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Geochemistry of Organic Matter in the Ocean
My work Geochemistry oj organic matter in the ocean first appeared in Russian in 1978. Since then much progress has been made in the exploration of various forms of organic matter in the ocean: dissolved, colloidal, organic matter sus pended in particles and that contained in bottom sediments and in interstitial waters. The appropriate evidence is found in hundreds of articles and several re view works, such as Andersen (1977), Biogeochimie de [a matiere organique a ['interjace eau-sedimentmarine (1980), Duursma and Dawson (1981). A great amount of new information has been obtained in the Soviet Union's scientific institutions on the composition and distribution in natural waters and bottom ...
The Oceans in the Nuclear Age
The advent of the nuclear age in 1945 fundamentally altered the course of human events. The oceans are not the focus of the nuclear age, but the affairs of the oceans are deeply woven into the history of that age. Knowledge of what the nuclear age has meant for the oceans, however, is highly fragmented and there exists a surprising gap in research on the impact of the nuclear age on the oceans and on ocean law and policy. Ranging from dumped wastes to transportation to security, this study frames the complex multidimensional set of relationships between the oceans and the nuclear age and illuminates patterns of impact and response in ocean law. This timely expanded edition includes a new chapter by Lt. Todd Hutchins, USN, on “Nuclear Risks in Coastal Areas: Legal and Regulatory Responses.” It provides a full discussion of the 2011 coastal Fukushima Nuclear Power Plant disaster, together with analysis more generally of the challenges to the environment and to the legal order globally that are posed by coastal siting of nuclear power plants.
Carbon Cycle in the Russian Arctic Seas
This study analyzes carbon-cycle conditions controlling the state of the Arctic ecosystem and their seasonal variations. Territory covered includes the Barents, White, Kara, Laptev, East-Siberian and Chukchi Seas, considering inter-correlations between sources of organic carbon, their fluxes, recycling and burial in bottom sediments. All biological communities (phythoplankton, macrophythobenthos, microphythobentos, bacterioplankton, zooplankton and zoobenthos) are taken into account regarding their participation in the carbon cycle.
Influence of Climate Change on the Changing Arctic and Sub-Arctic Conditions
The current warming trends in the Arctic may shove the Arctic system into a seasonally ice-free state not seen for more than one million years. The melting is accelerating, and researchers were unable to identify natural processes that might slow the deicing of the Arctic. Such substantial additional melting of Arctic and Antarctic glaciers and ice sheets would raise the sea level worldwide, flooding the coastal areas where many of the world's population lives. Studies, led by scientists at the National Center for Atmospheric Research (NCAR) and the University of Arizona, show that greenhouse gas increases over the next century could warm the Arctic by 3-5°C in summertime. Thus, Arctic summers by 2100 may be as warm as they were nearly 130,000 years ago, when sea levels eventually rose up to 6 m higher than today.
Biogeochemistry of Major World Rivers
This extract of the SCOPE/UNEP project ``Transport of Carbon and Minerals in Major World Rivers, Lakes, and Estuaries'' provides a comprehensive overview of the biogeochemistry of major rivers and their role in the biogeochemical cycles of its life-supporting animals for the first time. Rivers are viewed by continent or under certain scientific aspects. Concrete data on the chemistry and fluxes of major world rivers are given in addition to a more theoretical approach to the riverine system.
