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1

Moser, Barbara, Marek Metslaid, Lorenz Walthert, Ulrich Wasem, and Thomas Wohlgemuth. "Verjüngungspotenzial verschiedener Waldföhrenund Fichtenherkünfte bei variabler Trockenheit." Schweizerische Zeitschrift fur Forstwesen 166, no. 6 (2015): 399–407. http://dx.doi.org/10.3188/szf.2015.0399.

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Regeneration potential of different Scots pine and Norway spruce provenances under variable drought Rising temperatures will lead to extended periods of summer drought, which may challenge the persistence of Scots pine and Norway spruce in dry alpine valleys where these species play an important role in the protection against natural hazards. We tested whether the natural regeneration of the two species in the Rhine valley near Chur, Switzerland, might be limited under future climatic conditions and we compared the performance of autochthonous provenances with that of seedlings originating fro
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Mager, Sarah, Sean Fitzsimons, Russell Frew, Denis Samyn, and Reginald Lorrain. "Composition and origin of amber ice and its influence on the behaviour of cold glaciers in the McMurdo Dry Valleys, Antarctica." Journal of Glaciology 55, no. 190 (2009): 363–72. http://dx.doi.org/10.3189/002214309788608688.

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AbstractThis paper examines the basal ice sequence of Rhone Glacier, a cold-based glacier in the McMurdo Dry Valleys, Antarctica, using isotopic and solute chemistry data. Three different ice facies are identified: englacial, amber and stratified. The englacial facies is clean, bubbly ice of meteoric origin and is underlain by an amber facies. Amber ice is a characteristic of cold alpine glaciers in the McMurdo Dry Valleys and is distinctive for its high solute concentrations and much higher strain rates compared with the overlying englacial ice and the underlying stratified ice. Analysis of t
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Jacquet, O., M. Laurent, J. Oustric, et al. "CLONAL SELECTION IN THE RHONE VALLEY." Acta Horticulturae, no. 528 (May 2000): 739–46. http://dx.doi.org/10.17660/actahortic.2000.528.110.

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Moser, Barbara, Christoph Bachofen, and Thomas Wohlgemuth. "Föhrenverjüngung: Plastizität und Akklimatisation in einem trockeneren Klima." Schweizerische Zeitschrift fur Forstwesen 169, no. 5 (2018): 269–78. http://dx.doi.org/10.3188/szf.2018.0269.

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Pine regeneration: plasticity and acclimation in a dryer climate Increasing summer drought might limit the natural regeneration of Scots pine stands at low elevations of the Rhone valley. Common garden experiments at the forest-steppe ecotone have shown that emergence and establishment of Scots pine primarily depend on spring precipitation and, to a minor degree, on summer drought and rising temperatures. Scots pine seedlings acclimated rapidly to drought periods by favouring root to shoot growth. In the second year, the saplings were already adapted to drought so that most of them survived an
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Fleuriet, Annie, Robert Kalmes, Luis Pascual, and Georges Periquet. "Comparative evolution of P–M system and infection by the sigma virus in French and Spanish populations of Drosophila melanogaster." Genetical Research 60, no. 2 (1992): 77–86. http://dx.doi.org/10.1017/s0016672300030779.

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SummaryIn 1983, an extensive survey of populations of D. melanogaster was started in a southern French region (Languedoc) in two non-Mendelian systems: the P–M system of transposable elements and the hereditary Rhabdovirus sigma. Unexpectedly fast-evolving phenomena were observed and interesting correlations were noted, giving similar geographical pattern to the region in both systems. For these reasons, the analysis was continued and extended towards the north (Rhône Valley) and the south (Spain). In the P–M system, all the Languedoc populations evolved from 1983 to 1991 towards the Q type wh
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Hołodnik, Daria. "Collaborative Performances of Wine Tourism Destinations in the Northern Rhone Valley." European Management Studies 2023, no. 4 (2024): 30–48. http://dx.doi.org/10.7172/2956-7602.102.2.

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Purpose: The main aim of this article was to identify the wine tourism destination models set up on collaborative performances driven by Tourism Offices (Destination Marketing Organization, DMO) and wineries (private enterprises) from the appellate areas in the Northen Rhone Valley. Design/methodology/approach: The ethnographical methodology was used, including methods of participating observation (applied by a mysterious tourist method), study tours (to explore the study field), expert analysis (based on knowledge exchange with Tourism Office Managers) and official interviews (with Mangers of
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Tonini, Marj, Andrea Pedrazzini, Ivanna Penna, and Michel Jaboyedoff. "Spatial pattern of landslides in Swiss Rhone Valley." Natural Hazards 73, no. 1 (2013): 97–110. http://dx.doi.org/10.1007/s11069-012-0522-9.

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Fresnay, S., A. Hally, C. Garnaud, E. Richard, and D. Lambert. "Heavy precipitation events in the Mediterranean: sensitivity to cloud physics parameterisation uncertainties." Natural Hazards and Earth System Sciences 12, no. 8 (2012): 2671–88. http://dx.doi.org/10.5194/nhess-12-2671-2012.

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Abstract. In autumn, southeastern France is often affected by heavy precipitation events which may result in damaging flash-floods. The 20 October and 1 November 2008 are two archetypes of the meteorological situations under which these events occur: an upper-level trough directing a warm and moist flow from the Mediterranean towards the Cévennes ridge or a quasi stationary meso-scale convective complex developing over the Rhone valley. These two types of events exhibit a contrasting level of predictability; the former being usually better forecast than the latter. Control experiments performe
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Schmidli, Juerg, and Julian Quimbayo-Duarte. "Diurnal Valley Winds in a Deep Alpine Valley: Model Results." Meteorology 2, no. 1 (2023): 87–106. http://dx.doi.org/10.3390/meteorology2010007.

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Thermally driven local winds are ubiquitous in deep Alpine valleys during fair weather conditions resulting in a unique wind climatology for any given valley. The accurate forecasting of these local wind systems is challenging, as they are the result of complex and multi-scale interactions. Even more so, if the aim is an accurate forecast of the winds from the near-surface to the free atmosphere, which can be considered a prerequisite for the accurate prediction of mountain weather. This study combines the evaluation of the simulated surface winds in several Alpine valleys with a more detailed
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Dengler, Jürgen. "The beauty of xerothermic vegetation complexes in Ausserberg (Rhone valley, Switzerland)." Palaearctic Grasslands - Journal of the Eurasian Dry Grassland Group, no. 38 (October 2018): 34–38. http://dx.doi.org/10.21570/edgg.pg.38.34-38.

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Schmid, Fabienne, Juerg Schmidli, Maxime Hervo, and Alexander Haefele. "Diurnal Valley Winds in a Deep Alpine Valley: Observations." Atmosphere 11, no. 1 (2020): 54. http://dx.doi.org/10.3390/atmos11010054.

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Diurnal valley winds frequently form over complex topography, particularly under fair weather conditions, and have a significant impact on the local weather and climate. Since diurnal valley winds result from complex and multi-scale interactions, their representation in numerical weather prediction models is challenging. Better understanding of these local winds based on observations is crucial to improve the accuracy of the forecasts. This study investigates the diurnal evolution of the three-dimensional mean wind structure in a deep Alpine valley, the Rhone valley at Sion, using data from a
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Schoch‐Baumann, Anna, Jan Henrik Blöthe, Henry Munack, et al. "Postglacial outsize fan formation in the Upper Rhone valley, Switzerland – gradual or catastrophic?" Earth Surface Processes and Landforms 47, no. 4 (2022): 1032–53. http://dx.doi.org/10.1002/esp.5301.

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Gargani, J. "Modelling of the erosion in the Rhone valley during the Messinian crisis (France)." Quaternary International 121, no. 1 (2004): 13–22. http://dx.doi.org/10.1016/j.quaint.2004.01.020.

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14

CARISSIMO, B., O. MARCHAND, and E. DUPONT. "Boundary layer turbulence in the Rhone valley as seen with four acoustic sounders." International Journal of Remote Sensing 15, no. 2 (1994): 467–77. http://dx.doi.org/10.1080/01431169408954087.

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15

Blès, J. L., and Y. Gros. "Stress field changes in the Rhone Valley from the Miocene to the present." Tectonophysics 194, no. 3 (1991): 265–77. http://dx.doi.org/10.1016/0040-1951(91)90264-s.

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Duffa, C., and P. Renaud. "An assessment of plutonium and americium distribution in the lower Rhone Valley environment (France)." Radioprotection 37, no. C1 (2002): C1–1259—C1–1263. http://dx.doi.org/10.1051/radiopro/2002157.

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Fritsche, Stefan, Donat Fäh, and Gabriela Schwarz-Zanetti. "Historical intensity VIII earthquakes along the Rhone valley (Valais, Switzerland): primary and secondary effects." Swiss Journal of Geosciences 105, no. 1 (2012): 1–18. http://dx.doi.org/10.1007/s00015-012-0095-3.

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Violin-Wigent, Anne. "Tu lui les as donnés ?" Revue Romane / Langue et littérature. International Journal of Romance Languages and Literatures 48, no. 1 (2013): 32–50. http://dx.doi.org/10.1075/rro.48.1.02vio.

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Tuaillon (1983) claims that variation in the order of third-person multiple object pronouns is a “clear regionalism” from the lower Rhone valley. To investigate this phenomenon in Briançon, a small town in southeastern France, 41 participants from this area filled out an acceptability judgment questionnaire, evaluating sentences with such pronouns in different orders. The results of statistical tests show that, even though participants prefer the standard French order, they also accept the reversed order (standard ‘le lui’ vs. reversed ‘lui le’). The analysis also suggests a change in apparent
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Dengler, Jürgen, Stefan Widmer, Eline Staubli, et al. "Dry grasslands of the central valleys of the Alps from a European perspective: the example of Ausserberg (Valais, Switzerland)." Hacquetia 18, no. 2 (2019): 155–77. http://dx.doi.org/10.2478/hacq-2019-0008.

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Abstract The upper Rhone valley in the Swiss canton of Valais is one of the driest and most continental of the inner-alpine valleys and harbours a rich xerothermic flora. We studied syntaxonomy and ecology of dry grasslands and their species richness patterns. In 2018 we recorded 28 vegetation plots (10 m2) and three nested-plot series of 0.0001 to 100 m2 on the south-facing slopes above the village of Ausserberg. Mean richness of all species ranged from 1.7 on 1 cm2 to 47.3 on 100 m2, with little contribution of bryophytes and lichens. The species-area relationship for total richness closely
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Becker, Patrick, Martin Funk, Christian Schlüchter, and Kolumban Hutter. "A study of the Würm glaciation focused on the Valais region (Alps)." Geographica Helvetica 72, no. 4 (2017): 421–42. http://dx.doi.org/10.5194/gh-72-421-2017.

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Abstract. During the Last Glacial Maximum (LGM), the glaciation in the European Alps reached maximum ice extent. We already simulated the steady states of the Alpine ice coverage for several climate drivers in Becker et al. (2016) and heighten in this article such studies for the Swiss Valais region. To this end, we employ the Parallel Ice Sheet Model (PISM), which combines the shallow ice approximation (SIA) with basal sliding elements of the shallow shelf approximation (SSA), and subject this model to various external driving mechanisms. We further test the sensitivity of this kind of the ic
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21

Beres, Milan, Alan G. Green, and Andre Pugin. "Diapiric origin of the Chessel-Noville Hills of the Rhone Valley interpreted from georadar mapping." Environmental and Engineering Geoscience 6, no. 2 (2000): 141–53. http://dx.doi.org/10.2113/gseegeosci.6.2.141.

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Abstract In an attempt to understand the origin of the enigmatic Chessel-Noville hills in the Rhone River plain of western Switzerland, we have recorded two and three-dimensional ground-penetrating radar (georadar) data and drilled six shallow boreholes. Cross-sections and maps of horizons extracted from the georadar data reveal normal fault zones under the hill flanks and minor grabens and domes below the hill crests. Comparable graben-like structures with normal step faults converging with depth are observed at a nearby outcrop. Fine sand and silt within some of the exposed faults may have b
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Gimmi, Urs, Matthias Bürgi, and Martin Stuber. "Reconstructing Anthropogenic Disturbance Regimes in Forest Ecosystems: A Case Study from the Swiss Rhone Valley." Ecosystems 11, no. 1 (2007): 113–24. http://dx.doi.org/10.1007/s10021-007-9111-2.

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Hübner, Roland, Tiziano Maddalena, Jeremy B. Searle, and Peter Vogel. "The HSR on chromosome 1 of the house mouse, Mus domesticus: distribution and frequency in Switzerland." Genetical Research 64, no. 2 (1994): 107–14. http://dx.doi.org/10.1017/s0016672300032717.

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SummaryA total of 357 house mice (Mus domesticus) from 83 localities uniformly distributed throughout Switzerland were screened for the presence of a homogenously staining region (HSR) on chromosome 1. Altogether 47 mice from 11 localities were HSR/ + or HSR/HSR. One sample of 11 individuals all had an HSR/HSR karyotype. Almost all mice with the variant were collected from the Rhone valley (HSR frequency: 61%) and Val Bregaglia (HSR frequency: 81%). For samples from most of thearea of Switzerland, the HSR was absent. There was no strong association between the geographic distribution of the HS
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Dobbertin, Matthias, Beat Wermelinger, Christof Bigler, et al. "Linking Increasing Drought Stress to Scots Pine Mortality and Bark Beetle Infestations." Scientific World JOURNAL 7 (2007): 231–39. http://dx.doi.org/10.1100/tsw.2007.58.

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In the dry Swiss Rhone Valley, Scots pine forests have experienced increased mortality in recent years. It has commonly been assumed that drought events and bark beetles fostered the decline, however, whether bark beetle outbreaks increased in recent years and whether they can be linked to drought stress or increasing temperature has never been studied.In our study, we correlated time series of drought indices from long-term climate stations, 11-year mortality trends from a long-term research plot, and mortality probabilities modeled from tree rings (as an indicator of tree vitality) with docu
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Sabon, Isabelle, Gilles de Revel, Yorgos Kotseridis, and Alain Bertrand. "Determination of Volatile Compounds in Grenache Wines in Relation with Different Terroirs in the Rhone Valley." Journal of Agricultural and Food Chemistry 50, no. 22 (2002): 6341–45. http://dx.doi.org/10.1021/jf025611k.

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Duffa, C., and P. Renaud. "238Pu and 239+240Pu inventory and distribution through the lower Rhone valley terrestrial environment (Southern France)." Science of The Total Environment 348, no. 1-3 (2005): 164–72. http://dx.doi.org/10.1016/j.scitotenv.2004.12.064.

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Bruneton, Hélène, Gilles Arnaud-Fassetta, Mireille Provansal, and Dorit Sistach. "Geomorphological evidence for fluvial change during the Roman period in the lower Rhone valley (southern France)." CATENA 45, no. 4 (2001): 287–312. http://dx.doi.org/10.1016/s0341-8162(01)00143-6.

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Maurer, H. R., M. Burkhard, N. Deichmann, and A. G. Green. "Active tectonism in the central Alps: contrasting stress regimes north and south of the Rhone Valley." Terra Nova 9, no. 2 (1997): 91–94. http://dx.doi.org/10.1111/j.1365-3121.1997.tb00010.x.

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van der Leeuw, Sander E., and The ARCHAEOMEDES research team. "Climate, hydrology, land use, and environmental degradation in the lower Rhone Valley during the Roman period." Comptes Rendus Geoscience 337, no. 1-2 (2005): 9–27. http://dx.doi.org/10.1016/j.crte.2004.10.018.

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Fatichi, S., S. Rimkus, P. Burlando, R. Bordoy, and P. Molnar. "Elevational dependence of climate change impacts on water resources in an Alpine catchment." Hydrology and Earth System Sciences Discussions 10, no. 3 (2013): 3743–94. http://dx.doi.org/10.5194/hessd-10-3743-2013.

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Abstract. An increasing interest is directed toward understanding impacts of climate change on water related sectors in a particularly vulnerable area such as the Alpine region. We present a distributed hydrological analysis at scale significant for water management for pristine, present-days, and projected future climate conditions. We used the upper Rhone basin (Switzerland) as a test case for understanding anthropogenic impacts on water resources and flood risk in the Alpine area. The upper Rhone basin includes reservoirs, river diversions and irrigated areas offering the opportunity to stu
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Nedjai, R., Nghiem T. Van, A. Bensaid, and N. Messaoud-Nacer. "Consequences of land use change on lakes and rivers of a midmountain catchment area: application to the Ain watershed (France)." Geography and Tourism 5, no. 2 (2016): 117–30. https://doi.org/10.5281/zenodo.223952.

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The Ain river – tributary of the Rhone, is distinguished by a geological and geomorphological duality splitting it into two very clear parts: the mountainous (karstic-jura mountains) and the low alluvial valley of the Ain river, characterized by agricultural land use. The geographical boundary between the two zones is the dam of Vouglans (3rd water reserve of France). These geological differences give rise to two types of reserves: karstic reserves at the top of the watershed and an alluvial water table enclosed in the quaternary alluvium at the bottom. The last thirty years have been marked b
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Schultz, H. R. "Water in a warmer world – is atmospheric evaporative demand changing in viticultural areas?" BIO Web of Conferences 12 (2019): 01011. http://dx.doi.org/10.1051/bioconf/20191201011.

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The predicted developments in climate are region-specific and adaptation can only be successful considering the regional characteristics with its diverse technical, environmental, economic and social implications. One of the key concerns for many regions is the availability of water through precipitation, the distribution of precipitation throughout the year, and possible changes in evaporative demand of the atmosphere and thus water use. From rising temperatures it is mostly assumed that water holding capacity of the atmosphere will increase in the future as a function of the Clausius-Clapeyr
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Pautou, Guy, Jacky Girel, and Jean-Luc Borel. "Initial repercussions and hydroelectric developments in the French upper rhone valley: A lesson for predictive scenarios propositions." Environmental Management 16, no. 2 (1992): 231–42. http://dx.doi.org/10.1007/bf02393828.

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Clivaz, Mélanie, and Emmanuel Reynard. "How to Integrate Invisible Geomorphosites in an Inventory: a Case Study in the Rhone River Valley (Switzerland)." Geoheritage 10, no. 4 (2017): 527–41. http://dx.doi.org/10.1007/s12371-017-0222-7.

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Dorocki, Sławomir. "Kształtowanie się regionów przemysłowych Francji." Studies of the Industrial Geography Commission of the Polish Geographical Society 10 (January 1, 2008): 45–54. http://dx.doi.org/10.24917/20801653.10.4.

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The subject of the article is the process of creating industrial regions of France. On the basis of statistical data and referring to the number of employees in the industry, the number of industrial plants and the dimension of industrial production, an attempt at industrial regions delimitation has been made. Workshops dominated industrial activity up to the 19th century. They were mostly situated in densely populated northern parts of France.The factor which initiated the process of industry concentration was the invention of the steam engine. This dependence of industry on the steam engine
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Dergunov, A. V., and S. A. Lopin. "TECHNOCHEMICAL CHARACTERISTICS AND AROMA-FLAVOR FEATURES OF ALSACE AND RHONE VALLEY GRAPE VARIETIES UNDER ANAPA TERROIR`S CONDITION." Scientific Works of North Caucasian Federal Scientific Center of Horticulture, Viticulture, Wine-making 23 (June 2019): 225–29. http://dx.doi.org/10.30679/2587-9847-2019-23-225-229.

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Delhon, Claire, Nicolas Bernigaud, Jean-François Berger, Pierre-Gil Salvador, Stéphanie Thiébault, and Maheul Ploton. "Evolution and management of humid landscapes in northern Dauphiné (Rhone valley, France): Contribution of charcoal and wood studies." Holocene 23, no. 10 (2013): 1447–65. http://dx.doi.org/10.1177/0959683613493934.

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Smelror, Morten, and Han Leereveld. "Dinoflagellate and Acritarch assemblages from the late Bathonian to early Oxfordian of Montagne Crussol, Rhone valley, southern France." Palynology 13, no. 1 (1989): 121–41. http://dx.doi.org/10.1080/01916122.1989.9989358.

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Daujeard, Camille, and Marie-Hélène Moncel. "On Neanderthal subsistence strategies and land use: A regional focus on the Rhone Valley area in southeastern France." Journal of Anthropological Archaeology 29, no. 3 (2010): 368–91. http://dx.doi.org/10.1016/j.jaa.2010.05.002.

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Perron, N., J. Sandradewi, M. R. Alfarra, et al. "Composition and sources of particulate matter in an industrialised Alpine valley." Atmospheric Chemistry and Physics Discussions 10, no. 4 (2010): 9391–430. http://dx.doi.org/10.5194/acpd-10-9391-2010.

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Abstract. A three-week long field campaign was carried out under autumnal meteorological conditions at four valley floor sites in the industrialised Swiss Rhone Valley. For one week of stable meteorological conditions, particulate matter with an aerodynamic diameter below 10 μm (PM10) was analysed from daily filters using ion chromatography, X-ray fluorescence, anhydrosugars and radiocarbon analysis of the organic and elemental matter (OM and EM, respectively). Furthermore, PM1 composition along the whole campaign was monitored in Massongex (a site near industries) by a seven-wavelength aethal
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Duverger, Clara, Gilles Mazet-Roux, Laurent Bollinger, et al. "A decade of seismicity in metropolitan France (2010–2019): the CEA/LDG methodologies and observations." BSGF - Earth Sciences Bulletin 192 (2021): 25. http://dx.doi.org/10.1051/bsgf/2021014.

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We summarize ten years of the French seismicity recorded by the Geophysical and Detection Laboratory (LDG) of the French Alternative Energies and Atomic Energy Commission (CEA) network from 2010 to 2019. During this period, 25 265 natural earthquakes were detected by the LDG and located within metropolitan France and its immediate vicinity. This seismicity contributes to more than 47% of the natural earthquakes instrumentally recorded since 1962 (mainly due to the improvement of network capacity), and includes about 28% of the most significant earthquakes with a magnitude ML ≥ 4.0. Recent seis
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Dobbertin, M., and A. Rigling. "Pine mistletoe (Viscum album ssp. austriacum) contributes to Scots pine (Pinus sylvestris) mortality in the Rhone valley of Switzerland." Forest Pathology 36, no. 5 (2006): 309–22. http://dx.doi.org/10.1111/j.1439-0329.2006.00457.x.

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Eyrolle, F., C. Duffa, C. Antonelli, B. Rolland, and F. Leprieur. "Radiological consequences of the extreme flooding on the lower course of the Rhone valley (December 2003, South East France)." Science of The Total Environment 366, no. 2-3 (2006): 427–38. http://dx.doi.org/10.1016/j.scitotenv.2005.12.010.

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Schürch, Marc, and Vuataz François-D. "Groundwater components in the alluvial aquifer of the alpine Rhone River valley, Bois de Finges area, Wallis Canton, Switzerland." Hydrogeology Journal 8, no. 5 (2000): 549–63. http://dx.doi.org/10.1007/s100400000094.

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Vaudour, E. "Remote sensing of Red Mediterranean soils: a case study in the viticultural southern Rhone Valley using SPOT satellite imagery." Geocarto International 23, no. 3 (2008): 197–216. http://dx.doi.org/10.1080/10106040701207555.

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Chapuis, Hervé, Jordan Ré-Bahuaud, Joël Jolivet, and Didier Graillot. "Les gorges de la Cèze. Élaboration d’un modèle chronologique à partir des données géologiques : conséquences sur l’hydrogéologie." Karstologia : revue de karstologie et de spéléologie physique 75, no. 1 (2020): 3–6. https://doi.org/10.3406/karst.2020.3323.

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The gorges of the river Cèze -Development of a chronological model based on geological data : implications for hydrogeology. The content presented in this article is an integral part of the research work carried out with the aim of characterizing, evaluating and modeling the exchanges between the Cèze River and its karstic system that it crosses in the middle part of the valley [ Chapuis, 2017]. This paper presents the Cèze watershed with a lithological description of the terrain to lead to a chronological model in order to better understand the implication on the flow of water. Geological ana
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Panzera, Francesco, Jonas Alber, Walter Imperatori, Paolo Bergamo, and Donat Fäh. "Reconstructing a 3D model from geophysical data for local amplification modelling: The study case of the upper Rhone valley, Switzerland." Soil Dynamics and Earthquake Engineering 155 (April 2022): 107163. http://dx.doi.org/10.1016/j.soildyn.2022.107163.

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Doyen, Élise, Boris Vannière, Jean-François Berger, Fabien Arnaud, Kazuyo Tachikawa, and Edouard Bard. "Land-use changes and environmental dynamics in the upper Rhone valley since Neolithic times inferred from sediments in Lac Moras." Holocene 23, no. 7 (2013): 961–73. http://dx.doi.org/10.1177/0959683612475142.

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Meier, Michael, Jürg Fuhrer, and Annelie Holzkämper. "Changing risk of spring frost damage in grapevines due to climate change? A case study in the Swiss Rhone Valley." International Journal of Biometeorology 62, no. 6 (2018): 991–1002. http://dx.doi.org/10.1007/s00484-018-1501-y.

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BAUZA, T., M. KELLY, and A. BLAISE. "Study of polyamines and their precursor amino acids in Grenache noir and Syrah grapes and wine of the Rhone Valley." Food Chemistry 105, no. 1 (2007): 405–13. http://dx.doi.org/10.1016/j.foodchem.2006.12.046.

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