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Книги з теми "Transition marine à continentale"

Автор: Grafiati

Опубліковано: 7 вересня 2024

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1

Valentine, Page C. The shelf-slope transition--canyon and upper slope sedimentary processes on the southern margin of Georges Bank: An examination of sedimentary environments in water depths of 150-600 meters and of how they are determined by the interaction of available sediment, bottom currents, and sea-floor morphology. Washington, D.C: U.S. G.P.O., 1987.

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2

Valentine, Page C. The shelf-slope transition--canyon and upper slope sedimentary processes on the southern margin of Georges Bank: An examination of sedimentary environments in water depths of 150-600 meters and of how they are determined by the interaction of available sediment, bottom currents, and sea-floor morphology. Washington, DC: U.S. Geological Survey, 1987.

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3

Tomoya, Akimichi, ed. Coastal foragers in transition. Osaka: National Museum of Ethnology, 1996.

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4

R, Prothero Donald, Ivany Linda C, and Nesbitt Elizabeth R, eds. From greenhouse to icehouse: The marine Eocene-Oligocene transition. New York: Columbia University Press, 2003.

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5

name, No. From greenhouse to icehouse: The marine Eocene-Oligocene transition. New York: Columbia University Press, 2003.

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6

Lei, Guobin. Geochemical processes controlling transition metal distributions in marine manganese concretions and sediments. Stockholm, Sweden: Dept. of Geology and Geochemistry, Stockholm University, 1995.

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7

A, Wetherall Jerry, Southwest Fisheries Science Center (U.S.). Honolulu Laboratory, University of Hawaii (Honolulu). Joint Institute for Marine and Atmospheric Research, and United States. National Marine Fisheries Service, eds. Biology, oceanography, and fisheries of the North Pacific transition zone and subarctic frontal zone: Papers from the North Pacific Transition Zone Workshop, Honolulu, Hawaii, 9-11 May 1988. [Washington, D.C.]: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Marine Fisheries Service, 1991.

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8

S, Savino Carl. The military-to-civilian transition guide: A career transition guide for Army, Navy, Air Force, Marine Corps & Coast Guard personnel. 2nd ed. Fairfax Station, VA: Competitive Edge Services, 2011.

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9

Scharek, Renate. Die Entwicklung des Phytoplanktons im östlichen Weddellmeer (Antarktis) beim Übergang vom Spätwinter zum Frühjahr =: Development of phytoplankton during the late-winter/spring transition in the eastern Weddell Sea (Antarctica). Bremerhaven: Alfred-Wegener-Institut für Polar- und Meeresforschung, 1991.

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10

Reims, Université de, ed. Recherches en aménagement du territoire, en glaciologie fluviale, marine et continentale, sur le quaternaire (glaciaire et périglaciare) en géomorphologie et en tectonique. Lille: A.N.R.T, Université de Lille III, 1985.

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11

Scott, McIndoe J., ed. Transition metal carbonyl cluster chemistry. Amsterdam, The Netherlands: Gordon and Breach Science Publishers, 2000.

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12

Hasan, Mohammad R. Transition from low-value fish to compound feeds in marine cage farming in Asia. Rome: Food and Agriculture Organization of the United Nations, 2012.

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13

Savino, Carl S. From navy blue to corporate gray: A career transition guide for Navy, Marine Corps, and Coast Guard personnel. 2nd ed. Manassas Park, VA: Impact Publications, 1997.

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14

L, Krannich Ronald, ed. From navy blue to corporate gray: A career transition guide for Navy, Marine Corps, and Coast Guard personnel. 2nd ed. Manassas Park, VA: Impact Publications, 1997.

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15

L, Krannich Ronald, ed. From navy blue to corporate gray: A career transition guide for Navy, Marine Corps, and Coast Guard personnel. Manassas Park, VA: Impact Publications, 1995.

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16

Expert Consultation on Catalysing the Transition away from Overcapacity in Marine Capture Fisheries (2002 Rome, Italy). Report of the Expert Consultation on Catalysing the Transition away from Overcapacity in Marine Capture Fisheries: Rome, 15-18, October 2002. Rome: Food and Agriculture Organization of the United Nations, 2002.

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17

Nigro, Giampiero, ed. Reti marittime come fattori dell’integrazione europea / Maritime Networks as a Factor in European Integration. Florence: Firenze University Press, 2019. http://dx.doi.org/10.36253/978-88-6453-856-3.

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Анотація:

Il tema, di grande respiro, prende come punto di partenza il concetto braudeliano di Mediterraneo. La sua visione di un mare chiuso come una opportunità geografica per una integrazione economica fra popolazioni diverse per religioni, linguaggi ed entità etniche e politiche continua a funzionare come modello per studi applicati ad un ampio raggio di contesti. L’obiettivo che si è posta la 50ª Settimana di studi è stato quello di andare oltre lo studio dei singoli sistemi visti in modo isolato per combinare diverse analisi di mari aperti e chiusi o aree costiere, allo scopo di comprendere il ruolo di integrazione giocato in Europa dalle connessioni marittime. Poiché nelle civiltà preindustriali il trasporto per via d’acqua era più facile di quello via terra, è sembrato giunto il momento di richiamare l’attenzione sul modo in cui queste reti di relazione operavano a livello europeo e con i partner commerciali asiatici e nordafricani. Il volume prende le mosse dalle grandi tradizioni di ricerca su base regionale o tematica, che però sono state raramente integrate su una più ampia scala continentale. Immanuel Wallerstein ha elaborato il concetto braudeliano concettualizzandone le dimensioni interculturali e transnazionali e il ruolo nel sistema di divisione del lavoro. Egli lo chiamò un “sistema mondo”, non perché coinvolgesse il mondo intero, ma perché è più vasto di qualunque unità politica giuridicamente definita. E si tratta di una “economia mondo” perché il legame di base tra le varie parti del sistema è economico. I vari aspetti e le tradizioni regionali di ricerca sono stati collegati tra loro in un approccio coerente che si posto l'obiettivo di valutare: - Sulla base di quali elementi geografici, nautici, tecnici, economici, giuridici, sociali e culturali siano emerse le varie reti regionali, e come funzionavano, - Il carattere e il ruolo dei porti marittimi come punti nodali delle rotte marine e del loro hinterland, attraverso fiumi, canali e strade, - I legami commerciali e personali tra mercanti e armatori in vari porti, - In quale modo le reti regionali si collegavano tra di loro e come, nel corso del tempo, finirono per integrarsi in unità più ampie, - In quale modo le reti private, inizialmente costituite da organizzazioni di mercanti e navigatori, finirono per trattare con le autorità locali e, una volta cresciute, con gli stati e gli imperi, per proteggere i propri interessi

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18

Thomas, Rhidian. Marine Insurance: The Law in Transition. Informa Law, 2020.

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19

Thomas, Rhidian. Marine Insurance: The Law in Transition. Informa Law, 2020.

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20

Marine Insurance: The Law in Transition. Taylor & Francis Group, 2006.

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21

Marine Insurance: The Law in Transition. Informa Law, 2020.

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22

Dubinsky, Zvy, and Noga Stambler. Coral Reefs: An Ecosystem in Transition. Springer London, Limited, 2010.

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23

Coral Reefs: An Ecosystem in Transition. Springer, 2010.

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24

Dubinsky, Zvy, and Noga Stambler. Coral Reefs: An Ecosystem in Transition. Springer, 2014.

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25

Dubinsky, Zvy, and Noga Stambler. Coral Reefs: An Ecosystem in Transition. Springer, 2011.

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26

McIndoe, J. Scott, and Paul J. Dyson. Transition Metal Carbonyl Cluster Chemistry. Taylor & Francis Group, 2018.

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27

McIndoe, J. Scott, and Paul J. Dyson. Transition Metal Carbonyl Cluster Chemistry. Taylor & Francis Group, 2018.

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28

McIndoe, J. Scott, and Paul J. Dyson. Transition Metal Carbonyl Cluster Chemistry. Taylor & Francis Group, 2019.

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29

McIndoe, J. Scott, and Paul J. Dyson. Transition Metal Carbonyl Cluster Chemistry. Taylor & Francis Group, 2018.

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30

McIndoe, J. Scott, and Paul J. Dyson. Transition Metal Carbonyl Cluster Chemistry. Taylor & Francis Group, 2018.

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31

Navy RDT&E planning in an age of transition: A survey guide to contemporary literature. Washington: Navy Laboratory/Center Coordinating Group and Naval Historical Center, Dept. of the Navy, 1997.

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32

The Ming Maritime Trade Policy In Transition 1368 To 1567. Harrassowitz, 2010.

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33

Halperin, Alan. A marine/nonmarine transition in the Upper Devonian West Falls Group of south-central New York. 1987.

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34

Department of Defense. History of Headquarters Marine Corps Staff Organization from 1798 - Modern Staff, Transition, World War II, Postwar Adjustments, Marine Corps General Staff, Public Law 416, Vietnam Era. Independently Published, 2017.

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35

Ronald L. Krannich Carl S. Savino. From Navy Blue to Corporate Gray; a Career Transition Guide for Navy, Marine Corps and Coast Guard Personnel. Impact Publications, 1997.

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36

From Navy Blue to Corporate Gray: A Career Transition Guide for Navy, Marine Corps, and Coast Guard Personnel. Competitive Edge Services, 2004.

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37

Savino, Carl S. From Navy Blue to Corporate Gray: A Career Transition Guide for Navy, Marine Corps, and Coast Guard Personnel. Impact Publications, 1994.

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38

Diemer, John A. Sedimentology of the fluvial-marine transition in the Upper Devonian/Lower Carboniferous of Kerry Head, County Kerry, Ireland. 1985.

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39

McIndoe, J. Scott, and Paul J. Dyson. Transition Metal Carbonyl Cluster Chemistry (Advanced Chemistry Texts, Volume 2). CRC, 2000.

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40

Marlow, Heather, ed. Evolutionary Development of Marine Larvae. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198786962.003.0002.

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Access to a growing number of marine invertebrates with genetic and genomic tools has broadened our understanding of the diversity of developmental mechanisms, informing our understanding of larval evolution by allowing the identification of shared or divergent programs for the formation of body plan patterning and organ formation. Two such genetic programs are the apical plate patterning network and the hox/parahox trunk and gut patterning network common to larval and adult forms, respectively. While mounting evidence supports an ancient origin at the base of the Bilateria for both adult and larval forms, it is clear that many distinct organs and structures have appeared independently and can be shifted between the larval and adult phase frequently. Future advances in our understanding of larval evolution are likely to emerge from exhaustive studies of marine invertebrate cell types by single-cell sequencing technologies and through the study of the genetic basis of the metamorphic transition.

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41

From Navy Blue to Corporate Gray: A Career Transition Guide for Navy, Marine Corps, and Coast Guard Personnel 3rd Third Edition. Impact, 1998.

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42

Ainsworth, R. Bruce, Boyan K. Vakarelov, and James A. MacEachern. The Classic Tidally Influenced, Marginal-Marine Deposits of the Late Cretaceous Bearpaw to Horseshoe Canyon Formation Transition, Drumheller, Alberta: Volume 2. SEPM Society for Sedimentary Geology, 2022. http://dx.doi.org/10.2110/sepmfg.17-2.

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43

Ainsworth, R. Bruce, Boyan K. Vakarelov, and James A. MacEachern. The Classic Tidally Influenced, Marginal-Marine Deposits of the Late Cretaceous Bearpaw to Horseshoe Canyon Formation Transition, Drumheller, Alberta: Volume 1. SEPM Society for Sedimentary Geology, 2022. http://dx.doi.org/10.2110/sepmfg.17-1.

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Анотація:

The Upper Cretaceous Horseshoe Canyon Formation deposits near Drumheller, Alberta, Canada form world-class exposures of tidally-influenced, marginal marine to shoreline depositional environments. These outcrops have represented a fundamental training ground for generations of Canadian and international geoscientists. The compilation of work in this publication is the product of seven years of study by WAVE Consortium geoscientists. The WAVE Consortium was an industry-funded research collective run by the Australian School of Petroleum & Energy Resources, University of Adelaide between 2008 and 2014. The work integrates interpretations of outcrop observations with core descriptions and wireline log data to generate depositional models. These models were then convolved into 3D reservoir models from which synthetic seismic volumes were generated. This digital resource is provided in three parts: A) A Field and Core Guide: Volume 1, B) A Core and Outcrop Facies and Ichnology Guide: Volume 2, C) Posters - which can be downloaded from the SEPM Supplemental Materials Website.

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44

(US), National Research Council, and National Research Council Staff. Network Centric Naval Forces: A Transition Strategy for Enhancing Operational Capabilities. National Academy Press, 2000.

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45

Carrier, Tyler J., Adam M. Reitzel, and Andreas Heyland, eds. Section 3 Summary—Larval Transport, Settlement, and Metamorphosis. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198786962.003.0015.

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Life cycles for broadcast-spawning marine invertebrates are characterized by a pelagic (larval) and benthic (juvenile and adult) stage, which are differentiated by the process of settlement and metamorphosis. While settlement and recruitment are concepts that primarily deal with the ecological aspects of this transition, they are often accompanied by a drastic morphological and developmental transition. Larval transport, the means of reaching suitable settlement sites, is difficult to study, but insights from genetics, behavior, sensory ecology, and oceanography have provided important insights....

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46

Hodin, Jason, Matthew C. Ferner, Andreas Heyland, and Brian Gaylord, eds. I Feel That! Fluid Dynamics and Sensory Aspects of Larval Settlement across Scales. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198786962.003.0013.

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A commonality among oceanic life cycles is a process known as settlement, where dispersing propagules transition to the sea floor. For many marine invertebrates, this transition is irreversible, and therefore involves a crucial decision-making process through which larvae evaluate their juvenile habitat-to-be. In this chapter, we consider aspects of the external environment that could influence successful settlement. Specifically, we discuss water flow across scales, and how larvae can engage behaviors to influence where ocean currents take them, and enhance the likelihood of their being carried toward suitable settlement locations. Next, we consider what senses larvae utilize to evaluate their external environment and properly time such behavioral modifications, and settlement generally. We hypothesize that larvae integrate these various external cues in a hierarchical fashion, with differing arrangements being employed across ontogeny and among species. We conclude with a brief discussion of the future promises of larval biology, ecology, and evolution.

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47

Fogarty, Michael J., and Jeremy S. Collie. Fishery Ecosystem Dynamics. Oxford University Press, 2020. http://dx.doi.org/10.1093/oso/9780198768937.001.0001.

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This book provides an integrated framework for the quantitative analysis of exploited aquatic ecosystems, tracing the critical linkages between fundamental ecological processes and their implications for sustainable resource management. Examples are drawn from freshwater and marine ecosystems throughout the world. Fishery ecosystems have historically been subject to a broad array of human interventions, ranging from large-scale removal of biomass to deliberate attempts at ecosystem engineering involving species introductions, habitat alteration, and selective reorganization of ecosystem structure. Traditional approaches to fisheries analysis and management focus on extraction of resources viewed in isolation from the broader ecosystem setting. Further, these approaches typically are predicated on assumptions of “well-behaved” dynamical properties characterized by stable equilibrium properties. This book explores a broader range of possibilities concerning human impacts on aquatic ecosystems. It places software tools in the hands of students and professionals in an electronic supplement. Modeling and statistical programs in R and other platforms are provided to assist in the transition from concept to practical application.

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48

Weiss, Harvey. Megadrought, Collapse, and Causality. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199329199.003.0001.

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Recent discoveries of megadroughts, severe periods of drought lasting decades or centuries, during the course of the Holocene have revolutionized our understanding of modern climate history. Through advances in paleoclimatology, researchers have identified these periods of climate change by analyzing high-resolution proxy data derived from lake sediment cores, marine cores, glacial cores, speleothem cores, and tree rings. Evidence that megadroughts occurred with frequency and abruptly over the last 12,000 years, a timespan long assumed to be stable compared to earlier glacial periods, has also altered our understanding of societies’ trajectories. The fact that severe, multi-decadal or century-scale droughts coincided with societal collapses well known to archaeologists has challenged established multi-causal analyses of these events. Megadroughts, impossible to predict and impossible to withstand, may have caused political collapse, regional abandonment, and habitat tracking to still-productive regions. The nine megadrought and societal collapse events presented in this volume extend from the foraging-to-agriculture transition at the dawn of the Holocene in West Asia to the fifteenth-century AD collapse of the Khmer Empire in Angkor (Cambodia). Inevitably, this collection of essays also raises challenges to causal analyses of societal collapse and for future paleoclimatic and archaeological research.

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49

Vuorinen, Ilppo. Post-Glacial Baltic Sea Ecosystems. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.675.

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Post-glacial aquatic ecosystems in Eurasia and North America, such as the Baltic Sea, evolved in the freshwater, brackish, and marine environments that fringed the melting glaciers. Warming of the climate initiated sea level and land rise and subsequent changes in aquatic ecosystems. Seminal ideas on ancient developing ecosystems were based on findings in Swedish large lakes of species that had arrived there from adjacent glacial freshwater or marine environments and established populations which have survived up to the present day. An ecosystem of the first freshwater stage, the Baltic Ice Lake initially consisted of ice-associated biota. Subsequent aquatic environments, the Yoldia Sea, the Ancylus Lake, the Litorina Sea, and the Mya Sea, are all named after mollusc trace fossils. These often convey information on the geologic period in question and indicate some physical and chemical characteristics of their environment. The ecosystems of various Baltic Sea stages are regulated primarily by temperature and freshwater runoff (which affects directly and indirectly both salinity and nutrient concentrations). Key ecological environmental factors, such as temperature, salinity, and nutrient levels, not only change seasonally but are also subject to long-term changes (due to astronomical factors) and shorter disturbances, for example, a warm period that essentially formed the Yoldia Sea, and more recently the “Little Ice Age” (which terminated the Viking settlement in Iceland).There is no direct way to study the post-Holocene Baltic Sea stages, but findings in geological samples of ecological keystone species (which may form a physical environment for other species to dwell in and/or largely determine the function of an ecosystem) can indicate ancient large-scale ecosystem features and changes. Such changes have included, for example, development of an initially turbid glacial meltwater to clearer water with increasing primary production (enhanced also by warmer temperatures), eventually leading to self-shading and other consequences of anthropogenic eutrophication (nutrient-rich conditions). Furthermore, the development in the last century from oligotrophic (nutrient-poor) to eutrophic conditions also included shifts between the grazing chain (which include large predators, e.g., piscivorous fish, mammals, and birds at the top of the food chain) and the microbial loop (filtering top predators such as jellyfish). Another large-scale change has been a succession from low (freshwater glacier lake) biodiversity to increased (brackish and marine) biodiversity. The present-day Baltic Sea ecosystem is a direct descendant of the more marine Litorina Sea, which marks the beginning of the transition from a primeval ecosystem to one regulated by humans. The recent Baltic Sea is characterized by high concentrations of pollutants and nutrients, a shift from perennial to annual macrophytes (and more rapid nutrient cycling), and an increasing rate of invasion by non-native species. Thus, an increasing pace of anthropogenic ecological change has been a prominent trend in the Baltic Sea ecosystem since the Ancylus Lake.Future development is in the first place dependent on regional factors, such as salinity, which is regulated by sea and land level changes and the climate, and runoff, which controls both salinity and the leaching of nutrients to the sea. However, uncertainties abound, for example the future development of the Gulf Stream and its associated westerly winds, which support the sub-boreal ecosystems, both terrestrial and aquatic, in the Baltic Sea area. Thus, extensive sophisticated, cross-disciplinary modeling is needed to foresee whether the Baltic Sea will develop toward a freshwater or marine ecosystem, set in a sub-boreal, boreal, or arctic climate.

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