Foraging behaviour,swimming performance and malformations of early stages of commercially important fishes under ocean acidification and warming     

Marta S. Pimentel  Filipa Faleiro  Tiago Marques  Regina Bispo  Gisela Dionísio  Ana M. Faria  Jorge Machado  Myron A. Peck  Hans Pörtner  Pedro Pousão-Ferreira  Emanuel J. Gonçalves  Rui Rosa 《Climatic change》2016,136(3-4):495-505

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Noble-gas evidence for geothermal activity in a karstic terrain: Rocky Mountains,Canada.     

Emanuel Mazor  Robert O. van Everdingen  H.Roy Krouse 《Geochimica et cosmochimica acta》1983,47(6):1111-1115

Geothermally heated fluids are identified as a component in warm (up to 54°C) springs in the southern Canadian Rocky Mountains. High concentrations of radiogenic He (10^?3 ccSTP/cc gas) and atmospheric Ne, Ar, Kr and Xe in the gases that vigorously bubble at the Fairmont Hot Spring, assign the latter to be a “drowned” fumarole, fed by geothermal steam. Up to 75% depletions in the atmospheric noble gases in several warm springs indicate contributions of residual geothermal water. On the other hand, in a few cases noble gases were found in excess (W) over the expected concentrations in airequilibrated recharge water. The observed “reversed” pattern of w_nc >W_Ar >W_kr >W_xe is interpreted as excess air, incorporated during recharge through karstic conduits. The mixing ratios of geothermal and karstic waters can be deduced.  相似文献   

Flow variability and hillslope hydrology     

D. D. Huff  R. V. O'Neill  W. R. Emanuel  J. W. Elwood  J. D. Newbold 《地球表面变化过程与地形》1982,7(1):91-94

Examination of spatial variability of streamflow in headwater areas can provide important insight about factors that influence hillslope hydrology. Detailed observations of variations in stream channel input, based on a tracer experiment, indicate that topography alone cannot explain flow variability. However, determination of changes in channel input on a small spatial scale can provide valuable clues to factors, such as structural geology that control subsurface flows.  相似文献   

Interactive effects of pH and temperature on native and alien mussels from the west coast of South Africa     

MP Emanuel  D Pillay  M van der Merwe  GM Branch 《African Journal of Marine Science》2020,42(1):1-12

Global warming and ocean acidification influence marine calcifying organisms, particularly those with external shells. Among these, mussels may compensate for environmental changes by phenotypic plasticity, but this may entail trade-offs between shell deposition, growth and reproduction. We assessed main and interactive effects of pH and temperature on four mussel species on the west coast of South Africa (33°48′ S, 18°27′ E) in October 2012 by comparing shell dissolution, shell growth, shell breaking force and condition index of two native species, the ribbed mussel Aulacomya atra and the black mussel Choromytilus meridionalis, and two aliens, the Mediterranean mussel Mytilus galloprovincialis and the bisexual mussel Semimytilus algosus. Live mussels and dead shells were exposed for 42 days to seawater of pH 7.5 or 8.0, at 14 °C or 20 °C. Low pH, high temperature and their combination increased shell dissolution of the two aliens but their growth rates and condition indices remained unchanged. Aulacomya atra also experienced greater shell dissolution at a low pH and high temperature, but grew faster in low-pH treatments. For C. meridionalis, shell dissolution was unaffected by pH or temperature; it also grew faster in low-pH treatments, but had a lower condition index in the higher temperature treatment. Shell strength was not determined by thickness alone. In most respects, all four species proved to be robust to short-term reduction of pH and elevation of temperature, but the native species compensated for greater shell dissolution at low pH by increasing growth rate, whereas the aliens did not, so their invasive success cannot be ascribed to benefits accruing from climate change.  相似文献   

Seismogenic Origin of the Ancient Avdat Ruins,Negev Desert,Israel     

Korjenkov  A. M.  Mazor  E. 《Natural Hazards》1998,18(3):193-226

The present communication addresses the potential use of damage features, observed in the ancient ruins of the Avdat archeological site (Negev Desert, Israel) as a tool to identify the seismic origin of the destruction there and roughly to determine the direction of seismic wave propagation. This revised version was published online in June 2006 with corrections to the Cover Date.  相似文献   

Einfluss der Lagenungenauigkeit von Anschlusspunkten bei Punktbestimmung Durch Bogenschnitt und Durch Vorwärtseinschneiden mit Gemessenen Winkeln und Entfernungen     

Emanuel Procházka 《Studia Geophysica et Geodaetica》1968,12(4):350-362

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Evaluating uncertainty in Landsat-derived postfire recovery metrics due to terrain,soil, and shrub type variations in southern California     

Emanuel A. Storey  Douglas A. Stow  Dar A. Roberts 《地理信息系统科学与遥感》2020,57(3):352-368

ABSTRACT

Temporal trajectories of apparent vegetation abundance based on the multi-decadal Landsat image series provide valuable information on the postfire recovery of chaparral shrublands, which tend to mature within one decade. Signals of change in fractional shrub cover (FSC) extracted from time-sequential Normalized Difference Vegetation Index (NDVI) data can be systematically biased due to spatial variation in shrub type, soil substrate, or illumination differences associated with topography. We evaluate the effects of these variables in Landsat-derived metrics of FSC and postfire recovery, based upon three chaparral sites in southern California which contain shrub community ecotones, complex terrain, and soil variations. Detailed validations of prefire and postfire FSC are based on high spatial resolution ortho-imagery; cross-stratified random sampling is used for variable control. We find that differences in the composition and structure of shrubs (inferred from ortho-imagery) can substantially influence FSC-NDVI relations and impact recovery metrics. Differences in soil type have a moderate effect on the FSC-NDVI relation in one of the study sites, while no substantial effects were observed due to variation of terrain illumination among the study sites. Arithmetic difference recovery metrics – based on NDVI values that were not normalized with unburned control plots – correlate in a moderate but significant manner with a change in FSC (R ² values range 0.47–0.59 at two sites). Similar regression coefficients resulted from using Landsat visible reflectance data alone. The lowest correlations to FSC resulted from Soil-Adjusted Vegetation Index (SAVI) and are attributed to the effects of the soil-adjustment factor in sparsely vegetated areas. The Normalized Burn Ratio and Normalized Burn Ratio 2 showed a moderate correlation to FSC. This study confirms the utility of Landsat NDVI data for postfire recovery evaluation and implies a need for stratified analysis of postfire recovery in some chaparral landscapes.  相似文献   

Equatorial Atlantic Ocean dynamics in a coupled ocean–atmosphere model simulation     

Emanuel Giarolla  Leo San Pedro Siqueira  Marcus Jorge Bottino  Marta Malagutti  Vinicius Buscioli Capistrano  Paulo Nobre 《Ocean Dynamics》2015,65(6):831-843

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Calc-Alkaline Magmatism at the Archean Proterozoic Transition: the Caico Complex Basement (NE Brazil)     

De Souza  Zorano Sergio; Martin  Herve; Peucat  Jean-Jacques; Jardim De Sa  Emanuel Ferraz; Macedo  Maria Helena De Freitas 《Journal of Petrology》2007,48(11):2149-2185

The Paleoproterozoic metaplutonic rocks of the CaicóComplex Basement (Seridó region, NE Brazil) provide importantand crucial insights into the petrogenetic processes governingcrustal growth and may potentially be a proxy for understandingthe Archean–Proterozoic transition. These rocks consistof high-K calc-alkaline diorite to granite, with Rb–Sr,U–Pb, Pb–Pb and Sm–Nd ages of c. 2·25–2·15Ga. They are metaluminous, with high Yb_N, K₂O/Na₂O and Rb/Sr,low I_Sr ratios, and are large ion lithophile elements (LILE)enriched. Petrographic and geochemical data demonstrate thatthey belong to differentiated series that evolved by low-pressurefractionation, thus resulting in granodioritic liquids. We proposea model in which the petrogenesis of the Caicó Complexorthogneisses begins with partial melting of a metasomaticallyenriched spinel- to garnet-bearing lherzolite (with high-silicaadakite melt as the metasomatic agent), generating a basic magmathat subsequently evolved at depth through fractional crystallizationof olivine, followed by low-pressure intracrustal fractionation.A subduction zone setting is proposed for this magmatism, toaccount for both negative anomalies in high field strength elements(HFSE) and LILE enrichment. Mantle-derived juvenile magmatismwith the same age is also known in the São Franciscoand West Africa cratons, as well as in French Guyana, and thusthe Archean–Proterozoic transition marks a very importantcontinental accretion event. It also represents a transitionfrom slab-dominated (in the Archean) to wedge-dominated post-Archeanmagmatism. KEY WORDS: calc-alkaline; magmatism; NE Brazil; Paleoproterozoic; petrogenesis  相似文献   

A new framework to determine general multimodal soil water characteristic curves     

Yan  Wei  Birle  Emanuel  Cudmani  Roberto 《Acta Geotechnica》2021,16(10):3187-3208

Acta Geotechnica - A soil water characteristic curve (SWCC) model named as discrete-continuous multimodal van Genuchten model with a convenient parameter calibration method is developed to describe...  相似文献