By Krisztina Buczkó, János Korponai, Judit Padisák, Scott W. Starratt
Palaeolimnology is without doubt one of the such a lot quickly constructing fields of limnology. the first goal of this quantity is to offer new palaeolimnological findings from japanese and critical Europe. even supposing this sector has occasionally bought much less cognizance than different parts of Europe, the lakes and mires, coupled with the variety in panorama and the neighborhood alterations in weather, offer targeted chance for learning palaeolimnology. the quantity begins with a assessment on past due Quaternary files shape the Carpathian zone, via new effects at the background of a crater lake, Lake Saint Ana, glacial lakes within the Tatra Mountains and Lake Bled in Slovenia. furthermore, a number of the papers offer new insights at the improvement of lakes and bathrooms in the course of the overdue glacial and Holocene, utilizing a variety of palaeolimnological proxies, together with diatoms, pollen, macrofossils, pigments, cladoceran continues to be, chironomids, chaoborids, good isotopes and geochemistry. the inducement for gathering fresh wisdom derives from the popularity of the significance, and applicability of palaeolimnological instruments to assist in defining "reference stipulations" as exact in the Water Framework Directives and estimating effect of worldwide weather swap on floor waters.
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Additional info for Palaeolimnological Proxies as Tools of Environmental Reconstruction in Fresh Water
Szegva´ri & T. To¨r} ocsik, 2006. Mez} olak-Sze´lmez} o t} ozegla´p geoarcheolo´giai vizsga´lata´nak eredme´nyei. (Effects of the geoarcheological survey on the Mez} olak-Sze´lmez} o peatbog) (in Hungarian). Savaria 29: 147–215. , P. Su¨megi & E. Magyari, 2004a. A new paleobotanical method for the description of Late Quaternary organic sediments (Mire-development pathways and palaeoclimatic records from S Hungary). Acta Geologica Hungarica 47: 1–37. , P. Su¨megi & E. Magyari, 2004b. A new quantitative method for the paleobotanical description of Late Quaternary organic sediments.
1 Location of the study site in Europe and topographic map of the Ciomatu Massif showing the location of Lake Saint Ana. , 2006). By increasing the number of AMS 14C dates and applying higher stratigraphic resolution for the different proxies, this study improves the palaeoenvironmental reconstruction with a special focus on the hydrological changes. Study area Lake Saint Ana is a crater lake in the Ciomatu Massif of the Harghita Mountains (Fig. 1). The lake has no outlet; it is fed by rainwater and inwash from the surrounding slopes (Pa´l, 2000, 2001).
Late Pleistocene vegetation history in Hungary since the last interglacial. In Pe´csi, M. & F. Schweitzer (eds), Quaternary Environments in Hungary. Studies in Geography in Hungary 26. Akade´miai Kiado´, Budapest: 35–46. , 2005a. An overview of the palaeobotanical data from Keleme´r-Kis-Mohos-to´. , I. Juha´sz & P. Su¨megi (eds), Environmental Archaeology in NorthEastern Hungary, Vol. 19. Varia Archaeologica Hungarica, Budapest: 39–45. , 2005b. Detecting antropogenic impacts in the palaeobotanical samples from Csaroda-Nyı´res-to´.