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- W2890921580 abstract "The shore of the Steinhuder Meer is partly occupied by extensive mires of lacustrine origin. The zonation of their vegetation, as far as left in a relatively undisturbed state, corresponds very well with the sequence of the so-called hydrosere, and so the basic question for the whole investigation arose: How far did the stages involved in this process of terrestrialisation (Verlandung) in the past correspond to the present vegetational zonation? To answer this question macrofossil analyses were made for a number of peat profiles and the results were interpreted with respect to subfossil plant communities. The first part of the investigation, covered by this paper, deals with the present vegetation pattern, with the methods of macrofossil analyses, with the evaluation techniques and with the types of peat forming plant communities obtained from 307 single analyses. These types are compared with present vegetational units and with results of peat analyses of other areas. They cover the whole range between poor bog and rich fen communities. From the view of systematics of the present-day vegetation, most of them are mixtures, floristically intermediate between two or more “pure units”. The occurrence of wood remains in the peats is discussed in detail; it evidently does not indicate that swamp forests (carrs) are peat forming plant communities. The results and discussions concerning the succession and its history will follow later in the second paper." @default.
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- W2890921580 date "1974-01-01" @default.
- W2890921580 modified "2023-10-18" @default.
- W2890921580 title "Zum Verlauf der Verlandung bei einem eutrophen Flachsee (nach quartärbotanischen Untersuchungen am Steinhuder Meer)" @default.
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- W2890921580 doi "https://doi.org/10.1016/s0367-2530(17)31740-1" @default.
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