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hdv-13_fruit_bodies [2019/10/30 15:26]
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hdv-13_fruit_bodies [2020/11/13 09:36] (aktuell)
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-{{ :hdv-13.jpg?200|HdV-13}}<fs medium>**Type: **HdV-13\\ \\ **Category: **Fungi\\ \\ **Taxonomical identification: **//Entophyctis lobata//\\ \\ **First publication: **van Geel, B. (1978) A palaeoecological study of Holocene peat bog sections in Germany and the Netherlands, based on the analysis of pollen, spores and macro- and microscopic remains of fungi, algae cormophytes and anymals. Review of Palaeobotany and Palynology 25, 1–120\\ \\ **Other publication/s: **\\ van Geel, B., Bohncke, S.J.P. and Dee, H. (1981) A palaecological study of an upper Late Glacial and Holocene sequence from 'De Borchert', The Netherlands. Review of Palaeobotany and Palynology 31, 367–448\\ Kurhy, P. (1985) Transgressions of a raised bog across a coverstand ridge originally covered with an oak-lime forest. Review of Palaeobotany and Palynology 44, 313–353\\ Kuhry, P. (1997) The palaeoecology ot a treed bog in western boreal Canada: a study based on microfossils, macrofossils and physico-chemical properties. Review of Palaeobotany and Palynology 96, 183–224 \\ \\ **Description: **Sporangia crenulate, 18–40 × 18–32 µm, about 6 µm high and 0,5 µm thick walls. The exit pore, often observed at the upper side of the HdV-13 sporangia, is 4–7 µm in diameter. The inner part is closed, apart from a small pore in the center. It is restricted to the ombrotrophic part of the section of this research.\\ \\ **(Sub-) Fossil occurence: **In the most oligotrophic, wet //Scheuchzeria// peat; Part of a //Sphagnum// peat.\\ \\ **Co-occurence: **No information\\ \\ **Modern occurence: **No information\\ \\ **Palaeoenvironmental indication: **Ombrotrophic conditions\\ \\ </fs> +{{ :hdv-13.jpg?200|HdV-13}}<fs medium>**Type: **HdV-13\\ \\ **Category: **Fungi\\ \\ **Taxonomical identification: **//Entophyctis lobata//\\ \\ **First publication: **van Geel, B. (1978) A palaeoecological study of Holocene peat bog sections in Germany and the Netherlands, based on the analysis of pollen, spores and macro- and microscopic remains of fungi, algae cormophytes and anymals. Review of Palaeobotany and Palynology 25, 1–120\\ \\ **Other publication/s: **\\ van Geel, B., Bohncke, S.J.P. and Dee, H. (1981) A palaecological study of an upper Late Glacial and Holocene sequence from 'De Borchert', The Netherlands. Review of Palaeobotany and Palynology 31, 367–448\\ Kurhy, P. (1985) Transgressions of a raised bog across a coversand ridge originally covered with an oak-lime forest. Review of Palaeobotany and Palynology 44, 313–353\\ Kuhry, P. (1997) The palaeoecology ot a treed bog in western boreal Canada: a study based on microfossils, macrofossils and physico-chemical properties. Review of Palaeobotany and Palynology 96, 183–224 \\ \\ **Description: **Sporangia crenulate, 18–40 × 18–32 µm, about 6 µm high and 0,5 µm thick walls. The exit pore, often observed at the upper side of the HdV-13 sporangia, is 4–7 µm in diameter. The inner part is closed, apart from a small pore in the center. It is restricted to the ombrotrophic part of the section of this research.\\ \\ **(Sub-) Fossil occurence: **In the most oligotrophic, wet //Scheuchzeria// peat; Part of a //Sphagnum// peat.\\ \\ **Co-occurence: **No information\\ \\ **Modern occurence: **No information\\ \\ **Palaeoenvironmental indication: **Ombrotrophic conditions\\ \\ </fs>