首页> 外文期刊>Grana: An International Journal of Palynology and Aerobiology >Combined LM and SEM study of the middle Miocene (Sarmatian) palynoflora from the Lavanttal Basin, Austria: part III. Magnoliophyta 1 - Magnoliales to Fabales
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Combined LM and SEM study of the middle Miocene (Sarmatian) palynoflora from the Lavanttal Basin, Austria: part III. Magnoliophyta 1 - Magnoliales to Fabales

机译:奥地利拉万塔尔盆地中新世(Sarmatian)古植物区系的LM和SEM组合研究:第三部分。木兰属植物1-木兰属到Fabales

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Previous studies on the palynoflora from the Lavanttal Basin show that it contains a rich assemblage of spores and gymnosperm pollen. Present and ongoing investigations of dispersed angiosperm pollen suggest a high diversity within this group, and due to the excellent preservation of the material, some rare pollen types are recognised. The Magnoliales to Fabales pollen record documented here contains 30 different taxa. Only a few pollen types are assigned to Magnoliids (four taxa); these are rare in the pollen record. Similarly, the Commelinids comprise five taxa and are also rare. Most of the angiosperm pollen originates from Eudicots (21 taxa). Of the angiosperm taxa documented here, Magnolia, Carex, Ranunculaceae, Platanus, Trochodendron, Buxus, Cercidiphyllum, Daphniphyllum, Distylium, Fortunearia, Parrotia, Parthenocissus, Vitis, Euphorbia, Salix and Papilionoideae are recorded for the first time from the Lavanttal Basin. This also includes the first fossil pollen record of Trochodendron worldwide and the first reliable pollen record of Daphniphyllum. Several of the taxa described here had a wide Northern Hemispheric distribution from the Eocene until the end of the Miocene. Also, key relatives of the fossil taxa are presently confined to humid warm-temperate environments, suggesting a very mild climate during the middle Miocene (Sarmatian) of the Lavanttal area. Some of the taxa encountered also support previous observations that the sediments of the Lavanttal Basin accumulated in a lowland wetland environment. This is based on pollen from aquatic taxa thriving in lakes, streams and swamps, and pollen from terrestrial plant taxa occupying margins of lakes and streams, backswamps, floodplains, river plains and hummocks. Other angiosperm pollen clearly originates from plants thriving on drier substrates, reflecting various vegetation units of the mixed evergreen/deciduous broad-leaved/conifer forests surrounding the wetland basin.
机译:先前对拉凡特盆地的古生物进行的研究表明,它含有丰富的孢子和裸子植物花粉。目前和正在进行的对被子植物花粉分散的研究表明,该类植物中花粉的多样性很高,并且由于材料的优异保存,因此可以识别出一些罕见的花粉类型。此处记载的木兰至Fabales花粉记录包含30种不同的分类单元。仅少数花粉类型分配给了木兰类(四个类群)。这些在花粉记录中很少见。同样,Commelinids包含五个类群,也很少见。大多数被子植物花粉起源于Eudicots(21类群)。在这里记录的被子植物分类群中,首次从拉万特记录了木兰,Carex,毛an科,悬铃木,Trochodendron,雀舌,鹿角蕨,菊科,茎粉,香,鹦鹉螺,爬山虎,葡萄,大戟,柳和兜兰科。这还包括世界范围内首个Trochodendron的化石花粉记录和Daphniphyllum的第一个可靠花粉记录。从始新世到中新世末期,这里描述的几种分类单元具有广泛的北半球分布。此外,化石分类的主要亲属目前仅限于潮湿的温带环境,这表明在拉万塔尔地区中新世中期(萨尔马特时期)气候非常温和。遇到的一些分类单元也支持以前的观察,即拉瓦塔尔盆地的沉积物在低地湿地环境中积累。这是基于水生生物分类的花粉在湖泊,溪流和沼泽繁盛,以及陆生植物分类的花粉占据了湖泊和溪流,后沼泽,洪泛区,河川平原和山岗的边缘。其他被子植物花粉显然起源于在较干燥的基质上繁衍生息的植物,反映了湿地盆地周围常绿/落叶阔叶/针叶树混交林的各种植被单元。

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