共查询到20条相似文献,搜索用时 10 毫秒
1.
Julio M. Grandez-Rios;Walter S. de Araújo;Aarón Panduro-Bardales;Eurídice N. Honorio Coronado;Timothy R. Baker;Rodolfo Vásquez Martínez;Abel Monteagudo Mendoza;Roosevelt García-Villacorta;Gerardo Flores Llampazo;José Reyna Huaymacari;Valeria C. Maia; 《Biotropica》2024,56(3):e13312
Patterns of gall-inducing insect diversity tend to be influenced by both habitat-related and plant-related characteristics. We investigated the distribution patterns of galling insects in four vegetation types (terra firme forest, white-sand dry forest, white-sand wet forest and palm swamp forest) of the Peruvian Amazon to test if the insect gall diversity (1) differs among different types of vegetation and (2) depends on host plant richness. In total, we found 11,579 galls belonging to 249 insect gall morphotypes, distributed across 30 botanical families and 75 plant species. Among host plant families, Fabaceae showed the greatest richness of insect gall morphotypes. We found that galling species richness was lower in palm swamp forest than in white-sand forests, which can be explained by the lower richness of plants in this type of vegetation. However, we found no evidence of greater richness in xeric habitats (e.g., white-sand dry forest) than in more mesic vegetation (terra firme forest), contradicting the hypothesis of hygrothermal stress. We also found that plant species richness was positively influenced with the richness and abundance of galling species, regardless of vegetation type. Galling insect species composition differed significantly between vegetation types, similarly to the floristic composition. Our findings show that the diversity of galling insects in the tropical rainforests of Peruvian Amazon are mainly influenced by host plant composition and host plant richness. 相似文献
2.
生物化石群落在埋葬过程中普遍经历了均时作用的过程。正是这种作用导致了同一生态环境域,但不同时期生物组合相混合的结果。因此,这种化石群落可能为一个连续演化群落的不同阶段的混合体,也可能是环境连续演化过程中不同生态群落的混合组合,这样的化石组合所记录的古生物学信息非常复杂。因此,对化石累积过程中的均时作用的清晰了解,将非常有助于古生物群落的分类学、居群动力学、埋葬学、古生态学、演化古生物学,甚至地层学研究精度的提高。文章根据前人的研究,扼要介绍和讨论均时作用的概念、过程、程度、效应和判别,及受均时作用影响的化石组合的分类。 相似文献
3.
Palerasnitsynus ohlhoffigen. et sp. n. is described fromBurmese amber of late Albian (Lower Cretaceous) age. This is the first record of the family Psychomyiidae from Burmese amber, and the earliest fossil record of the family. The genus Palerasnitsynusgen. n. differs from all other known psychomyiid genera by the absence of fork III in the forewings. 相似文献
4.
Abstract: A new species of the genus Epiphaxum (family Lithotelestidae) is described and illustrated in detail, and compared to other species. Epiphaxum arbuscula sp. nov. has been collected from Upper Eocene (Priabonian), Upper Oligocene (Chattian) and Lower Miocene (Upper Burdigalian) deposits of the Aquitaine Basin, south-west France. Epiphaxum is a poorly documented genus but its fossil record extends back to the Late Cretaceous; it was previously known only from the Paleocene (Danian). Epiphaxum arbuscula differs from all others species of the genus in the form of its colony. In contrast to the creeping colonies of previously known species, it has branched colonies. It is very common at one Upper Oligocene outcrop from which an assemblage with submarine cave remains has been described. A close relationship between the three extant species (two from the Caribbean Sea and one from the Indo-West Pacific region) and the Paleogene species is also noted. These constitute a group that has not undergone any important morphological changes for the last 65 million years. 相似文献
5.
F. LIHOREAU†¶ J. BARRY‡ C. BLONDEL Y. CHAIMANEE§ J.-J. JAEGER M. BRUNET 《Palaeontology》2007,50(2):503-524
Abstract: New fossil remains of the anthracothere genus Merycopotamus Falconer and Cautley, are described. Most of them were discovered by the Harvard University and Geological Survey of Pakistan joint research project (Y-GSP) in the well-dated Middle and Late Miocene deposits of the Potwar Plateau in northern Pakistan. This new material led us to revise the systematics of the genus with the validation of three species, M. nanus Falconer ( M. pusillus Lydekker), M. dissimilis Falconer and Cautley, and M. medioximus Lihoreau et al. , and allowed us to determine precisely their chronological distributions in a continuous Neogene sequence. Other specimens reported from the late Miocene deposits of the Khorat Plateau in north-east Thailand by the Department of Mineral Resources are the first remains of Merycopotamus to have been discovered in that region and are attributed to M. medioximus . These discoveries indicate a wider geographical distribution of the genus in the early Late Miocene. Anatomical investigations highlight the evolution of Merycopotamus through the Miocene towards more amphibious habits. Palaeobiogeographical and palaeoecological information for Merycopotamus stress the role of the Himalayan orogenesis as a dispersal barrier and the impact of a major global regression event on the evolution of Indian Subcontinent faunas from the Middle Miocene to the Late Pliocene. 相似文献
6.
Lawrence J. Flynn Alisa J. Winkler Margarita Erbaeva Nadia Alexeeva Ulrike Anders Chiara Angelone Stanislav Čermák Florian A. Fladerer Brian Kraatz Luis A. Ruedas Irina Ruf Yukimitsu Tomida Kristof Veitschegger Zhaoqun Zhang 《Mammal Review》2014,44(3-4):164-176
- Although Lagomorpha (rabbits, hares and pikas) have a long evolutionary history in Eurasia and Africa, including primitive genera of Eurasia historically considered assignable at the family level to Leporidae, the predecessors of modern rabbits were absent throughout this vast region for most of the Miocene until late in that epoch. During the early and middle Miocene, crown group Leporidae differentiated in North America, then dispersed to northern Asia in the late Miocene around 8 Ma (million years before present) and afterward. They then spread widely and apparently rapidly throughout Eurasia, reaching South Asia by 7.4 Ma and penetrating Africa about 7 Ma.
- The apparently abrupt introduction of Leporidae is a striking late Miocene event that we call the Leporid Datum. Perceived in terms of biochrons, the Leporid Datum includes localities in Europe and western Asia of late MN11 (Mammifères Néogènes system) age and younger, and precedes by less than one million years the Bahean‐Baodean land mammal age boundary in China.
- The late Miocene spread of Leporidae throughout Eurasia was a successful invasion in terms of the numerous occurrences and abundant fossils preserved. Where dating is sufficiently robust, the Leporid Datum is late Miocene, nowhere certainly more than ~8 Ma.
- In contrast to this sudden and widespread invasion, rare older finds suggest two possible refinements to this scenario: stem lagomorphs close to modern Leporidae may have lingered into the middle Miocene of Eurasia, or an independent, unsuccessful leporid invasion from North America may have preceded the 8 Ma datum.
- The Leporid Datum marks an important palaeoecological event for the Old World and complements the significance of molecular dates for origins of modern genera.
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Much of Beringia was composed of graminoid (grass and sedge) dominated habitats during the Late-Pleistocene, yet the account of the actual gramioids that were present is relatively vague. The spatial and temporal variabilities of palaeoclimate, mega-fauna, archaeology, and vegetation interactions could be significantly enhanced with accounts of Beringian graminoids. Fossil graminoid foliage is well preserved in permafrost sediments from Beringia and is available for identification using the micro-morphologies of the leaf epidermis (cuticles), which are often consistent with taxonomic identity. We present a scanning electron microscope (SEM) guide to the leaf cuticles of 38 graminoid species shown to be, or suspected of being present in former Eastern Beringian habitats during marine isotope stages (MIS) 2 and 3 (∼ 56,000-12,000 cal. yrs BP). We examine whether modern specimens have sufficient cuticle variability to identify fossil foliage. We surveyed SEM images from herbarium specimens for 50 quantitative and qualitative features on both sides (adaxial and abaxial) of leaves, and entered these into an interactive key program (Delta Editor). Individual species were unique based on the combined presence of 2-4 cuticle features. Replicate samples (n = 5) of 10 species were integrated into a cluster analysis and visually compared using a dendrogram. Overall, fossils that match modern specimens with a Gower's similarity coefficient of 0.80 or higher can be considered a reliable identification match. Several fossil graminoid specimens were compared and identified with our reference collection. Cuticle identification appears to be a viable method for future macrofossil analysis in Beringia. 相似文献
9.
Louis H. TAYLOR 《古脊椎动物学报》2004,42(4):340-344
WilliamR .Downs,III,knownasDongWeilintomanyfriends,diedarelativelyyoungman (1 950~ 2 0 0 2 )attheheightofhiscareerinpaleontology .HiscareerbeganattheMuseumofNorthernArizonain 1 975.OneofhisearlytaskswasthepreparationofTriassiccynodontsfromAntarcticaforEdwinH .Colbert,thenCuratorEmeritusoftheAmericanMuseumofNaturalHistoryandCuratorofVertebratePaleontologyattheMuseumofNorthernArizona (ColbertandKitching ,1 977) .WillpreparedtheEarlyJurassicarmoredornithischianScutellosaurusforColbe… 相似文献
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Abstract: The quality of the Triassic–Jurassic bivalve fossil record in northwest Europe has been measured using the Simple Completeness Metric (SCM). The SCM has been applied to the fossil record of total bivalve diversity and to the records of different ecological guilds. The Westbury and Lilstock Formations record high SCM values for most ecological groups. The ‘Pre‐Planorbis Beds’ of the lower Lias Group, however, witness a precipitous decline in the completeness of most guilds and emigration of taxa due to localized marine anoxia is a likely cause. Neither variation in lithofacies, shell mineralogy, sedimentary rock outcrop area, nor sequence architecture can convincingly explain the observed patterns of completeness. Our SCM data reveal that the Early Jurassic fossil record of infaunal suspension‐feeding bivalves is significantly poorer than that of epifaunal bivalves. Any differences in the apparent Rhaetian extinction rates between these two guilds should therefore be viewed with caution. Analyses of selectivity during the Late Triassic mass extinction based on studies of global databases appear robust in light of our SCM data. Nevertheless, future investigations of the Triassic–Jurassic benthic marine ecosystem undertaken at a finer‐resolution, may need to account for the poor quality of the Early Jurassic fossil records of certain ecological guilds, such as the infaunal suspension‐feeding taxa. 相似文献
11.
Lufeng rhizomyid fossils collected by exeavation and underwater sieving of fossili-ferous sediments, are studied in this paper.<br>The specimen referable to Brachyrhizomys nagrii is a left lower dentition with M1—M3(V. 8126) . Length of M1-M3, is 11. 75 mm. Both size and characters (such as short M3 and an elongated mesolophid on M3 ) agree well with Siwalik specimens (Fig. 4).<br>The specimens identifiable to Brachyrhizomys ef. B. pilgrimi are a left dentary with M1—M3 (V8127. 1) , a right M3 (V8127. 2) and an I1 (V8127. 3) . This is a large species with heavy deep dentary (depth below M=15. 4 mm) and massive incisors. It also is the biggest one of three species of Lufeng Brachyrhizomys. An apparent trait is suppression of mure on Mo-3. The narrow connection may not be present in early wear. Length of M-Ms is 15. 6 mm and more closer to B. ef. pilgrimi than to B. pilg- rimi of Siwaliks in size (Fig. 5, A, B and C).<br>The third species is B. tetracharax to which the most of the rhizomyine fossils from Lufeng Ramapithecus locality belong. The materials include an incomplete skull and associated lower jaw (V8128. 1) , five maxilla fragments (V8128. 2—6) . fourteen lower jaws (V8128. 7-20) . Fifty five isolated upper and lower ehack teeth (V8128. 21-75) , eleven isolated upper and lower incisors (V8128. 76—86) . Unfortunately, the skull and assoeiated lower jaw are crushed and fiattened laterally (Fig. 6, A) . The portions of it preserved are the ear region of two sides, partial right palate and left zygoma、partial maxilla, premaxilla, temporal bone and nasal. The infraorbital foramina were damaged and the shape of their ventral slit ean not be observed. The dentary is deep. In general, the upper dentition is longer than the lower one. Average length of them is 12. 28 mm and 14. 30 mm respectively. It is undoubtedly to refer the specimens from Lufeng to B. tetracharar, although there is discrepaney between the dimensions of the cheek teeth of Lufeng and Siwalik. M' has four roots. Ma elongates transversely. There is a strong mesolophid on M2 and an evident mure on worn M2-3. M, extends longitudinally. These traits distinguish the specimens from the other speeies easily. The yariations of upper and lower eheek teeth manifested by differences of wear stage in size and pattern of occlusal surface are shown in Fig. 6.<br>In addition, two isolated cheek teeth are referred to Rhizomyidae indet. A right M' with four roots (V8129) possesses an antero-lingual flexus (Fig. 7) . Another right M5 with a root (V8130) has been well worn and only retained lingual reentrant and three enamel lakes on oeclusal surface (Fig. 8).<br>The best known record of rhizomyid evolution is doeumented in Siwaliks of Pakistan. It is considered to be a standard for comparison of fossil rhizomyids through. out the world especially Asia. Three species of Brachyrhizomys mentioned above have known temporal ranges in Pakistan and eoexisted for a short time at 8 Ma. So Lufeng hominoid fauna can be placed about 8 Ma or perhaps a bit later. 相似文献
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A. E. Weis 《Journal of evolutionary biology》1996,9(5):623-640
Standard quantitative genetic theory predicts that when a trait is exposed to selection, the between-generation change in the phenotypic mean, Δz?i, will be equal to the product of the trait's heritability and the selection differential, h2S. By extension, this theory implies that if a number of replicate populations are exposed to varying intensities of selection, the between-generation changes in means should covary with the selection differential applied. This relationship offers an opportunity for a statistical test to detect evolutionary change when selection is measured in replicate populations. If an evolutionary response to phenotypic selection occurs, the regression of over Si, where i indicates population, will have a positive slope. This statistical test was applied to data on the insect Eurosta solidaginis (Diptera: Tephritidae). The larvae of this fly induce galls on the stems of the host plant, Solidago altissima (Asteraceae). Previous work has shown that gall size is a heritable trait of the insect. Further, size-dependent attack on Eurosta larvae by parasitoids selects for larger gall size (Weis and Abrahamson, 1986). Long-term data on phenotypic selection in 16 populations across 5 generations were analyzed for selection response. Apparent upward evolutionary responses were seen in 2 of the 4 between-generation transitions. However, no response was seen when the analysis was applied to the cumulative change in gall size. Examination of the data suggested that some of the change in mean gall size was a developmental response to spatial and temporal variation in the environment. Non-linear developmental effects of environment, when combined with non-linear fitness functions, can induce a spurious selection response; these non-linear relationships can account for the apparent evolutionary change gall size found in the by-generation analysis. Thus, there is no reliable evidence for evolutionary change in Eurosta's gall size over the generations studied. Stasis of gall size in the face of ongoing selection may be due to counterbalancing selection on the gallmaker imposed by host plant resistance. 相似文献
14.
Ryu Nakata Naoko Yoshinaga Masayoshi Teraishi Yutaka Okumoto Alisa Huffaker Eric A. Schmelz 《Bioscience, biotechnology, and biochemistry》2018,82(8):1309-1315
To aid in the identification and quantification of biologically and agriculturally significant natural products, tandem mass spectrometry can provide accurate structural information with high selectivity and sensitivity. In this study, diagnostic fragmentation patterns of isoflavonoids were examined by liquid chromatography-ion trap-time of flight-mass spectrometry (LC-IT-TOF-MS). The fragmentation scheme for [M+H?2CO]+ ions derived from isoflavones and [M+H?B-ring?CO]+ ions derived from 5-hydroxyisoflavones, were investigated using different isotopically labeled isoflavones, specifically [1′,2′,3′,4′,5′,6′,2,3,4-13C9] and [2′,3′,5′,6′,2-D5] isoflavones. Specific isotopically labeled isoflavones were prepared through the biosynthetic incorporation of pharmacologically applied 13C- and D-labelled L-phenylalanine precursors in soybean plants following the application of insect elicitors. Using this approach, we empirically demonstrate that the [M+H?2CO]+ ion is generated by an intramolecular proton rearrangement during fragmentation. Furthermore, [M+H?B-ring?CO]+ ion is demonstrated to contain a C2H moiety derived from C-ring of 5-hydroxyisoflavones. A mechanistic understanding of characteristic isoflavone fragmentation patterns contributes to the efficacy and confidence in identifying related isoflavones by LC-MSn. 相似文献
15.
L. R. Gurley J. G. Valdez W. D. Spall B. F. Smith D. D. Gillette 《Journal of Protein Chemistry》1991,10(1):75-90
Proteins have been successfully extracted from the fossil vertebra of a 150-million-year-old sauropod dinosaur (Seismosaurus) recently excavated from the Morrison Formation of New Mexico. HCl and guanidine·HCl extracts of the fossil bone and its sandstone matrix were concentrated, demineralized, and resolved into a number of different protein fractions by reversed-phase high-performance liquid chromatography (HPLC). One of these fractions had the same retention time as collagen. Amino acid analysis (Pico-Tag method) of these fractions confirmed they were proteins. Comparison of the correlation coefficients of the amino acid analyses with that of collagen standards indicated that none of the fractions contained significant amounts of collagen. Similar HPLC profiles were obtained for the HCl extracts of fossil bone and its sandstone matrix suggesting they contained the same proteins. However, different HPLC profiles were obtained when these HCl extracts were dried and reextracted with guanidine·HCl. These different fractions represent proteins unique to the fossil and were not found in the sandstone matrix. These differences were confirmed by amino acid analysis. Such information on fossil bone proteins might provide useful knowledge concerning the evolution of skeletal molecules and the fossilization process. Similar information on the proteins from the geological matrix might provide useful fingerprints for reconstructing ancient environments and for assessing sedimentary rocks for fossil fuel exploration. 相似文献
16.
Richard H. Tedford 《古脊椎动物学报》1995,(4)
INTRODUCTIoNThedevelopmentoftheNeogenebiostratigraphyofChinawasoneoftheearliestgoalsoftheCenozoicResearchLaboratoryoftheGeologicalSurveyofChina,pre-decessoroftoday'sInstituteofVertebratePaleontologyandPaleoanthropologyaVPP).Therationaleforsuchstudies1iesintheuniversalobjectiveofestablishingthenatureandtempooffaunalchangeinaregionandinadjacentregionsthatarelinkedzoogeographically.Eventuallythedataareusedtoincorporatelocaleventsintotheglobalhistoryoffaunalchange.Besidesthisgoal,thereis… 相似文献
17.
粪化石(coprolite)是石化的动物粪便,而广义上粪化石(bromalite)是石化的动物消化物、排泄物和排出物的总称。作为一类重要遗迹化石,粪化石蕴含了大量实体化石难以提供的生物学信息,为古生态学研究提供以下依据:1)粪化石作为媒介帮助理解远古动物的行为习性、消化系统的结构和功能、食谱特征以及古生态系统食物链/食物网;2)粪化石中保存的古寄生虫线索能有效地解读古生物寄生关系和某些常见肠道寄生虫的起源问题;3)新生代以来古人类粪化石证据可以直接解开早期古人类的食谱、疾病特征及其迁移路径;4)中、新生代以来的粪化石中保存的植物残留信息(孢粉化石和植硅体)是重建古植被面貌、恢复古气候和探索早期动植物关系的重要依据。本文回顾了粪化石研究历史,并针对粪化石在上述古生态各研究方向的最新进展进行了系统总结和综述,认为粪化石可有效解读古生态。文章最后对粪化石的最新研究技术方法(如CT扫描技术)及未来发展方向进行了展望。 相似文献
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L. B. BRATTSTEN J. H. SAMUELIAN K. Y. LONG S. A. KINCAID C. K. EVANS 《Ecological Entomology》1983,8(2):125-132
ABSTRACT.
- 1 All instars of Spodoptera eridania larvae grow as well or better when cyanide is present in their diet as when it is absent. Concentrations up to 0.05% stimulate feeding in first to fourth instar larvae. Concentrations from 0.1% to 1.0% stimulate feeding in fifth and sixth instar larvae.
- 2 Three-day-old sixth instar larvae pre-exposed to cyanide are completely resistant to its acutely toxic effects, but previously unexposed larvae suffer reversible symptoms of poisoning when feeding on a diet containing 1.0% KCN.
- 3 A 1.0% dietary KCN exposure during the sixth instar reduces ecdysis to 17% adult emergence and completely inhibits oviposition.
- 4 Cyanide concentrations from 0.5% to 1.0% in the diet, although effecting increased growth rates, induce necrotic lesions in larval mid-gut epithelial cells.
- 5 Thiocyanate, one of the in vivo cyanide metabolites, at 0.5% in the diet reduces pupation to 23%, delays and reduces adult emergence to 20% and inhibits oviposition.
- 6 The preferred host plant of S.eridania is the lima bean, Phaseolus lunatus, probably due to its content of the cyanogenic glycoside linamarin. Dietary valine has no effect on the southern armyworm feeding and growth behaviour (Long & Brattsten, 1982) but dietary cyanide does. The lima bean is known to contain up to 31 ppm cyanide in some varieties.
20.
Integrated palaeoecological evidence for biodiversity at the floodplain-forest margin 总被引:2,自引:0,他引:2
This paper presents the results of a combined palynological and palaeoentomological investigation into the changing diversity of Holocene floodplain forest biota at Bole Ings in the lower reaches of the River Trent. The aim in combining the two techniques represents an attempt to overcome some of the inherent differences of scale and resolution which characterize different types of fossil species data. The two lines of ecofactual evidence, pollen and beetle remains indicate changes in the biodiversity of the floodplain, both in terms of the diversity and abundance of individual species, habitats and ecosystem structure. The results of the study demonstrate the potential of this approach in tracing the decline in plant and entomofaunal diversity at the floodplain forest margin. Although there are recognized limitations imposed by taphonomic uncertainties, taxonomic resolution and restricted ecological data, the combined results provide added details of variations in both species composition and structural diversity within the landscape. The results emphasize the need for multidisciplinary research design in palaeoecological investigations of biodiversity. 相似文献

