乌克兰顿涅茨盆地Belaya Kalitva组化石植物生物损伤(上巴什基里亚石炭世

V. Dernov
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引用次数: 0

摘要

从乌克兰东部卢甘斯克地区南部Belaya Kalitva组(晚巴什基尔阶,石炭纪)中部的粉砂岩中研究了主要由陆生节肢动物(如千足虫、螨虫和昆虫)引起的陆生植物的生物损害。所研究的痕迹被划分为Labandeira等人开发的数字分类学的13种损伤类型(DT)。(2007):外部叶片取食DTs03,12,13,14,15,75,78,81,103;穿刺抽吸DT46;磨损DT146;产卵DT102和DT108。所有研究的生物破坏都来自位于沿海堆积低地的浅水湖沉积物。与更古老的Mospyne组的动植物相互作用的证据相比,Belaya Kalitva组的植物生物破坏具有一些特征,例如没有真菌的痕迹,通常生物破坏的频率更高。与Mospyne组一样,Belaya Kalitva组缺乏种子喂养的痕迹。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Fossil plant biodamages from the Belaya Kalitva Formation (upper Bashkirian, Carboniferous) of the Donets Basin, Ukraine
Biodamages of terrestrial plants caused mainly by terrestrial arthropods, e.g. millipedes, mites, and insects, were studied from siltstones of the middle part of the Belaya Kalitva Formation (late Bashkirian, Carboniferous) of the southern part of Luhansk Region, eastern Ukraine. The traces studied were assigned to 13 damage types (DT) of the numerological systematics developed by Labandeira et al. (2007): external foliage feeding DTs03, 12, 13, 14, 15, 75, 78, 81, 103; piercing-and-sucking DT46; galling DT146; oviposition DT102 and DT108. All studied biodamages come from sediments of a shallow lake located on a coastal accumulative lowland. Compared to evidence of animal-plant interactions of a more ancient Mospyne Formation, plant biodamages from the Belaya Kalitva Formation have some characteristic features, e.g. the absence of traces of fungi and, generally, a higher frequency of biodamages. As in the Mospyne Formation, the Belaya Kalitva Formation lacks traces of seed feeding.
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CiteScore
0.80
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