Remote sensing of photosynthetic-light-use efficiency of a Siberian boreal forest   总被引：3，自引：0，他引：3  

CAROLINE J. NICHOL  JON LLOYD  OLGA SHIBISTOVA  ALMUT ARNETH  CAROLA RÖSER  ALEXANDER KNOHL  SHIZUE MATSUBARA  JOHN GRACE 《Tellus. Series B, Chemical and physical meteorology》2002,54(5):677-687

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The Skaergaard Layered Series. Part VI. Excluded Trace Elements   总被引：1，自引：2，他引：1  

McBIRNEY  ALEXANDER R. 《Journal of Petrology》2002,43(3):535-556

In contrast to the smooth trends of major elements and mineralcompositions, the excluded trace elements in the SkaergaardLayered Series have an irregular distribution that does notconform to the normal trends of Rayleigh-type fractionation.Their concentrations are about constant or even decline throughthe Lower and Middle Zones before increasing sharply to reachmaximum concentrations 100–200 m above the Sandwich Horizon.As in the case of included elements, the relative concentrationsof excluded elements in coexisting phases deviate widely fromthose predicted by experimentally determined partition coefficientsunder presumed magmatic conditions. This is seen most clearlyin the immiscible melanogranophyres and conjugate ferrogabbros.Although the major elements conform to the experimentally determinedrelations for immiscible liquids, the trace elements do not;they follow a totally independent trend. The abrupt increasein the concentrations of excluded elements in the upper partof the intrusion could plausibly be attributed to an additionof new magma or to a density inversion that resulted in upwardmigration of a late liquid or fluid, but these possibilitiesare inconsistent with the compositional and spatial relationsof the upper parts of the intrusion. Although a late residualliquid certainly migrated upward, the most likely explanationfor the observed distribution of excluded elements is that thepartition coefficients were altered by volatile components,which gradually increased during the early stages of crystallizationthen began to exsolve near the top of the Middle Zone. KEY WORDS: igneous differentiation; Skaergaard intrusion  相似文献   

On the CO₂ exchange between the atmosphere and the biosphere: the role of synoptic and mesoscale processes     

DOUGLAS CHAN  CHIU WAI YUEN  KAZ HIGUCHI  ALEXANDER SHASHKOV  JANE LIU  JING CHEN  DOUGLAS WORTHY 《Tellus. Series B, Chemical and physical meteorology》2004,56(3):194-212

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Assessing the link between coastal morphology,wave energy and sea ice throughout the Holocene from Antarctic raised beaches          下载免费PDF全文

LAUREN MILLER SIMKINS  ALEXANDER RAY SIMMS  REGINA DEWITT 《第四纪科学杂志》2015,30(4):335-348

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Notes on the ecology and physiology of the Antarctic oribatid mite Maudheimia wilsoni     

LAURITZ SøMME  ALEXANDER STRøMME  KARL ERIK ZACHARIASSEN 《Polar research》1993,12(1):21-25

The oribatid mite Maudheimia wilsoni Dalenius was found to be numerous on the underside of stones at Jutulsessen (72°S, 3'E) in Dronning Maud Land, Antarctica. Daily temperature fluctuations of the microhabitat from as high as 19°C and to as low as – 17°C were observed during the austral summer. Optimal activity of the mites occurred at 10°C. Even in January the mean supercooling point of adult mites was as low as -30.8±4.7°C. Haemolymph osmolality ranged from 500 to 800mOsmol and thermal hystersis freezing points from −4.7 to −6.1°C. Adult mites had a mean water content of 43.6% and a water loss rate of 0.12 μgh⁻¹ at 15°C and 10% relative humidity.  相似文献   

Carbonates in fractures of Martian meteorite Allan Hills 84001: Petrologic evidence for impact origin     

EDWARD R. D. SCOTT  ALEXANDER N. KROT  AKIRA YAMAGUCHI 《Meteoritics & planetary science》1998,33(4):709-719

Abstract— Carbonates in Martian meteorite Allan Hills 84001 occur as grains on pyroxene grain boundaries, in crushed zones, and as disks, veins, and irregularly shaped grains in healed pyroxene fractures. Some carbonate disks have tapered Mg-rich edges and are accompanied by smaller, thinner and relatively homogeneous, magnesite microdisks. Except for the microdisks, all types of carbonate grains show the same unique chemical zoning pattern on MgCO₃-FeCO₃-CaCO₃ plots. This chemical characteristic and the close spatial association of diverse carbonate types show that all carbonates formed by a similar process. The heterogeneous distribution of carbonates in fractures, tapered shapes of some disks, and the localized occurrence of Mg-rich microdisks appear to be incompatible with growth from an externally derived CO₂-rich fluid that changed in composition over time. These features suggest instead that the fractures were closed as carbonates grew from an internally derived fluid and that the microdisks formed from a residual Mg-rich fluid that was squeezed along fractures. Carbonate in pyroxene fractures is most abundant near grains of plagioclase glass that are located on pyroxene grain boundaries and commonly contain major or minor amounts of carbonate. We infer that carbonates in fractures formed from grain boundary carbonates associated with plagioclase that were melted by impact and dispersed into the surrounding fractured pyroxene. Carbonates in fractures, which include those studied by McKay et al. (1996), could not have formed at low temperatures and preserved mineralogical evidence for Martian organisms.  相似文献   

Environmental Politics in New Zealand/ Aotearoa: Clashes and Commonality Between Māoridom and Environmentalists     

ALEXANDER GILLESPIE 《New Zealand geographer》1998,54(1):19-26

It has long been assumed that Māori¹, like many other indigenous peoples, have utilised ecologically sustainable practices. However, over recent years a chasm has developed between many conservationists and various Māori groupings as environmental objectives and philosophies have come into conflict. This article seeks to examine this chasm, and then move towards an understanding about what may really be the basis of the claim for sustainable practices in this area.  相似文献   

Indigenous amino acids in primitive CR meteorites     

Z. MARTINS  C. M. O'D. ALEXANDER  G. E. ORZECHOWSKA  M. L. FOGEL  P. EHRENFREUND 《Meteoritics & planetary science》2007,42(12):2125-2136

Abstract— –CR chondrites are among the most primitive meteorites. In this paper, we report the first measurements of amino acids in Antarctic CR meteorites. Three CRs, Elephant Moraine (EET) 92042, Graves Nunataks (GRA) 95229, and Grosvenor Mountains (GRO) 95577, were analyzed for their amino acid content using high‐performance liquid chromatography with UV fluorescence detection (HPLC‐FD) and gas chromatography–mass spectrometry (GC‐MS). Our data show that EET 92042 and GRA 95229 are the most amino acid–rich chondrites ever analyzed, with total amino acid concentrations ranging from 180 ppm to 249 ppm. The most abundant amino acids present in the EET 92042 and GRA 95229 meteorites are the α‐amino acids glycine, isovaline, α‐aminoisobutyric acid (α‐AIB), and alanine, with δ¹³C values ranging from +31.6‰ to +50.5‰. The carbon isotope results together with racemic enantiomeric ratios determined for most amino acids strongly indicate an extraterrestrial origin for these compounds. Compared to Elephant Moraine (EET) 92042 and GRA 95229, the more aqueously altered GRO 95577 is depleted in amino acids. In both CRs and CMs, the absolute amino acid abundances appear to be related to the degree of aqueous alteration in their parent bodies. In addition, the relative abundances of α‐AIB and β‐alanine in the Antarctic CRs also appear to depend on the degree of aqueous alteration.  相似文献   

Drilling Blake Nose: the search for evidence of extreme Palaeogene–Cretaceous climates and extraterrestrial events     

KROON  NORRIS  KLAUS  IAN T. ALEXANDER  LEON PAUL BARDOT  CHARLES E. BARKER  JEAN-PIERRE BELLIER  CHARLES D. BLOME  LEON J. CLARKE  JOCHEN ERBACHER  KRISTINA L. FAUL  MARY ANNE HOLMES  BRIAN T. HUBER  MIRIAM E. KATZ  KENNETH G. MACLEOD  SANDRA MARCA  FRANCISA C. MARTINEZ-RUIZ  ISAO MITA  MUTSUMI NAKAI  JAMES G. OGG  DOROTHY K. PAK  THOMAS K. PLETSCH  JEAN M. SELF-TRIAL  NICHOLAS J. SHACKLETON  JAN SMIT  WILLIAM USSLERIII  DAVID K. WATKINS  JOEN WIDMARK  & PAUL A. WILSON 《Geology Today》1998,14(6):222-226

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Aircraft vertical profiling of variation of CO₂ over a Canadian Boreal Forest Site: a role of advection in the changes in the atmospheric boundary layer CO₂ content     

ALEXANDER SHASHKOV  KAZ HIGUCHI  DOUGLAS CHAN 《Tellus. Series B, Chemical and physical meteorology》2007,59(2):234-243

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