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中生代中叶昆虫在裸子植物上的虫瘿为早期采矿进化提供了缺失的环节。

Middle Jurassic insect mines on gymnosperms provide missing links to early mining evolution.

机构信息

Guangdong Key Laboratory of Animal Conservation and Resource Utilization, Guangdong Public Laboratory of Wild Animal Conservation and Utilization, Institute of Zoology, Guangdong Academy of Sciences, Guangzhou, 510260, China.

College of Life Science and Academy for Multidisciplinary Studies, Capital Normal University, Beijing, 100048, China.

出版信息

New Phytol. 2024 Jun;242(6):2803-2816. doi: 10.1111/nph.19517. Epub 2024 Jan 7.

DOI:10.1111/nph.19517
PMID:38184785
Abstract

We investigated the mining mode of insect feeding, involving larval consumption of a plant's internal tissues, from the Middle Jurassic (165 million years ago) Daohugou locality of Northeastern China. Documentation of mining from the Jurassic Period is virtually unknown, and results from this time interval would address mining evolution during the temporal gap of mine-seed plant diversifications from the previous Late Triassic to the subsequent Early Cretaceous. Plant fossils were examined with standard microscopic procedures for herbivory and used the standard functional feeding group-damage-type system of categorizing damage. All fossil mines were photographed and databased. We examined 2014 plant specimens, of which 27 occurrences on 14 specimens resulted in eight, new, mine damage types (DTs) present on six genera of bennettitalean, ginkgoalean, and pinalean gymnosperms. Three conclusions emerge from this study. First, these mid-Mesozoic mines are morphologically conservative and track plant host anatomical structure rather than plant phylogeny. Second, likely insect fabricators of these mines were three basal lineages of polyphagan beetles, four basal lineages of monotrysian moths, and a basal lineage tenthredinoid sawflies. Third, the nutrition hypothesis, indicating that miners had greater access to nutritious, inner tissues of new plant lineages, best explains mine evolution during the mid-Mesozoic.

摘要

我们调查了昆虫取食的采矿方式,涉及幼虫消耗植物的内部组织,这是从中侏罗世(1.65 亿年前)中国东北的道虎沟地区获得的。侏罗纪时期的采矿记录几乎是未知的,而这个时间间隔的结果将解决在从以前的晚三叠世到随后的早白垩世期间,在矿-种子植物多样化的时间间隔内采矿演化的问题。植物化石通过标准的微观程序进行了研究,以确定其是否受到了取食,并且还使用了标准的功能取食群体-损伤类型系统对损伤进行分类。所有的化石矿都进行了拍照并建立了数据库。我们检查了 2014 个植物标本,其中 14 个标本上有 27 个出现的情况,导致了 6 个柏科、银杏科和松柏科裸子植物属上出现了 8 种新的矿损伤类型。从这项研究中得出了三个结论。首先,这些中生代中期的矿在形态上是保守的,它们跟踪植物宿主的解剖结构,而不是植物的系统发育。其次,这些矿的可能的昆虫制造者是三种原始多食性甲虫、四种原始单孔类蛾和一种原始叶蜂类。第三,营养假说表明,矿工更容易获得新植物谱系的有营养的内部组织,这最好地解释了中生代中期的矿化演化。

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