昆虫的口器

概述了口器的基本结构、基本类型（九个类型），每种类型口器的特点，适于取食的食物类型．具有该种口器的昆虫种类。还简介了口器与昆虫头部形式，口器类型与化学防治的关系。     

大气CO_2浓度升高对植物-植食性昆虫的作用机制

大气二氧化碳浓度升高及其伴随的全球变暖引起国内外科学家的极大关注。CO2浓度升高主要通过改变植物的初级和次级代谢产物,影响以之为食的昆虫。本文结合作者近年来的研究成果,着重于以CO2浓度升高为作用因子,以植物和植食性昆虫的相互关系为对象,比较了咀嚼式口器昆虫与刺吸式口器昆虫对大气CO2浓度升高的响应特征,分析了不同取食类型昆虫-植物对大气CO2浓度升高的响应机制。     

襀翅目化石稚虫口器及其食性分析

本文概述了现生襀翅目稚虫的食性,其通常分为腐食-植食性、肉食性和杂食性;食性不同,其口器结构差异明显.古生物学家根据化石保存的口器结构,利用将今论古、形态功能分析等手段推测襀翅目化石稚虫的食性有腐食-植食性、刮食性、肉食性,以及因化石保存等因素导致的食性不确定.此外,选取热河昆虫群中襀翅目昆虫的优势种类Perlidae的一代表化石稚虫,对其保存的口器形态及其食性的关系进行了分析,推断其食性为捕食性.     

伤害和挥发物对棉花花外蜜的诱导效应

植物花外蜜的分泌是一种植物间接防御反应。为了明确植食性昆虫、机械伤和机械伤诱导的挥发性气体在植物花外蜜诱导分泌中的作用,分析了咀嚼式口器昆虫棉铃虫Helicoverpa armigera(Hübner)、刺吸式口器昆虫棉蚜Aphis gossypii Glover取食、剪刀机械伤、剪刀机械伤+棉铃虫反吐物、针刺机械伤以及机械伤诱导挥发物、顺式-茉莉酮对棉花Gossypium hirsutum L.叶片花外蜜分泌量的影响。结果表明,棉铃虫取食、剪刀机械伤、剪刀机械伤+棉铃虫反吐物处理均显著增加了被处理叶片花外蜜的分泌量。棉花花外蜜的诱导效应在处理叶片上表现明显,并且在较幼嫩的第3片真叶上也有系统性增长。顺式-茉莉酮和机械伤挥发物处理1 d对棉花较幼嫩的第4、5片真叶花外蜜有诱导效应。棉花叶片花外蜜的诱导主要与植物组织损伤有关;不同口器类型的昆虫对棉花叶片花外蜜的诱导量不同,咀嚼式口器的棉铃虫对棉花花外蜜的诱导强度显著高于刺吸式口器的棉蚜;顺式-茉莉酮和机械伤诱导的挥发物能作为棉花植株间交流的信息物质诱导棉花幼嫩叶片花外蜜的分泌。     

植物与植食性昆虫相互作用的分子机制

在长期的协同进化中,植物建立起应对昆虫取食为害的精密而又复杂的防御机制,植物转录组调控中防御应答基因的表达及防御物质的合成因不同的昆虫取食方式而异。一般来说,咀嚼式口器昆虫取食时造成大面积组织伤害,可诱导植物产生伤害反应;而刺吸式口器昆虫因其特殊的口针取食,诱导植物激活病原体相关的防御途径。不同的防御途径激活不同的识别机制和信号途径。本文从信号识别和转导上综述了不同食性的昆虫取食植物时所引发的防御反应,分析了昆虫-植物相互作用关系的分子机制。     

刺吸式口器昆虫吸食量测定

<正> 就咀嚼式口器昆虫取食研究,由于其取食行为较为直观,经常采用称重法,直接测定昆虫某一龄期或整个一生的取食量。但刺吸式口器的昆虫,其取食对象是寄主的汁液,而且取食行为较为复杂,加上对昆虫人工饲料筛选的难度,尽管许多学者采用了许多方法,但还不能精确测定其吸食量。本文就刺吸式口器昆虫吸食量的研究方法作一概述。     

昆虫嘴巴趣谈

昆虫种类极多,已记载的现存种类达780,000种,化石种类约15,000种,约占已知动物种数的四分之三,广布于地面、土壤中、空中、水中,以及动植物体内和体表。昆虫食性较杂,它们的嘴巴也各有千秋。昆虫的嘴巴又称口器,基本上都由一片上唇、一片下唇、一对上颚、一对下颚和一个舌组成,但由于它们的食性复杂,取食的方法不同,因此口器的外形和结构有了多种变化,形成了不同类型的口器。     

转Bt基因棉花对刺吸式口器害虫种群的影响

综述了转Bt基因棉花对棉田刺吸式口器害虫的影响,并从棉田生态、棉花生理和昆虫生理等方面分析了转Bt基因棉田刺吸式口器害虫种群上升的原因.     

转历基因棉花对刺吸式口器害虫种群的影响

综述了转Bt基因棉花对棉田刺吸式口器害虫的影响,并从棉田生态、棉花生理和昆虫生理等方面分析了转Bt基因棉田刺吸式口器害虫种群上升的原因。     

中华蚊蝎蛉成虫口器感器的超微结构

口器感器在昆虫取食活动中起着重要作用, 但蚊蝎蛉成虫口器上感器的种类和形态迄今未见报道。我们利用扫描电子显微镜, 观察了中华蚊蝎蛉Bittacus sinensis Walker成虫口器上的感器。结果显示: 中华蚊蝎蛉口器上共有8种感器, 分别为锥形、毛形、刺形、指形、掌状、钟形、柱状感器及Böhm氏鬃毛, 主要集中于内唇、 下颚须以及下唇须上。锥形感器和刺形感器数量最多; 毛形感器主要在下颚轴节、 茎节和下唇的亚颏和前颏有分布; 钟形感器和Böhm氏鬃毛只存在于下唇须和下颚须上。下颚须端节和下唇须端节的感器种类相同, 以锥形感器为主。高度骨化的上颚以及下颚内颚叶与外颚叶上未发现感器分布。简要讨论了口器感器在昆虫分类中的意义。     

A new long-proboscid genus of Pseudopolycentropodidae (Mecoptera) from the Middle Jurassic of China and its plant-host specializations

We describe a new genus and species of Mecoptera with siphonate mouthparts, Sinopolycentropus rasnitsynigen. et sp. n., assigned to the family Pseudopolycentropodidae Handlirsch, 1925. The specimen was collected from late Middle Jurassic nonmarine strata of the Jiulongshan Formation in Inner Mongolia, northeastern China. The new material provides additional evidence for an early diversification of pseudopolycentropodids that was ongoing during the Middle Jurassic. This diversity also adds to the variety of known pseudopolycentropodids with tubular proboscides that apparently fed on ovulate fluids produced by Mesozoic gymnosperms.     

Late Triassic, Early and Middle Jurassic Radiolaria from ferromanganese-chert ‘nodules’ (Angelokastron, Argolis, Greece): evidence for prolonged radiolarite sedimentation in the Maliac-Vardar Ocean

In the Argolis, the Basal Sequence, constituting the eastern Pelagonian margin which bordered the Maliac-Vardar oceanic domain, includes shallow-water carbonates of Late Triassic-Early Jurassic, condensed pelagic limestones of Early-Middle Jurassic, radiolarian cherts of late Middle-Late Jurassic age and siliceous mudstones and sandstones rich in ophiolite fragments. Up-section, coarse breccias, including clasts of boninites derived from the ophiolite obducted onto the Pelagonian margin in Late Jurassic times crop out. Near Angelokastron a small quarry exposes pervasively sheared dark reddish-brown, radiolarian-bearing cherty shales with disrupted fragments of chert and chert nodules impregnated by ferro-manganese oxides. These shales occur in the footwall of a thrust bringing them into contact with the Pantokrator Limestone of the Basal Sequence. We collected more than 30 samples of the chert fragments and the shaly matrix. Thirteen nodules and one matrix sample yielded determinable radiolarians. Low to non-detectable concentrations of trace metals such as Co, Cr, Cu, Ni, Zn, and Pb indicate a hydrothermal origin of the ferro-manganese mineralization. The radiolarian taxa found indicate four age groups for the nodules that are embedded in the siliceous shale matrix that yielded a Middle Jurassic age (middle Bathonian). The first group includes a nodule of Late Triassic age (late Norian to Rhaetian); the second group nodules of Early Jurassic age (late early to late Pliensbachian and probably middle-late Toarcian); the third group nodules of early Middle Jurassic age (Aalenian–Bajocian); the last group finally includes nodules of late Middle Jurassic age (Bajocian–Bathonian). The presence of Upper Triassic to Middle Jurassic Mn-impregnated chert nodules in a Middle Jurassic matrix indicates a deep oceanic environment of deposition outside the Pelagonian realm (easternmost Adria Plate), which at that time was a shallow-water carbonate platform with a thin pelagic limestone cover. The chert nodules are with all certainty derived from the oceanic Maliac-Vardar domain and were, together with their host formation, tectonically emplaced onto the Pelagonian margin. We speculate that these nodules, more lithified than their matrix, were exhumed on the slope of an intra-oceanic accretionary wedge and were redeposited in the Middle Jurassic siliceous mudstones on the floor of the subducting Maliac-Vardar Ocean.     

Insect herbivory and plant defense on ginkgoalean and bennettitalean leaves of the Middle Jurassic Daohugou Flora from Northeast China and their paleoclimatic implications

Interactions between terrestrial arthropods and plants play a significant role in terrestrial ecosystems. Research on plant–insect interactions through geologic time provides valuable information for studying insect behavior and plant structure, understanding their coevolution, as well as analyzing climate change. In this paper, we choose fossil ginkgoalean and bennettitalean leaves as the plant hosts to study insect herbivory in the Middle Jurassic Daohugou area. Seven damage types of four functional feeding groups have been identified. Of the four functional feeding groups, margin feeding is the most common, indicating an abundance of insects with chewing mouthparts. Ginkgoalean leaves, probably because of their chemical defense, suffered less severe insect damage than bennettitalean leaves. Physical defense has also been observed in various genera of the bennettitalean leaves. Significantly, leaves of Anomozamites had a shaggy indumentum on the abaxial leaf surface and long stiff hairs along the rachis protecting them from insect herbivory. Our results indicate that the climate in the Middle Jurassic of the Daohugou area was relatively warm and humid. This work contributes to the study of plant–insect coevolution in the Daohugou Biota and provides more proxy data for understanding the Middle Jurassic paleoclimate and paleoenvironment in Daohugou area.     

Jurassic reef events in the Moroccan Atlas: A review

In the Moroccan Atlas, sedimentary deposits provide important data on reef events that characterize the Jurassic period. Recent work allows us to enhance knowledge of the Jurassic reefs in the Atlas, in particular their age, character and palaeogeographic distribution. Numerous localities with sponge-microbial mud mounds, coral reefs, and lithiotid bioherms are recorded from the Middle and High Atlas regions. These different biogenic constructions occupy different palaeogeographic settings: on the top of tilted blocks within the basin center; in slightly deeper positions, at the basin platform junction; and on adjacent platforms in the middle of the coastal area. The main episodes of reef building span nearly 30 million years, as follows: (1) Sinemurian, (2) early Pliensbachian, (3) late Toarcian, (4) Aalenian–early Bajocian (pars), and (5) late Bajocian. These five distinct reef events can be linked with general fluctuations of sea level and tectonism, and have palaeoclimatic implications.     

The morphology of mouthparts,wings and genitalia of Paleozoic insect families Protohymenidae and Scytohymenidae reveals new details and supposed function

Megasecoptera is an extinct group of insects with specialized rostrum-like mouthparts, which is a synapomorphy shared with all members of the Late Paleozoic Palaeodictyopterida, and markedly slender wings that are unable to flex backwards. Here we describe the close up morphology of Protohymenidae and Scytohymenidae and uncover new aspects of the endoskeleton (tentorium) of the head, structure of the mouthparts with discernible proximal part of stylets controlled by muscles, surface of compound eyes that consist of a hexagonal pattern of large facets, structure and microstructures on the wings and reconstruct male and female external genitalia using ESEM and light stereomicroscopy. Furthermore, we describe Protohymen novokshonovi sp. n. based on an exceptionally well preserved fossil from the early Permian at Tshekarda in Russia, which shows crucial details, and the earliest species of Protohymenidae, Carbohymen testai gen. et sp. n. from a late Carboniferous siderite nodule at Mazon Creek in Illinois, USA. Our comparative study confirmed a set of structural and microstructural details on their wings, such as the composite anterior wing margin, development of an apical cell and the previously unknown external genitalia. Based on the results and comparison of homologous structures known primarily for extant relatives, such as mayflies and dragonflies, we outline for the first time the function of the mouthparts, in particular, the stylets, structure of the tentorium, vision provided by large hexagonal ommatidia and male copulatory structures bearing curved claspers for holding a female during copulation and penial lobes with seminal grooves.     

Middle Jurassic Spore- pollen Assemblages from Turpan- Shanshan Area,Xinjiang

The Middle Jurassic palynoflora from the two wells of PUl and CN1 of Turpan-Shanshan area in Xinjiang consists of 97 species of fossil spores and pollen grains referred to 45 genera, of which 2 species are newly described. Three palynological assemblages including: 1) Cyathidites-Cycadopites-Quadraeculina (CCQ), 2) Cyathidites-Classopollis-Picites (CCP) and 3 ) Granu-latisporites-Classopollis-Podocarpidites (GCP) assemblages are established in the Xishanyao, Sanjianfang and Qiketai Formations, respectively. Comparisons have been made between these assemblages with those of the adjacent regions in Xinjiang and other domestic areas and at abroad. The geological age of the CCQ assemblage is suggested to be at early Middle Jurassic (corresponding to Aalenian to Bajocian age); while the CCP and GCP assemblages are considered to be at late Middle Jurassic (corresponding to early to late Bathonian age, respectively).     

新疆吐鲁番—鄯善地区中侏罗世孢粉组合

研究新疆吐鲁番鄯善地区葡１井和草南１井中侏罗世孢子花粉化石４５属９７种,包括２个新种。建立西山窑组、三间房组和七克台组共３个孢粉组合,其地质时代相当于中侏罗世早期和晚期。     

Fossil coniferous wood from the Middle Jurassic of Liaoning Province, China

Silicified coniferous wood was collected from the Lanqi Formation (late Middle Jurassic in age) at Shebudaigou Village, Liaoning Province, China. Three taxa are identified, namely Pinoxylon dacotense Knowlton, Xenoxylon phyllocladoides Gothan, and Araucariopitys sp. Based on these new data, and those of other fossil plants reported previously from the same formation, we consider the climate during the deposition of the Lanqi Formation was subtropical, humid and seasonal. In this respect the Lanqi flora differs from the coeval Shimengou and Longmen floras from North China. The Longmen flora was deposited during more humid, subtropical conditions, while the Shimengou Formation indicates that the climate was warm temperate and dry. Our data would suggest that the Late Jurassic climatic pattern was initiated as early as the late Middle Jurassic.     

A new species of glypheid lobster,Glyphea pisuergae (Crustacea,Glypheoidea), from the Early Jurassic of Palencia,Basque-Cantabrian Basin,Spain

A new glypheid lobster (Crustacea, Glypheidae), Glyphea pisuergae sp. nov. is described from the Early Jurassic (late Pliensbachian–early Toarcian) of Salinas de Pisuerga, Palencia, Spain. This species represents the second record for the genus in the Early Jurassic.