Berane盆地(下中新世)的Nelumbo protospeciosa SAPORTA 1891

Desa Đorđević Milutinović, B. Stevanović, G. Ćulafić
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引用次数: 1

摘要

黑山的Berane盆地以丰富的不同地质年代的古植物群而闻名。晚渐新世至上新世早期,该地区的湖泊保存了不同时代的古植被遗迹。因此,通过研究Berane盆地收集的古植物区系,可以很容易地了解中新世植被的变化。1995年,在早中新世沉积物中的Rosulje (Berane盆地)地区收集了第一个也是唯一已知的水生(漂浮)植物遗迹。根据叶片的叶面形状、叶脉、脉脉、中心盘或叶柄的位置等形态解剖学特征,鉴定为欧亚大陆第三纪广泛分布的原种蓝属(Nelumbo protospeciosa SAP.)。在Rosulje遗址没有其他植物或伴生植被的记录,因此Nelumbo原生种的存在不足以确定其存在期间的栖息地、植被或气候。因此,古环境重建还包括对已经发表的早中新世Luge-Haremi (Berane Basin)地区植物区系的分析和新近的Nelumbo物种的生态气候特征。最后得出结论认为,Nelumbo的叶片直径至少为30 cm,过去可能生活在亚热带/地中海型气候的影响下,生长在开阔、日照充足的地方。
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Nelumbo protospeciosa SAPORTA 1891 from the Berane Basin (Lower Miocene)
Berane Basin in Montenegro has been known for rich paleoflora of diverse geological ages. Theremains of paleovegetation of various ages were preserved by the lake occurring in this area from LateOligocene to Early Pliocene. Therefore, the shifts in vegetation during the Miocene period may be easily followed by studying the paleofloras collected at the Berane Basin. The first and only known remains of aquatic (floating) plants were collected in 1995 at the locality Rosulje (Berane Basin) in the Early Miocene sediments. According to the morphoanatomical characteristics of leaves such as shape of lamina, veins, venation, presence of central disk or position of petiola, the specimens were identified as Nelumbo protospeciosa SAP., a widely distributed form during the Tertiary of Eurasia. No other plants or accompanying vegetation were recorded at the Rosulje site, so presence of Nelumbo protospeciosa was insufficient for determining the habitat, vegetation or climate during its existence. Therefore the paleoenvironmental reconstruction also included analysis of the already published Early Miocene flora from the locality Luge-Haremi (Berane Basin) and eco-climatic characteristics of recent Nelumbo species. At last was concluded that Nelumbo, which had leaves at least 30 cm in diameter, used to inhabit open, well-insolated sites, probably under the influence of the subtropical/Mediterranean-type climate.
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