Lake Pavin
History, geology, biogeochemistry, and sedimentology of a deep meromictic maar lake
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The aim of this chapter is to provide a critical assessment of the approaches and production of tools within the PIREN-Seine programme over the past 30 years, as well as their use for river basin management an...
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The Seine River basin in France (76,238 km2, 17 million (M) people) has been continuously studied since 1989 by the PIREN-Seine, a multidisciplinary programme of about 100 scientists from 20 research units (hydro...
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Sedimentary archives provide long-term records of particulate-bound pollutants (e.g. trace metal elements, PAHs). We present the results obtained on a set of selected cores from alluvial deposits within the Se...
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The Seine River basin (65,000 km2) is extremely rich in cartographic documents generated over the past two centuries: general maps describing the territory, fiscal land registries, navigation charts (e.g. bathyme...
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Mountain areas provide disproportionally high runoff in many parts of the world, but their importance for water resources and food production has not been clarified from the viewpoint of the lowland areas down...
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In 1852 a new machine to provide greater volumes of Seine River water to Versailles was decided. The new Marly Machine was operated by the Versailles Water Service (VWS), a 150-year old state-owned institution...
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Lake Pavin is located in the Auvergne Mountains, central France, at 1300 m a.s.l. This small lake (0.44 km2), partially fills an explosive volcanic crater in the Cezallier, a young volcanic area south of the Mont...
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The legends, miracles and fantastic stories of Pavin and around are numerous, although the key ones are so far not attributed to it. The current legend, that of the Sunken City, common to many lakes, was created ...
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“Pavin Stories”, told to the lake’s visitors seeking its wild beauty, were reported throughout the nineteenth century by famous scholars such as Pierre Larousse, an encyclopedist, and Elysée Reclus, a geograph...
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Nature 503, 355–359 (2013); doi:10.1038/nature12760 In Fig. 1a of this Article, the highest value on the colour scale should be 11,772 instead of 1,772. This has been corrected in the HTML and PDF versions of ...
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Carbon dioxide (CO2) transfer from inland waters to the atmosphere, known as CO2 evasion, is a component of the global carbon cycle. Global estimates of CO2 evasion have been hampered, however, by the lack of a f...
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The terrestrial surface, the “skin of the earth”, is an important interface for global (geochemical) material fluxes between major reservoirs of the Earth system: continental and oceanic crust, ocean and atmos...
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We present a spatially explicit global overview of nearshore coastal types, based on hydrological, lithological and morphological criteria. A total of four main operational types act as active filters of both ...
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Comparing atmospheric inversion estimates of the carbon fluxes of continents with bottom-up estimates (Pacala et al. 2001; Janssens et al. 2003; Peylin et al. 2005) is no easy task because (1) inversion fluxes...
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This paper provides a global synthesis of reactive nitrogen (Nr) loading to the continental landmass and subsequent riverine nitrogen fluxes under a gradient of anthropogenic disturbance, from pre-industrial t...
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This volume is a synthesis of the research undertaken by the Biospheric Aspects of the Hydrological Cycle (BAHC) Core Project of the International Geosphere-Biosphere Programme (IGBP) since its inception in 19...
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The foregoing parts demonstrate that the dynamics and biophysical character of land-atmosphere interactions are intimately connected to the dynamics and biophysical character of the land-based water cycle. The...
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