Wendy B. Foden  Bruce E. Young  H. Resit Akakaya  Raquel A. Garcia  Ary A. Hoffmann  Bruce A. Stein  Chris D. Thomas  Christopher J. Wheatley  David Bickford  Jamie A. Carr  David G. Hole  Tara G. Martin  Michela Pacifici  James W. Pearce‐Higgins  Philip J. Platts  Piero Visconti  James E. M. Watson  Brian Huntley 《Wiley Interdisciplinary Reviews: Climate Change》2019,10(1)

Assessing species' vulnerability to climate change is a prerequisite for developing effective strategies to conserve them. The last three decades have seen exponential growth in the number of studies evaluating how, how much, why, when, and where species will be impacted by climate change. We provide an overview of the rapidly developing field of climate change vulnerability assessment (CCVA) and describe key concepts, terms, steps and considerations. We stress the importance of identifying the full range of pressures, impacts and their associated mechanisms that species face and using this as a basis for selecting the appropriate assessment approaches for quantifying vulnerability. We outline four CCVA assessment approaches, namely trait‐based, correlative, mechanistic and combined approaches and discuss their use. Since any assessment can deliver unreliable or even misleading results when incorrect data and parameters are applied, we discuss finding, selecting, and applying input data and provide examples of open‐access resources. Because rare, small‐range, and declining‐range species are often of particular conservation concern while also posing significant challenges for CCVA, we describe alternative ways to assess them. We also describe how CCVAs can be used to inform IUCN Red List assessments of extinction risk. Finally, we suggest future directions in this field and propose areas where research efforts may be particularly valuable. This article is categorized under:

• Climate, Ecology, and Conservation > Extinction Risk

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Mohammed M. Rahman  Sate Ahmad  Ayesha S. Mahmud  Md. Hassan‐uz‐Zaman  Mahin A. Nahian  Ali Ahmed  Quamrun Nahar  Peter K. Streatfield 《Wiley Interdisciplinary Reviews: Climate Change》2019,10(5)

Climate change affects almost all aspects of human life, including health. This is particularly true in densely populated and low lying deltas such as Bangladesh. However, the climate‐health nexus is a relatively poorly explored domain of research, which is a cause for concern given the country's intrinsic vulnerability to climatic impacts. The impact of climate change on human health and well‐being can be manifested through different pathways and can be categorized as being direct or indirect, mediated through complex biophysical and social dynamics. The direct effects of climate change that have been observed in Bangladesh include morbidity and mortality due to heat stress, cyclones, floods, droughts and other weather extremes at different spatio‐temporal scales. The indirect effects adopt more complex routes which includes, threatening food and water security due to salinity intrusion, and spread of infectious diseases due to changes in vector and pathogen ecology. Social dynamics in Bangladesh, such as those related to gender roles, poverty and power relations, also influence how the effects of climate change are experienced by different segments of the society. The Government of Bangladesh has a number of measures already in place, efforts that have been complemented by local interventions. Evidence to take robust health policy decisions related to climate change is limited and scattered, while there is a lack of multidisciplinary research efforts. Considering these limitations, generating and summarizing scientific evidence is vital for informing a resilient health system against future public health concerns in climate vulnerable countries such as Bangladesh and in other low‐income regions. This article is categorized under:

• Assessing Impacts of Climate Change > Evaluating Future Impacts of Climate Change

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Stephen Woroniecki  Ruth Krüger  Anna‐Lena Rau  Maren Stefanie Preuss  Nora Baumgartner  Sanne Raggers  Laura Niessen  Lars Hollnder  Felix Beyers  Julius Rathgens  Kai Christian Wagner  Lisa Habigt  Torsten Krause  Christine Wamsler  Henrik von Wehrden  David Abson 《Wiley Interdisciplinary Reviews: Climate Change》2019,10(6)

Power mechanisms and structures shape climate change adaptation outcomes, the measures adopted, and who is identified as requiring adaptation support. But to what extent does research recognize such power‐adaptation linkages? Based on a systematic literature review, we enquire if and how the framing of power matters for adaptation research and what the implications may be for practice. Our enquiry is predicated on the relationship between the researcher and the research focus being itself a relationship of power. Since power is complex and a single definition is not desirable, different actor‐orientated frames of power were used for the data analysis. The results show that authors are more likely to work with issues of power to (i.e., agency), power over, and empowerment, rather than resistance or disempowerment. Demonstrating the effect of such frames, these proportions change according to whether the research focuses on equity, effectiveness, or participation. For instance, power to is strongly associated with effectiveness, while disempowerment is associated more with equity. Together with other identified patterns, our review shows that researchers frame power in adaptation in ways that constitute biases and blind spots. Attention to particular frames of power can limit attention to important dynamics within adaptation processes. Both the content and context to which the identified frames are applied suggest structural trends in adaptation research that require increased attention. Since researchers' frames of power influence both research outcomes and broader adaptation‐power relations, the results indicate that reflexivity is needed to improve both adaptation research and practice. This article is categorized under:

• Vulnerability and Adaptation to Climate Change > Institutions for Adaptation

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Mayuko Shimizu  Naomi Sano  Tadamasa Ueki  Tetsuya Komatsu  Ken‐ichi Yasue  Masakazu Niwa 《Island Arc》2019,28(2)

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Hafiz U. Rehman  Tahseenullah Khan  Hao‐Yang Lee  Sun‐Lin Chung  Mamoru Murata  M. Qasim Jan 《Island Arc》2019,28(6)

We report Permian (ca. 272 Ma ±5.4 Ma) felsic dykes that intrude into the Neoproterozoic (ca. 750 Ma) magmatic suite of the Nagar Parkar Igneous Complex (NPIC), the western extension of the Malani Igneous Suite (MIS). The NPIC consists of Neoproterozoic basement amphibolites and granites (riebeckite–aegirine gray granites and the biotite–hornblende pink granites), all of which are intruded by several generations of mafic and felsic dykes. Granitic magmatism occurred in the Late Neoproterozoic (ca. 750 Ma) due to the subduction‐, followed by the rift‐related tectonic regime during the breakup of the Rodinia supercontinent. U–Th–Pb zircon and monazite CHIME age data of 700–800 Ma from the earlier generation porphyritic felsic dykes suggest the dyke intrusion was coeval or soon after the emplacement of the host granites. Our findings of Permian age orthophyric felsic dykes provide new insights for the prevalence of active tectonics in the MIS during late Paleozoic. Textural features and geochemistry also make the orthophyric dykes distinct from the early‐formed porphyritic dykes and the host granites. Our newly obtained age data combined with geochemistry, suggest the existence of magmatism along the western margin of India (peri‐Gondwana margin) during Permian. Like elsewhere in the region, the Permian magmatism in the NPIC could be associated with the rifting of the Cimmerian micro‐continents from the Gondwana.  相似文献   

    

P. Kessouri  A. Furman  J.A. Huisman  T. Martin  A. Mellage  D. Ntarlagiannis  M. Bücker  S. Ehosioke  P. Fernandez  A. Flores‐Orozco  A. Kemna  F. Nguyen  T. Pilawski  S. Saneiyan  M. Schmutz  N. Schwartz  M. Weigand  Y. Wu  C. Zhang  E. Placencia‐Gomez 《Near Surface Geophysics》2019,17(6):595-621

This paper provides an update on the fast‐evolving field of the induced polarization method applied to biogeophysics. It emphasizes recent advances in the understanding of the induced polarization signals stemming from biological materials and their activity, points out new developments and applications, and identifies existing knowledge gaps. The focus of this review is on the application of induced polarization to study living organisms: soil microorganisms and plants (both roots and stems). We first discuss observed links between the induced polarization signal and microbial cell structure, activity and biofilm formation. We provide an up‐to‐date conceptual model of the electrical behaviour of the microbial cells and biofilms under the influence of an external electrical field. We also review the latest biogeophysical studies, including work on hydrocarbon biodegradation, contaminant sequestration, soil strengthening and peatland characterization. We then elaborate on the induced polarization signature of the plant‐root zone, relying on a conceptual model for the generation of biogeophysical signals from a plant‐root cell. First laboratory experiments show that single roots and root system are highly polarizable. They also present encouraging results for imaging root systems embedded in a medium, and gaining information on the mass density distribution, the structure or the physiological characteristics of root systems. In addition, we highlight the application of induced polarization to characterize wood and tree structures through tomography of the stem. Finally, we discuss up‐ and down‐scaling between laboratory and field studies, as well as joint interpretation of induced polarization and other environmental data. We emphasize the need for intermediate‐scale studies and the benefits of using induced polarization as a time‐lapse monitoring method. We conclude with the promising integration of induced polarization in interdisciplinary mechanistic models to better understand and quantify subsurface biogeochemical processes.  相似文献   

    

Hajar Taheri‐Soudejani  Manouchehr Heidarpour  Mohammad Shayannejad  Hossein Shariatmadari  Hossein Kazemian  Majid Afyuni 《洁净——土壤、空气、水》2019,47(8)

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Zoya Zafar  Javaid Akhtar  Muhammad Amjad  Muhammad Anwar‐ul‐Haq  Zulfiqar Ahmed Saqib 《洁净——土壤、空气、水》2019,47(7)

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Manuel D. Menzel  Carlos J. Garrido  Vicente Lpez Snchez‐Vizcaíno  Kroly Hidas  Claudio Marchesi 《Journal of Metamorphic Geology》2019,37(5):681-715

At sub‐arc depths, the release of carbon from subducting slab lithologies is mostly controlled by fluid released by devolatilization reactions such as dehydration of antigorite (Atg‐) serpentinite to prograde peridotite. Here we investigate carbonate–silicate rocks hosted in Atg‐serpentinite and prograde chlorite (Chl‐) harzburgite in the Milagrosa and Almirez ultramafic massifs of the palaeo‐subducted Nevado‐Filábride Complex (NFC, Betic Cordillera, S. Spain). These massifs provide a unique opportunity to study the stability of carbonate during subduction metamorphism at P–T conditions before and after the dehydration of Atg‐serpentinite in a warm subduction setting. In the Milagrosa massif, carbonate–silicate rocks occur as lenses of Ti‐clinohumite–diopside–calcite marbles, diopside–dolomite marbles and antigorite–diopside–dolomite rocks hosted in clinopyroxene‐bearing Atg‐serpentinite. In Almirez, carbonate–silicate rocks are hosted in Chl‐harzburgite and show a high‐grade assemblage composed of olivine, Ti‐clinohumite, diopside, chlorite, dolomite, calcite, Cr‐bearing magnetite, pentlandite and rare aragonite inclusions. These NFC carbonate–silicate rocks have variable CaO and CO₂ contents at nearly constant Mg/Si ratio and high Ni and Cr contents, indicating that their protoliths were variable mixtures of serpentine and Ca‐carbonate (i.e., ophicarbonates). Thermodynamic modelling shows that the carbonate–silicate rocks attained peak metamorphic conditions similar to those of their host serpentinite (Milagrosa massif; 550–600°C and 1.0–1.4 GPa) and Chl‐harzburgite (Almirez massif; 1.7–1.9 GPa and 680°C). Microstructures, mineral chemistry and phase relations indicate that the hybrid carbonate–silicate bulk rock compositions formed before prograde metamorphism, likely during seawater hydrothermal alteration, and subsequently underwent subduction metamorphism. In the CaO–MgO–SiO₂ ternary, these processes resulted in a compositional variability of NFC serpentinite‐hosted carbonate–silicate rocks along the serpentine‐calcite mixing trend, similar to that observed in serpentinite‐hosted carbonate‐rocks in other palaeo‐subducted metamorphic terranes. Thermodynamic modelling using classical models of binary H₂O–CO₂ fluids shows that the compositional variability along this binary determines the temperature of the main devolatilization reactions, the fluid composition and the mineral assemblages of reaction products during prograde subduction metamorphism. Thermodynamic modelling considering electrolytic fluids reveals that H₂O and molecular CO₂ are the main fluid species and charged carbon‐bearing species occur only in minor amounts in equilibrium with carbonate–silicate rocks in warm subduction settings. Consequently, accounting for electrolytic fluids at these conditions slightly increases the solubility of carbon in the fluids compared with predictions by classical binary H₂O–CO₂ fluids, but does not affect the topology of phase relations in serpentinite‐hosted carbonate‐rocks. Phase relations, mineral composition and assemblages of Milagrosa and Almirez (meta)‐serpentinite‐hosted carbonate–silicate rocks are consistent with local equilibrium between an infiltrating fluid and the bulk rock composition and indicate a limited role of infiltration‐driven decarbonation. Our study shows natural evidence for the preservation of carbonates in serpentinite‐hosted carbonate–silicate rocks beyond the Atg‐serpentinite breakdown at sub‐arc depths, demonstrating that carbon can be recycled into the deep mantle.  相似文献   

    

Arturo Carranza‐Edwards  Juan Jos Kasper‐Zubillaga  Raymundo G. Martínez‐Serrano  Mayumy Cabrera‐Ramírez  Leticia Rosales Hoz  Miguel Angel Alatorre Mendieta  Antonio Z. Mrquez‐García  Rufino Lozano‐Santa Cruz 《Geological Journal》2019,54(1):552-563

Different parent rocks, climate, and relief control the provenance of beach sands on the coast of Mexico. This is the first paper to address the provenance problem of beach sands in south‐eastern Mexico considering a homogeneous climate and relative similarity in parental rocks but different relief. Two coastal areas are confined in this study: (a) the Western Gulf of Tehuantepec (WGT) and (b) the Eastern Gulf of Tehuantepec (EGT). The WGT beach sands are probably controlled by the denudation of orthogneisses, Eocene–Miocene basaltic–andesites–dacites–rhyolites from the Volcanic Belt of the Sierra Madre del Sur (VBSMS), and granites to diorites from the Coastal Plutonic Belt (CPB). The rocks exposed in the EGT are represented by orthogneisses and tonalite, granodiorite, and gabbro suites from the Palaeozoic–Mesozoic Chiapas Coastal Plutonic Belt (CHCPB). Quaternary andesites and dacites from the Tacaná Volcano are located in the eastern coastal area. The Chemical Index of Alteration (CIA) and Plagioclase Index of Alteration (PIA) values indicate that the less weathered beach sands are in the WGT compared to the EGT coastal area. Plagioclase transport is preserved in a narrow coastal plain that contributes to a lower a weathering rate compared to the EGT sands deposited in a wider coastal plain. Geochemical analyses show that the WGT and EGT beach sands are admixtures of felsic, intermediate, metamorphic, and volcanic sources in their sands composition. Relief seems to play a major role in the composition of beach sand in both coastlines, since parental rocks are mostly similar in composition and climate remains homogeneous along the coast.  相似文献