The systematic position of Equus hydruntinus, an extinct species of Pleistocene equid     

Ariane Burke  Vera Eisenmann  Graeme K. Ambler 《Quaternary Research》2003,59(3):459

Palaeolithic people commonly hunted Equus hydruntinus, an extinct species of equid whose cursorial body proportions suggest an adaptation to semi-arid conditions. Despite the frequency with which it is encountered in fossil deposits, only partial cranial remains have been reported until now. As a result, the systematic affiliation of the species remains a subject of controversy. Two nearly complete E. hydruntinus crania are presented here for the first time. These skulls show that E. hydruntinus is a distinct species, more closely related to the hemiones (Asiatic asses) than to any other equid. This suggests that the social organisation of E. hydruntinus followed one of two known equid sociotypes: resource defense territoriality.  相似文献   

The systematic position of Equus hydruntinus, an extinct species of Pleistocene equid☆     

Ariane Burke  Vera EisenmannGraeme K Ambler 《Quaternary Research》2003,59(3):459-469

Palaeolithic people commonly hunted Equus hydruntinus, an extinct species of equid whose cursorial body proportions suggest an adaptation to semi-arid conditions. Despite the frequency with which it is encountered in fossil deposits, only partial cranial remains have been reported until now. As a result, the systematic affiliation of the species remains a subject of controversy. Two nearly complete E. hydruntinus crania are presented here for the first time. These skulls show that E. hydruntinus is a distinct species, more closely related to the hemiones (Asiatic asses) than to any other equid. This suggests that the social organisation of E. hydruntinus followed one of two known equid sociotypes: resource defense territoriality.  相似文献   

MM Herculis: An eclipsing binary of the RS CVn type     

J. R. Sowell  D. S. Hall  G. W. Henry  E. W. Burke Jr.  E. F. Milone 《Astrophysics and Space Science》1983,90(2):421-435

Differential photoelectric photometry inV, B, andU has been obtained for the eclipsing binary MM Her, a member of the RS Canum Venaticorum class. The light outside eclipse was Fourier-analyzed to study the wave. The migration and amplitude of the wave and the mean light level of the system now have been monitored from 1976 through 1980. The phase of wave minimum has decreased from 0 _. ^P 80 to 0 _. ^P 25, the wave amplitude has varied between 0 _. ^m 06 and 0 _. ^m 12, and the mean light level has fluctuated between 0.94 and 0.99. Observations within eclipse revealed that the eclipses are partial, not total as previously thought, and a new time of mid-eclipse was found to be JD (hel.)=2444 500.6665±0 _. ^d 0008. The Russell model was used to solve the 1980 light curve. Elements of the rectified light curve werei=86 _. ^° 35±0 _. ^° 09,r _h =0.070±0.002,r _c =0.125±0.001,L _h (V)=0.585±0.008 andL _h (B)=0.683±0.010. The geometric elements were forced on the pre-1980 light curves and found to be compatible. With these elements and previously obtained double-lined radial velocity curves, new absolute dimensions have been calculated: 1.18M and 1.58R for the hotter star and 1.27M and 2.83R for the cooler star. By plotting color indices on the color-color curve, spectral types of G2V and K21V were found, each uncertain by a couple of subclasses.Guest Observer Kitt Peak National Observatory, operated by the Association of Universities for Research in Astronomy, under contract with the National Science Foundation.  相似文献   

Maximum extent and readvance dynamics of the Irish Sea Ice Stream and Irish Sea Glacier since the Last Glacial Maximum     

J. D. Scourse  R. C. Chiverrell  R. K. Smedley  D. Small  M. J. Burke  M. Saher  K. J. J. Van Landeghem  G. A. T. Duller  C. Ó Cofaigh  M. D. Bateman  S. Benetti  S. Bradley  L. Callard  D. J. A. Evans  D. Fabel  G. T. H. Jenkins  S. McCarron  A. Medialdea  S. Moreton  X. Ou  D. Praeg  D. H. Roberts  H. M. Roberts  C. D. Clark 《第四纪科学杂志》2021,36(5):780-804

The BRITICE-CHRONO Project has generated a suite of recently published radiocarbon ages from deglacial sequences offshore in the Celtic and Irish seas and terrestrial cosmogenic nuclide and optically stimulated luminescence ages from adjacent onshore sites. All published data are integrated here with new geochronological data from Wales in a revised Bayesian analysis that enables reconstruction of ice retreat dynamics across the basin. Patterns and changes in the pace of deglaciation are conditioned more by topographic constraints and internal ice dynamics than by external controls. The data indicate a major but rapid and very short-lived extensive thin ice advance of the Irish Sea Ice Stream (ISIS) more than 300 km south of St George's Channel to a marine calving margin at the shelf break at 25.5 ka; this may have been preceded by extensive ice accumulation plugging the constriction of St George's Channel. The release event between 25 and 26 ka is interpreted to have stimulated fast ice streaming and diverted ice to the west in the northern Irish Sea into the main axis of the marine ISIS away from terrestrial ice terminating in the English Midlands, a process initiating ice stagnation and the formation of an extensive dead ice landscape in the Midlands.  相似文献   

厄尔尼诺和南方涛动对中国水稻产量的影响(英文)     

邓祥征  黄季焜  乔方彬  Marshall Burke  Scott Rozelle  David Battisti 《地理学报(英文版)》2010,20(1)

This paper aims to demonstrate the relationships between ENSO and rice production of Jiangxi province in order to identify the reason that ENSO might have little effect on Chinese rice production. Using a data set with measures of Jiangxi's climate and rice production,we find the reason that during 1985 and 2004 ENSO's well correlated with rainfall did not promote Chinese rice production. First,the largest effects of ENSO mostly occur in the months when there is no rice in the field. Second,there is almost ...  相似文献   

Nitrogen-rich fluid in the upper mantle: fluid inclusions in spinel dunite from Lanzarote,Canary Islands   总被引：2，自引：0，他引：2  

T. Andersen  E. A. J. Burke  E. -R. Neumann 《Contributions to Mineralogy and Petrology》1995,120(1):20-28

Fluid inclusions, ranging from pure N₂ to pure CO₂, occur in olivine porphyroclasts in spinel dunite xenoliths (chrome-diopside suite) from two localities within the Quaternary to Historic alkaline lavas of Lanzarote, Canary Islands. This is the first report of fluid inclusions containing major amounts of N₂ in mantle xenoliths. The nitrogen-rich fluid inclusions predate at least one generation of nitrogen-free carbon dioxide inclusions; textural evidence indicates that the inclusions were trapped within the upper mantle. Some of the nitrogen-rich fluid inclusions are intimately associated with solid inclusions of spinel. The nitrogen-rich fluid was most likely produced in-situ, by oxidation-dehydration reactions destabilizing ammonium-bearing silicate minerals (phlogopite, amphibole), increasing oxygen fugacity or, possibly, increasing temperature of the mantle. This process could be related to an event of CO₂ and silicate melt injection at 6–8 kbar (Neumann et al., in press), or to some earlier event in the evolution of the mantle beneath Lanzarote. The existence of a N₂-rich fluid phase in at least some mantle lithology(ies) at certain conditions is demonstrated by these data. This discovery has consequences for the understanding of the evolution of the mantle below the Canary Islands, as well as for the global nitrogen budget.  相似文献   

A tribute to Jacques Touret     

Tom Andersen  Marie-Luce Frezzotti  Ernst A. J. Burke 《Lithos》2001,55(1-4):ix-xi

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Immigration of larvae of fall/winter spawning marine fishes into a North Carolina estuary     

Stanley M. Warlen  John S. Burke 《Estuaries and Coasts》1990,13(4):453-461

Larval fishes were sampled weekly from late fall to early spring in the Newport River estuary just inside Beaufort Inlet, North Carolina. Quantitative samples were taken during darkness at mid-flood tide with paired 60-cm bongo nets (505-μm mesh). Larvae of 22 species from 15 families were collected. Seventy-seven percent of the species and 97% of the individuals were fishes that had been spawned on the continental shelf and had immigrated to the estuary. In descending order, the five most abundant species, accounting for 90% of the individuals, were spot (Leiostomus xanthurus), Atlantic croaker (Micropogonias undulatus), Atlantic menhaden (Brevoortia tyrannus), pinfish (Lagodon rhomboides), and speckled worm ell (Myrophis punctatus). Most species immigrated through-out the winter and into spring, but there were distinct patterns in their temporal abundances.  相似文献   

REPLY TO the preceding Discussion by Yoram Eckstein and J. Charles Burke of "An Integrated Approach to Identifying the Salinity Source Contaminating a Ground-Water Supply"     

Yoram Eckstein  J. Charles Burke 《Ground water》1990,28(6):951-952

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Impacts of acid emissions from Nevado del Ruiz volcano, Colombia, on selected terrestrial and aquatic ecosystems     

Roderic A. Parnell Jr.  Kelly J. Burke 《Journal of Volcanology and Geothermal Research》1990,42(1-2)

Emissions of acidic gases and thermal waters from Nevado del Ruiz volcano have recently increased in concert with the November 13, 1985 eruption. This study examines the downwind and downstream effects of these emissions on alpine ecosystems high on the slopes of the volcano (4100 m) and on coffee plantations at lower elevations (< 2000 m) and greater distances from the active vent (> 30 km). Samples of bulk deposition, rain, soils, soil solutions, and streams were collected over a six-month period (January–July, 1987) to examine the impacts of this volcanogenic acidity.Bulk deposition falling on the higher slopes of the volcano is usually acidified; however, deposition reaching the distal coffee plantations seldom is acidic. The sources of the acids are hydrogen chloride and sulfur dioxide in the plume of the volcano. Although sulfur dioxide is by far the more abundant gas, hydrogen chloride is most responsible for acidification of rain falling on the slopes of the volcano. With distance from the vent, the chloride/sulfate ratio drops exponentially. The only major influence on regional precipitation chemistry in addition to the volcano appears to be land-use-related activities around the coffee plantations. Deposition on these areas is enriched by an order of magnitude in nitrate and base cations, compared to all other stations.Throughfall chemistry in the coffee plantations shows a dramatic response to occasional acid-rain events. A base-leaching process on coffee plant leaves is triggered by acid rain. For each equivalent of hydrogen ion in rain on the leaf surface, over 23 equivalents of potassium ion are leached from the leaf.In spite of this dramatic response by the vegetation, the plantation soils appear relatively unaffected by acidic deposition. In contrast, the alpine soils on the volcano exhibit low pHs, high sulfate and chloride concentrations in soil solutions, and high extractable sulfate concentrations. All of these factors indicate that these soils have undergone significant acid loading.While the deposition of the region is acidified by hydrogen chloride, the streams flowing off the volcano are apparently acidified by sulfuric acid in thermal waters discharging into the streams. The acidity of these streams decreases downstream, while the silica concentrations increase downstream. The composition of stream water is most influenced by thermal-water discharges as well as equilibrium dissolution of amorphous silica glass and non-equilibrium leaching of unweathered ash.The impacts of acid gases and thermal water released from the volcano appear to be restricted to ecosystems on the slope of the volcano. The only impact of Nevado del Ruiz on surrounding coffee plantations appears to be potassium leaching of coffee leaves from occasional acid-deposition events.  相似文献