasts and proteolytic bacteria from the land into the study area. The eight factors selected covered about 60 to 98% of the variance of the microbiological parameters. The highest values (above 90%) were obtained for direct counts of bacteria, for plate counts of mesophilic and polymyxin-resistant bacteria, and for the two community respiration parameters; the lowest values (60 to 75%) were obtained for H(2)S-producing and proteolytic bacteria.     

Annual variations in the concentrations of Betula pollen in the London area, 1961–1990

Annual variations in the ambient concentrations of Betula pollen monitored by volumetric sampling at sites in London and also at a site to the South of the city between the years 1961–1990 are analysed in relation to the main meteorological parameters. Attention is focussed on variations in the start and duration of the seasons and on the annual patterns of pollen abundance. Consideration is given also to the variation in the severity of seasons. The paper examines possible rhythms in the annual production of Betula pollen and develops empirical regression models from the analyses of the trends to predict the main characteristics of the seasons.     

Molecular Clocks and the Timing of the Placental and Marsupial Radiations in Relation to the Cretaceous–Tertiary Boundary

Paleostratigraphic estimates of divergence time for nine independent cladogenic events within Mammalia, ranging from 14 to 130 million years, were regressed against Tamura–Nei-corrected 12S rRNA transversions. Relative rate-adjusted distances were also regressed against paleostratigraphic divergence times. The resulting equations were used to estimate interordinal divergence times within Eutheria and Metatheria for a data set that includes representatives of all orders in each infraclass. Without the adjustment for rate variation, divergence times range from 34 to 156 million years for placental orders, versus 32 to 86 million years for marsupial orders. With rate adjustments, the range of divergence estimates decreases to 53 to 133 million years for placentals versus 40 to 79 million years for marsupials. The effect of rate adjustments is most noticeable for carnivores and perissodactyls, where rates are slow, and proboscideans, where rates are fast. In agreement with studies based on nuclear genes, both unadjusted and rate-adjusted estimates of sequence divergence indicate that the majority of placental orders originated before the terminal Cretaceous extinction. Exceptions include the perissodactyl–carnivore split and cladogenesis among paenungulate orders. Most marsupial orders, in turn, may have originated in the early Tertiary although didelphimorphs, at least, appear to have split from other lineages in the late Cretaceous. Marsupial divergence times based on 12S rRNA data are in good agreement with estimates based on single-copy DNA hybridization and disagree with the suggestion of Hershkovitz (1992) that Dromiciops separated from other marsupials in the Jurassic.     

Social–ecological dynamics of change and restoration attempts in the Chihuahuan Desert grasslands of Janos Biosphere Reserve,Mexico

Shrub encroachment and declining grass production are widespread throughout the grasslands and savannas of the Mexico–US borderlands, with negative consequences for ecosystem services, livestock production, and native biodiversity. The problem suggests a complex interaction of social and ecological drivers that are not well understood. Using the Chihuahuan Desert grasslands of the Janos Biosphere Reserve of northern Mexico as a case study, we sought to understand the social–ecological context that shaped landscape change. Our approach included a synthesis of the historical literature and interviews with local residents, with the goal of facilitating long-term grassland restoration. Findings indicate that recent changes in Chihuahuan Desert grasslands are likely related to the co-occurrence of heavy grazing, fire suppression, and the elimination of key species, including prairie dogs and native ungulates. Local residents widely perceive both fire and prairie dogs to be destructive to grasslands and livelihoods. Over the last 50 years, evolving land tenure policies have fragmented the landscape into smaller parcels which typically produce an insufficient livelihood from cattle despite high stocking rates. Declining cattle profitability has motivated the sale and conversion of rangelands to more profitable croplands irrigated with groundwater. Since the founding of the Janos Biosphere Reserve in 2009, universities, local cattle operators, conservation organizations, and federal agencies have begun collaborating on restoration activities. While complete restoration of grasslands is unlikely, progress appears possible largely because of the willingness of local residents to try new management practices that may improve their ability to benefit from the land.     

Composition and spatial distribution of microencrusters and microbial crusts in upper Jurassic–lowermost Cretaceous reef limestone (Torinosu Limestone,southwest Japan)

Tethyan microencrusters and microbial crusts, most of them previously unknown in Japanese Mesozoic biotas, are present in the uppermost Jurassic–lowermost Cretaceous Torinosu Limestone distributed in southwestern Japan. They construct reefal facies together with reef-forming metazoans. Bacinella irregularis and Lithocodium aggregatum are quantitatively most important, while subordinate constituents include Thaumatoporella parvovesiculifera, Koskinobullina socialis , Iberopora bodeuri , Girvanella sp. and Tubiphytes morronensis. They are especially common in the shallow-water reefal facies, but appear micritic in outcrops. Microencrusters and microbial crusts can only be recognized in thin sections, and they grow around the reef building metazoans and form bindstone. Each microencruster exhibits some specific spatial distribution associated with its paleoecology. Similarities with the taxonomic composition of the upper Jurassic Tethyan microencruster association imply that the community extended geographically at least to the Tethyan gateway where the Japanese Island Arc was located.     

Ethnicity and biodemographic structure in the Arbëreshe of the province of Cosenza, southern Italy, in the XIX century

Cultural and environmental factors interact in determining the genetic structure of human populations. Bio-demographic investigations of ethnic minorities are able to disentangle the influences that these two components have on the evolution of the genetic structure of a population. The ethnic minority of the Arb?reshe of the province of Cosenza (Calabria, southern Italy) is analyzed in this paper and its bio-demographic structure in the early 1800s is compared with that of neighboring Italian populations. The data derive from surnames recorded in the birth registers of the 19 Arbdreshe municipalities of the province of Cosenza and in 5 non-Arb?reshe municipalities of the same province. Isonymy and repeated pairs of surnames are used to analyze the bio-demographic structure of these populations, while analysis of isonymic relationships is used to investigate the variability between populations. Higher values of marital isonymy and subdivision into subpopulations characterize the Arb?reshe populations with respect to their non-Arb?reshe neighbors. However, the high range of variability of these parameters suggests a strong influence of geographic location on the marriage pattern of each community. At the same time, cultural differences linked to group identity had a strong impact in limiting marriage exchanges between the different ethnic groups living in the province of Cosenza in the early 1800s. In fact, the analysis of isonymic relationships demonstrates that geographic location shaped kinship patterns among the Arbereshe communities, but it also shows that the non-Arb?reshe neighbors formed a clearly separate reproductive cluster.     

Serum LH,progesterone and estradiol-17β levels throughout the ovarian cycle,during the early stage of pregnancy and after the parturition and the abortion in the common marmoset,Callithrix jacchus

In the ovarian cycle of common marmosets, serum progesterone began to increase at two to three days after estradiol-17β or LH surge, attained a peak of 25–70 ng/ml and then declined to a level of under 2 ng/ml before the ensuing rise in estradiol-17β and LH. Serum estradiol-17β increased to 700–5,500 pg/ml during the luteal phase, synchronizing with progesterone. It is suggested that the corpus luteum secreted estradiol-17β as well as progesterone. The cycle length as determined from the interval between successive LH surges was approximately 28 days. During the luteal phase, the levels of progesterone and estradiol-17β were higher than in Old World monkeys and women, but marmosets were not accompanied by any clinical symptoms due to excessive progesterone and estradiol-17β. This suggests that such unresponsiveness to progesterone and estradiol-17β in marmosets reflects the small amount of estradiol-17β receptor and presumably also the lower function of the post receptor system. Recovery of the post-partum ovarian cycle in two marmosets differed from that observed in Old World monkeys and women. The first LH surge was found on the ninth and tenth day after parturition and the first ovulation led to the next pregnancy. This suggests that the suckling stimulus of newborns in the common marmoset does not cause any delay in recovery of the ovarian cycle. In three cases of abortion, the recovery of the ovarian cycle was almost the same as that in the case of normal parturition: the first LH surge appeared on the 10th, 14th, and 34th day after abortion.