03421nam 2200757 450 991078748860332120230612051719.01-4426-5615-81-4426-2357-810.3138/9781442623576(CKB)3710000000329562(EBL)3296728(SSID)ssj0001420425(PQKBManifestationID)12626813(PQKBTitleCode)TC0001420425(PQKBWorkID)11403927(PQKB)11254286(MiAaPQ)EBC4670084(CEL)449194(OCoLC)903421439(CaBNVSL)slc00211021(DE-B1597)465670(OCoLC)944178823(DE-B1597)9781442623576(Au-PeEL)EBL4670084(CaPaEBR)ebr11256598(OCoLC)958580520(MdBmJHUP)musev2_107018(EXLCZ)99371000000032956220160921h19951995 uy 0engur|n|---|||||txtccrCritical issues in editing exploration texts papers given at the twenty-eighth annual Conference on Editorial Problems, University of Toronto, 6-7 November 1992 /edited by Germaine WarkentinToronto, [Ontario] ;Buffalo, [New York] ;London, [England] :University of Toronto Press,1995.©19951 online resource (167 p.)Heritage0-8020-0694-9 1-4426-5503-8 Includes bibliographical references.Frontmatter -- Contents -- Notes on Contributors -- Introduction -- Tractable Texts: Modern Editing and the Columbian Writings -- Editing Italian Sources for the History of Exploration -- The Editing of Richard Hakluyt's "Discourse of Western Planting" -- The Metamorphosis of Travellers into Authors: The Case of Paul Kane -- The Great Publication Societies -- A Double Tradition: Editing Book Twelve of the Florentine Codex -- Members of the Conference -- Backmatter The papers in this collection deal with a cultural problem central to the study of the history of exploration: the editing and transmission of the texts in which explorers relate their experiences. The papers chart the transformation of the study of exploration writing from the genres of national epic and scientific reportage to the genre of cultural analysis. As well, they reflect on ongoing changes in our ideas about editorial procedures, literary genres, and cultural appropriation.Discoveries in geographySourcesEditingCongressesTravelers' writings, EnglishCongressesTravel writingHistoryCongressesCriticism, TextualCongressesHistory.Conference papers and proceedings.Electronic books. Discoveries in geographySourcesEditingTravelers' writings, EnglishTravel writingHistoryCriticism, Textual808.027Warkentin GermaineConference on Editorial Problems.MiAaPQMiAaPQMiAaPQBOOK9910787488603321Critical issues in editing exploration texts3682122UNINA03989nam 2200577z- 450 991055739590332120211118(CKB)5400000000041938(oapen)https://directory.doabooks.org/handle/20.500.12854/73700(oapen)doab73700(EXLCZ)99540000000004193820202111d2020 |y 0engurmn|---annantxtrdacontentcrdamediacrrdacarrierInteractive Feedbacks between Soil Fauna and Soil ProcessesFrontiers Media SA20201 online resource (120 p.)2-88963-548-1 Soil fauna plays a significant role at all trophic levels of the soil food web and regulates processes that are crucial for soil functioning, such as nutrient cycling, immobilization and/or degradation of toxic compounds, formation of soil structure, greenhouse gas emissions and C turnover. Although soil fauna is not thought to contribute significantly to soil respiration during litter or soil organic matter (SOM) decomposition, the diversity of soil fauna has been found to strongly influence SOM distribution and dynamics. Yet, the functional contribution of soil fauna to many soil processes is not well understood due to methodological limitations and the high complexity of interactions at various spatiotemporal scales. In general, soil fauna has received far less scientific attention than bacteria and fungi (and lately archaea) in soil studies and has been regularly ignored in global biogeochemical models, with maybe exceptions for some earthworms. However, recent studies are raising the awareness of the influence of soil fauna on ecosystems dynamics. For instance, earthworms have been found to be major players in N2O emissions from soils. They exert a strong influence on C stabilization, and they promote the degradation of polycyclic aromatic hydrocarbons (PAHs). Less studied, ants and termites have been found to increase crop productivity in drylands, and different lifeforms of Collembola have been shown to impact microorganisms in various ways over time, thereby potentially affecting C and N cycles within farming systems. The influence of soil fauna indeed manifests over a broad ranges of spatiotemporal scales. For example, some effect such as aggregate formation may cumulate over time and finally contribute to the formation of whole soil profiles, which serve as a framework for other soil processes such as water movement, decomposition, etc. Meanwhile, soil biodiversity is impacted by an increasing human pressure through deforestation, agriculture intensification, habitat fragmentation or climate change (increasing temperatures, extreme weather events), which leads to soil biodiversity loss, in particular of soil fauna, with associated consequences on soil functioning and resilience.Environmental science, engineering and technologybicsscScience: general issuesbicsscbiogeochemical cyclesC sequestrationearthwormsgreenhouse gasmacroarthropodsmicroarthropodsnematodesprotistsresiliencesoil alterationssoil functionssoil stabilitysoil structureEnvironmental science, engineering and technologyScience: general issuesLuz Cayuela Mariaedt1295610Clause JuliaedtFrouz JanedtBaveye Philippe CedtLuz Cayuela MariaothClause JuliaothFrouz JanothBaveye Philippe CothBOOK9910557395903321Interactive Feedbacks between Soil Fauna and Soil Processes3023672UNINA