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  • 1
    Publication Date: 2011-09-29
    Print ISSN: 0001-1541
    Electronic ISSN: 1547-5905
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Published by Wiley on behalf of American Institute of Chemical Engineers.
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  • 2
    Publication Date: 2011-11-18
    Print ISSN: 0043-1397
    Electronic ISSN: 1944-7973
    Topics: Architecture, Civil Engineering, Surveying , Geography
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 3
    Publication Date: 2011-11-19
    Description: Climate change is expected to be a significant threat to biodiversity, including crop diversity at centers of origin and diversification. As a way to avoid food scarcity in the future, it is important to have a better understanding of the possible impacts of climate change on crops. We evaluated these impacts on maize, one of the most important crops worldwide, and its wild relatives Tripsacum and Teocintes. Maize is the staple crop in Mexico and Mesoamerica and there are currently about 59 described races in Mexico, its center of origin. In this study, we modeled the distribution of maize races and of its wild relatives in Mexico for the present and in two time periods in the future (2030 and 2050), to identify the potentially most vulnerable taxa and geographic regions in the face of climate change. Bioclimatic distribution of crops has seldom been modeled, probably because social and cultural factors play an important role on crop suitability. Nonetheless, rainfall and temperature still represent a major influence on crop distribution pattern, particularly in rainfed crop systems under traditional agrotechnology. Such is the case of Mexican maize races and consequently, climate change impacts can be expected. Our findings generally show significant reductions of potential distribution areas by 2030 and 2050 in most cases. However, future projections of each race show contrasting responses to climatic scenarios. Several evaluated races show new potential distribution areas in the future, suggesting that proper management may favor diversity conservation. Modeled distributions of Tripsacum species and Teocintes indicate more severe impacts compared to maize races. Our projections lead to in situ and ex situ conservation recommended actions to guarantee the preservation of the genetic diversity of Mexican maize.
    Print ISSN: 1354-1013
    Electronic ISSN: 1365-2486
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Geography
    Published by Wiley
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  • 4
    Publication Date: 2011-03-26
    Description: The reduction of tungsten hexachloride with iron powder or cobalt powder resulted in the formation of M W 2 Cl 10 ( M = Fe and Co) in fused silica tubes at 250 °C and 225 °C, respectively. Crystal structures of the new compounds were refined isotypically from X-ray powder diffraction patterns [ C 2/ c , Z = 4, a = 6.1226(1) Å, b = 16.7943(1) Å, c = 12.3737(1) Å, and β = 108.99(1)° for FeW 2 Cl 10 , and a = 6.111(1) Å, b = 16.696(1) Å, c = 12.384(1) Å, and β = 108.97(1)° for CoW 2 Cl 10 ]. The structures of Fe 1/5 W 2/5 Cl 2 and Co 1/5 W 2/5 Cl 2 can be considered as a cation-deficient CdI 2 -type structure, in which bioctahedral [W 2 Cl 10 ] n – anions with n ≈ 2 introduce significant distortions. The compounds M W 6 Cl 14 ( M = Fe and Co) were prepared following the same procedure at 475 °C. Their crystal structures were refined isotypically [ Pn , Z = 4, a = 12.567(1) Å for FeW 6 Cl 14 , and 12.525(1) Å for CoW 6 Cl 14 ] to the structure of PbMo 6 Cl 14 from X-ray powder diffraction patterns.
    Print ISSN: 0044-2313
    Electronic ISSN: 1521-3749
    Topics: Chemistry and Pharmacology
    Published by Wiley
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  • 5
    Publication Date: 2011-02-26
    Print ISSN: 1045-6740
    Electronic ISSN: 1099-1530
    Topics: Geography , Geosciences
    Published by Wiley
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  • 6
    Publication Date: 2011-02-11
    Description: Herschel Island in the southern Beaufort Sea is a push moraine at the northwestern-most limit of the Laurentide Ice Sheet. Stable water isotope (δ 18 O, δD) and hydrochemical studies were applied to two tabular massive ground ice bodies to unravel their genetic origin. Buried glacier ice or basal regelation ice was encountered beneath an ice-rich diamicton with strong glaciotectonic deformation structures. The massive ice isotopic composition was highly depleted in heavy isotopes (mean δ 18 O: −33‰; mean δD: −258‰), suggesting full-glacial conditions during ice formation. Other massive ice of unknown origin with a very large δ 18 O range (from −39 to −21‰) was found adjacent to large, striated boulders. A clear freezing slope was present with progressive depletion in heavy isotopes towards the centre of the ice body. Fractionation must have taken place during closed-system freezing, possibly of a glacial meltwater pond. Both massive ground ice bodies exhibited a mixed ion composition suggestive of terrestrial waters with a marine influence. Hydrochemical signatures resemble the Herschel Island sediments that are derived from near-shore marine deposits upthrust by the Laurentide ice. A prolonged contact between water feeding the ice bodies and the surrounding sediment is therefore inferred. Copyright © 2011 John Wiley & Sons, Ltd.
    Print ISSN: 1045-6740
    Electronic ISSN: 1099-1530
    Topics: Geography , Geosciences
    Published by Wiley
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  • 7
    Publication Date: 2011-01-22
    Description: Thermophilic microbes in hydrothermal ecosystems have multiple metabolic strategies for taking up carbon and nitrogen, which may result in distinct stable isotopic compositions of C and N in living biomass, as well as other biosignatures that accumulate in the geologic record. Biofilms from “Bison Pool” at Yellowstone National Park display large variations in carbon and nitrogen isotopic values as a function of downstream sampling and illustrate the presence of large shifts in ecological functions as temperature decreases. This is the first study to couple isotopic data with community genomic analysis to predict dominant carbon fixation pathways that create hydrothermal biofilm signatures. The results also suggest nitrogen limitation through the chemotrophic zone and nitrogen fixation in the lower-temperature phototrophic zone.
    Print ISSN: 0148-0227
    Topics: Biology , Geosciences
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 8
    Publication Date: 2011-07-19
    Description: Question: How can we disentangle facilitation and seed dispersal from environmental heterogeneity as mechanisms causing spatial associations of plant species? Location: Semi-arid savanna in the Kimberley Thorn Bushveld, South Africa. Methods: We developed a two-step protocol for the statistical differentiation of association-promoting mechanisms in plants based on the Acacia erioloba–Grewia flava association. Individuals of the savanna shrub G. flava and the tree A. erioloba were mapped on four study plots. Disentangling the mechanism causing the association of G. flava and A. erioloba involved tests of three spatial and one non-spatial null model. The spatial null models include homogeneous and heterogeneous Poisson processes for spatial randomness based on the bivariate spatial point patterns of the four plots. With the non-spatial analysis, we determined the relationship between the canopy diameter of A. erioloba trees and presence or absence of G. flava shrubs in the tree understorey to find whether shrub presence requires a minimum tree canopy diameter. Results: We first showed a significant positive spatial association of the two species. Thereafter, the non-spatial analysis supported an exclusion of environmental heterogeneity as the sole cause of this positive association. We found a minimum tree size under which no G. flava shrubs occurred. Conclusions: Our two-step analysis showed that it is unlikely that heterogeneous environmental conditions caused the spatial association of A. erioloba and G. flava . Instead, this association may have been caused by seed dispersal and/or facilitation (e.g. caused by hydraulic lift and/or nitrogen fixation by the host tree).
    Print ISSN: 1100-9233
    Electronic ISSN: 1654-1103
    Topics: Biology
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  • 9
    Publication Date: 2011-01-20
    Description: Recent, Holocene and Late Weichselian (Sartan) generations of syngenetic ice wedges developed in loess-like and alluvial sediments were investigated along the coast of the Yenisey Bay from Sopochnaya Karga Cape (71°88'N, 82°68'E) to Dikson (73°31'N, 80°34'E). Ages of about 3.4 − 4.6 ka BP were determined for peat layer and wood fragments in ice-rich deposits surrounding ice wedges near Dikson. The isotopic composition of these wedges reflects relatively cold winter temperatures in the Holocene. The lightest isotope composition characterises older ice wedges near Dikson and Sopochnaya Karga Cape. A warming trend between ice wedges of different generations was indicated by a distinct increase in O (4 − 5 ‰) and H (35 − 40‰) stable isotopes. Palaeotemperature reconstruction based on the data shows that winter temperatures during the formation of older generation ice wedges were lower than Holocene winter temperatures, indicating that they developed in the Late Weichselian (MIS2). The presence of syngenetic ice wedges strongly suggests that the coast of western Taymyr was not ice-covered at this time. Copyright © 2011 John Wiley & Sons, Ltd.
    Print ISSN: 1045-6740
    Electronic ISSN: 1099-1530
    Topics: Geography , Geosciences
    Published by Wiley
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  • 10
    Publication Date: 2011-04-29
    Description: The terrestrial carbon cycle is influenced by environmental variability at scales ranging from diurnal to inter-annual. Here we present five-years of growing season (day 131-275) observations of the carbon isotope ratio of ecosystem respiration (δ 13 C R ) from a semi-arid woodland. This ecosystem has a large necromass component resulting from 97% Pinus edulis mortality in 2002, is dominated by drought-tolerant Juniperus monosperma trees, and experiences large variability in the timing and intensity of seasonal and synoptic water availability. Mean growing season δ 13 C R was remarkably invariant (-23.57±0.4‰), with the exception of particularly enriched δ 13 C R in 2006 following a winter with anomalously low snowfall. δ 13 C R was strongly coupled to climate during pre-monsoon periods (∼May-June), including fast (≤two days) responses to changes in crown-level stomatal conductance ( G c ) and vapor pressure deficit ( vpd ) following rain pulses. In contrast, δ 13 C R was relatively de-coupled from G c and environmental drivers during monsoon and post-monsoon periods (July-August and September, respectively), exhibiting only infrequent couplings of δ 13 C R to vpd and soil water content ( SWC ) with longer lags (∼eight days) and variable response slopes (both positive and negative). Notably, δ 13 C R exhibited consistent dynamics after rainfall events, with depleted δ 13 C R occurring within one hour, progressive hourly δ 13 C R enrichment over the remainder of the night, and net δ 13 C R depletions over the multiple nights post-event in monsoon and post-monsoon periods. Overall this ecosystem demonstrated strong dependence of δ 13 C R on precipitation, with an apparent dominance by the autotrophic δ 13 C signal in pre-monsoon periods when deep soil moisture is abundant and surface soil moisture is low, and weaker coupling during monsoonal periods consistent with increasing heterotrophic dominance when deep soil moisture has declined and surface moisture is variable.
    Print ISSN: 1354-1013
    Electronic ISSN: 1365-2486
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Geography
    Published by Wiley
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