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首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >Plant-arthropod associations from the Siwalik forests (middle Miocene) of Darjeeling sub-Himalaya, India
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Plant-arthropod associations from the Siwalik forests (middle Miocene) of Darjeeling sub-Himalaya, India

机译:印度喜马拉雅山大吉岭西瓦里克森林(中新世中期)的植物节肢动物协会

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摘要

Fossil leaves from the Siwalik sedimentary rocks of Darjeeling sub-Himalaya, evidence a variety of plant-insect interactions that operated during the evolution of monsoon-influenced forests from middle Miocene times. We assessed the diversity and frequency of insect herbivory on 137 specimens representing the Darjeeling lower Siwalik flora (DLSF). We also examined the percent of leaf area removed by herbivory as an independent measure of the effect of insect herbivore removal of host plant photosynthetic tissue. Five functional feeding groups (FFGs) are identified in this study namely leaf mining, hole feeding, skeletonizing, galling and margin feeding. These traces indicate that insects interacted with the plants for various purposes, including feeding, egg laying and sheltering. Furthermore, these morphotraces tend to suggest similarities in insect interactions with leaves of extant plant species such as Persea, Woodfordia, Shorea, Artocarpus, Callicarpa, Albizia, Lagerstroemia etc. On the basis of comparison with extant taxa, possible leaf feeders could have belonged to the insect orders Orthoptera, Coleoptera, Lepidoptera and Diptera. Although the morphology of the phytophagous insects associated with the fossil leaves is unknown, present findings reveal that many modern plant-insect relationships were established by the Miocene time and continue to the present, shaping both the present day flora and fauna. In the present study we compare insect herbivory at DLSF to that of our previously investigated Arunachal lower Siwalik flora and two younger floras from that area. We note a similar range of FFGs and damage types observed among these four fossil floras and conclude that compared to biotic factors climate had little influence in determining the evolution of plant-insect interactions in the eastern Himalayan region. (C) 2015 Elsevier B.V. All rights reserved.
机译:大麦岭喜马拉雅山西瓦里克沉积岩的化石叶子证明了在中新世中期以来受季风影响的森林演变过程中发生的各种植物-昆虫相互作用。我们评估了代表大吉岭下西瓦里克植物群(DLSF)的137个标本上的昆虫食草的多样性和频率。我们还检查了食草动物去除叶面积的百分比,作为对昆虫草食动物去除宿主植物光合组织的影响的独立度量。在这项研究中,确定了五个功能性进食组(FFG),即叶片采摘,孔洞进食,骨骼化,擦伤和边缘进食。这些痕迹表明昆虫出于各种目的与植物相互作用,包括进食,产卵和庇护。此外,这些形态示踪剂倾向于暗示昆虫与现存植物物种(例如Persea,Woodfordia,Shorea,面包果,Callicarpa,Albizia,紫薇等)的叶片相互作用时具有相似性。根据与现存类群的比较,可能的叶片饲养者可能属于昆虫命令直翅目,鞘翅目,鳞翅目和双翅目。尽管与化石叶子相关的食植物昆虫的形态尚不清楚,但目前的发现表明,中新世时期已经建立了许多现代植物与昆虫的关系,并一直延续至今,从而塑造了当今的动植物群。在本研究中,我们将DLSF上的昆虫食草与之前研究过的Arunachal较低的Siwalik植物区系和该地区的两个较年轻的植物区系进行了比较。我们注意到在这四个化石区系中观察到的FFG和损害类型的范围相似,并得出结论,与生物因子相比,气候对确定喜马拉雅东部地区植物与昆虫相互作用的演化影响很小。 (C)2015 Elsevier B.V.保留所有权利。

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