FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1987138418> ?p ?o ?g. }

• W1987138418 endingPage "81" @default.
• W1987138418 startingPage "53" @default.
• W1987138418 abstract "In the low Venetian plain (northeastern Italy) thick sequences of silt and sand layers alternate with common, thin layers of peat and organic silt; the organic layers in the topmost 30 m of the Late Pleistocene alluvial series span between 23,000 and 14,000 yr BP (radiocarbon dating), in an area measuring 100 km by 30 km. They indicate broad areas where wetlands developed. We aim to understand the features and the origin of the wetlands by undertaking sedimentological, pollen, non-pollen palynomorph and plant macrofossil analyses. Thirteen cores were drilled in the central zone of the low Venetian plain near the coast of the Adriatic Sea and 79 samples were analysed. The palaeoenvironmental reconstruction based on previous pollen analysis did not emphasize the areas where peat layers were formed, suggesting a homogenous steppe environment, typical of a cold and dry climate. They were probably waterlogged for most of the year allowing the formation of peat and the development of local plant communities of mainly aquatic species. Macrofossil and pollen analyses suggest that herbaceous plants, such as Cyperaceae and Poaceae (probably Carex fusca and Phragmites australis), and brown mosses (mainly Scorpidium scorpioides) were the most important components of wetland communities. Fossils of obligate aquatic organisms indicate open water environments, these include macrofossils of Nymphaea, Characeae, Bryozoa and Potamogeton, and non-pollen palynomorphs such as algal resting cells, free cells and colonies (Zygnemataceae, Spirogyra, Mougeotia, Closterium idiosporum, Type 225, Type 229, Botryococcus, Pediastrum cf. boryanum, P. cf. simplex, Ceratium hirundinella, Tetraedron cf. minimum and Type 333), oocytes of aquatic invertebrates (Type 353A and 353B) and incompletely known types probably of algal origin (Type 303, Type 74, Type 128A and 128B). A discontinuous occurrence of fungal spores and other microfossils (Type 200, Gaeumannomyces (Type 126), Glomus (Type 207), Type 351, Type 79, and incompletely known types) suggests frequent fluctuations of the water depth with periodic emersions of the bottom of the ponds or fens. The water quality preferred by the identified species, or suggested in literature for the fossil types, is mainly eutrophic to mesotrophic and rich in cations. Peatland formed in wide, low-lying areas between the fluvial ridges which were periodically inundated by the fluctuating groundwater. Peat accumulated in continuous layers only where the fen organic deposition prevailed the alluvial minerogenic sediment. When alluvial deposition buried the organic deposit, the peat level was incorporated into the stratigraphic record." @default.
• W1987138418 created "2016-06-24" @default.
• W1987138418 creator A5002076176 @default.
• W1987138418 creator A5004231372 @default.
• W1987138418 creator A5022579166 @default.
• W1987138418 creator A5042170109 @default.
• W1987138418 creator A5056735638 @default.
• W1987138418 creator A5068878513 @default.
• W1987138418 creator A5075660744 @default.
• W1987138418 date "2006-08-01" @default.
• W1987138418 modified "2023-10-12" @default.
• W1987138418 title "Wetlands in the Venetian Po Plain (northeastern Italy) during the Last Glacial Maximum: Interplay between vegetation, hydrology and sedimentary environment" @default.
• W1987138418 cites W1966458617 @default.
• W1987138418 cites W1967219328 @default.
• W1987138418 cites W1972468579 @default.
• W1987138418 cites W1976635806 @default.
• W1987138418 cites W1980885201 @default.
• W1987138418 cites W1984909104 @default.
• W1987138418 cites W1995433078 @default.
• W1987138418 cites W1995506238 @default.
• W1987138418 cites W2037359762 @default.
• W1987138418 cites W2038125527 @default.
• W1987138418 cites W2041363260 @default.
• W1987138418 cites W2050504868 @default.
• W1987138418 cites W2079010881 @default.
• W1987138418 cites W2087305554 @default.
• W1987138418 cites W2140630023 @default.
• W1987138418 cites W2168517632 @default.
• W1987138418 doi "https://doi.org/10.1016/j.revpalbo.2006.03.016" @default.
• W1987138418 hasPublicationYear "2006" @default.
• W1987138418 type Work @default.
• W1987138418 sameAs 1987138418 @default.
• W1987138418 citedByCount "71" @default.
• W1987138418 countsByYear W19871384182012 @default.
• W1987138418 countsByYear W19871384182013 @default.
• W1987138418 countsByYear W19871384182014 @default.
• W1987138418 countsByYear W19871384182015 @default.
• W1987138418 countsByYear W19871384182016 @default.
• W1987138418 countsByYear W19871384182017 @default.
• W1987138418 countsByYear W19871384182018 @default.
• W1987138418 countsByYear W19871384182019 @default.
• W1987138418 countsByYear W19871384182020 @default.
• W1987138418 countsByYear W19871384182021 @default.
• W1987138418 countsByYear W19871384182022 @default.
• W1987138418 countsByYear W19871384182023 @default.
• W1987138418 crossrefType "journal-article" @default.
• W1987138418 hasAuthorship W1987138418A5002076176 @default.
• W1987138418 hasAuthorship W1987138418A5004231372 @default.
• W1987138418 hasAuthorship W1987138418A5022579166 @default.
• W1987138418 hasAuthorship W1987138418A5042170109 @default.
• W1987138418 hasAuthorship W1987138418A5056735638 @default.
• W1987138418 hasAuthorship W1987138418A5068878513 @default.
• W1987138418 hasAuthorship W1987138418A5075660744 @default.
• W1987138418 hasConcept C127313418 @default.
• W1987138418 hasConcept C140345934 @default.
• W1987138418 hasConcept C151730666 @default.
• W1987138418 hasConcept C18903297 @default.
• W1987138418 hasConcept C25868968 @default.
• W1987138418 hasConcept C2778169228 @default.
• W1987138418 hasConcept C2778556696 @default.
• W1987138418 hasConcept C2780539527 @default.
• W1987138418 hasConcept C2780618852 @default.
• W1987138418 hasConcept C2781178838 @default.
• W1987138418 hasConcept C46757340 @default.
• W1987138418 hasConcept C53657456 @default.
• W1987138418 hasConcept C559758991 @default.
• W1987138418 hasConcept C67715294 @default.
• W1987138418 hasConcept C86803240 @default.
• W1987138418 hasConceptScore W1987138418C127313418 @default.
• W1987138418 hasConceptScore W1987138418C140345934 @default.
• W1987138418 hasConceptScore W1987138418C151730666 @default.
• W1987138418 hasConceptScore W1987138418C18903297 @default.
• W1987138418 hasConceptScore W1987138418C25868968 @default.
• W1987138418 hasConceptScore W1987138418C2778169228 @default.
• W1987138418 hasConceptScore W1987138418C2778556696 @default.
• W1987138418 hasConceptScore W1987138418C2780539527 @default.
• W1987138418 hasConceptScore W1987138418C2780618852 @default.
• W1987138418 hasConceptScore W1987138418C2781178838 @default.
• W1987138418 hasConceptScore W1987138418C46757340 @default.
• W1987138418 hasConceptScore W1987138418C53657456 @default.
• W1987138418 hasConceptScore W1987138418C559758991 @default.
• W1987138418 hasConceptScore W1987138418C67715294 @default.
• W1987138418 hasConceptScore W1987138418C86803240 @default.
• W1987138418 hasIssue "1-2" @default.
• W1987138418 hasLocation W19871384181 @default.
• W1987138418 hasOpenAccess W1987138418 @default.
• W1987138418 hasPrimaryLocation W19871384181 @default.
• W1987138418 hasRelatedWork W1977644122 @default.
• W1987138418 hasRelatedWork W2062102731 @default.
• W1987138418 hasRelatedWork W2266640097 @default.
• W1987138418 hasRelatedWork W2352358572 @default.
• W1987138418 hasRelatedWork W2365745334 @default.
• W1987138418 hasRelatedWork W2379413617 @default.
• W1987138418 hasRelatedWork W2596457782 @default.
• W1987138418 hasRelatedWork W2756317680 @default.
• W1987138418 hasRelatedWork W3034629243 @default.
• W1987138418 hasRelatedWork W2560835994 @default.
• W1987138418 hasVolume "141" @default.

• next