狭胸天牛分类地位初步研究（鞘翅目：天牛总科）

天牛类幼虫特征是探讨天牛总科演化和分类系统的重要依据。长期以来由于未找到狭胸天牛幼虫,其地位难以确定,影响到天牛总科分类系统的重建。近年来,在中国广西和西藏发现的猜胸天牛Philus antennatus (Gyllenhal）和细点音天牛Het-erophilus punctulatus Ching et Chen幼虫,为研究猜胸天牛分类地位提供了新的证据。综合比较认为,猜胸天牛与暗天牛科最相近,倾向于将狭胸天牛亚科归和暗天牛科。     

中国脊花天牛属一种（鞘翅目：天牛科）

记述中国花天牛亚科1新种－－裂跗脊花天牛Stenoconus schizotarsus,sp.nov.,模式标本存西南农业大学昆虫标本馆。     

祁连山刺脊天牛属一新种(鞘翅目：天牛科)

祁连山刺脊天牛属一新种（鞘翅目：天牛科）蒲富基（中国科学院动物研究所北京１０００８０）汪有奎李晓明（甘肃省祁连山国家级自然保护区管理局甘肃７３４００）１９９５－０５－２５收稿,１９９５－１２－２６收修改稿·８２·在１９９１～１９９４年祁连山自然保护区...     

中国花天牛亚科三新种记述（鞘翅目：天牛科）

训国花天牛亚科３新种－－黑角瘤花天牛Ｇａｕｒｏｔｉｎａ ｎｉｇｒｏａｎｔｅｎａｔａ,ｓｐ．ｎｏｖ．,青海皮花一在牛Ｒｈａｇｉｕｍ ｑｉｎｇｈａｉｅｎｓｉｓ,ｓｐ．ｎｏｖ．,四面山华花天牛Ｓｉｎｏｓｔｒａｎｇａｌｉｓｓｉｍｉａｎｓｈａｎａ,ｓｐ．ｎｏｖ．。模式标本存西南农业大学昆虫标本馆。     

狭胸天牛类雄性外生殖嚣分类研究——附一新种

该文就狭胸天牛类3属6种雄性外生殖器的形态结构,比较研究其系统发育及其归属,并记录太谷芫天牛Mantitheus tazguensts sp. nov.一新种和重新描述细点音天牛的雄性外生殖器。狭胸天牛类属较原始的类群,祖征为中茎突中央加厚,边缘极薄;阳基侧突基部还保留着一条横裂。狭胸天牛属与音天牛属和芫天牛属关系较密切,应为姊妹群,狭胸天牛属较始,其衍征为中茎突较长的分开,内囊具基骨片、骨化细长管和大小较一致骨化微刺。音天牛属和芫天牛属为姊妹群,芫天牛较原始,音天牛较进化,其衍征为阳基侧突背面因基部裂缝消失而完全合并,骨化细长管较细;外部形态表现为触角较短,较圆;中胸发音器中央无缝;而芫天牛内囊基骨片明显易见。     

中国花天牛亚科三新种记述：鞘翅目：天牛科

本文了中国花天牛亚科３新种－卵斑长颊瘦花牛Ｇｎａｔｈｏｓｔｒａｎｇａｌｉａ ｅｌｌｉｐｔｉｃａ,ｓｐ．ｎｏｖ。,暗背脊花天牛Ｓｔｅｎｏｃｏｒｕｓ ｆｕｓｃｏｄｏｒａｌｉｓ,ｓｐ．ｎｏｖ．,四斑短腿瘦花天牛Ｐｅｄｏｓｔｒａｎｇａｌｉａ ｑｕａｄｒｉｍａｃｕｌａｔａ,ｓｐ．ｎｏｖ。模式标本存西农业大学昆虫标本馆。     

中国两种狭胸天牛类幼虫的描述（鞘翅目：天牛总科）

天牛类的幼虫特征,已成为天牛总科探讨演化和分类系统的重要手段,狭胸天牛类由于长期以来未找到幼虫,其地位不能确定,影响到整个天牛科和天牛总科的演化和分类系统的研究存在一个缺口。近年在中国广西和西藏发现了松狭胸天牛ＰｈｉｌｕｓａｎｔｅｎｎａｔｕｓＧｙｌｌｅｎｈａｌ和细点音天牛ＨｅｔｅｒｏｐｈｉｌｕｓｐｕｎｃｔｕｌａｔｕｓＣｈｉａｎｇｅｔＣｈｅｎ的幼虫,前者王缉健（１９８９）和尹新明（１９９４）曾有简短报道。本文对这两种幼虫的形态作了详细描述,以供与近缘类群作比较研究。     

中国艳天牛属一新种：鞘翅目：天牛科：天牛亚科

中国艳天牛属一新种（鞘翅目：天牛科：天牛亚科）蒋书楠,陈力（西南农业大学植物保护系,四川省重庆市北碚６３０７１６）关键词天牛科,分类学,艳天牛属,新种天牛亚科艳天牛属ＡｃｒｏｃｙｒｔｉｄｕｓＪｏｒｄｏｎ的已知种类,可分为金色毛被种和银色毛被种两类。Ｊ...     

云南天牛科三新种记述：鞘翅目：天牛科

记述了采自云南的沟胫天牛亚科３新种：齿尾毡天牛Ｔｈｙｌａｃｕｓｄｅｎｔｉｐｅｎｎｉｓ、黑斑灰天牛Ｂｌｅｐｅｐｈａｅｕｓｎｉｇｒｏｓｔｉｇｍａ和云南刺锦天牛Ｓｔｅｒｎｏｈａｍｍｕｓｙｕｎｎａｎａ。其中,刺锦天牛属ＳｔｅｒｎｏｈａｍｍｕｓＢｒｅｕｎｉｎｇ为我国首次记载。新种模式标本保存于西南农业大学昆虫标本馆。     

虎天牛族中国六新纪录种(鞘翅目,天牛科,天牛亚科)

共记述了绿虎天牛属Chlorophorus Chevrolat中国1新纪录种,横纹绿虎天牛Chlorophorus copiosus Holzschuh;艳虎天牛属Rhaphuma Pascoe中国2新纪录种,回纹艳虎天牛Rhaphuma lanzhui Holzschuh和箭纹艳虎天牛Rhaphuma illicata Holzschuh;刺虎天牛属Demonax T homson中国3新纪录种,断纹刺虎天牛Demonax traudae Holzschuh,蔷薇刺虎天牛Demonax rosae Holzschuh和格氏刺虎天牛Demonax gertrudae Holzschuh。研究标本保存在西南大学昆虫标本馆。     

Notulae de Ranunculaceis sinensibus (ⅩⅩⅢ)

(1) In this paper, differences among the five genera constituting the tribe Cimi cifugeae of the family Ranunculaceae are discussed. Beesia, the first genus, with compound cymes and flowers bearing neither petals nor staminodes, is different from the other four genera with simple or compound racemes and flowers bearing either petals or staminodes, and may occupy a primitive position within the tribe. As to the other four genera, Souliea is characterized by the stem without basal leaf but with 2～5 sheath-like cataphylls, the sepals being deciduous but not caducous, moderate in size and petaloid, the petals being much smaller than sepals, but pink in color and more or less petaloid, the pollen grains being pan tocolpate or pantoporate, the carpels being 1～3 per flower, when mature forming dry linear follicles conspicuously reticulate on the surface and dehiscent along the ventral suture, and the seeds being reticulate-foveolate on the surface. These diagnostic characters indicate clear ly that Souliea might have deviated from the lineage formed by the next three genera, i. e. Anemopsis, Cimicifuga, and Actaea, which have their own well-recognizable diagnostic characters. Anemopsis is characterized by the normally developed basal leaf, the racemose inflorescence with sparse and few long pedicellate flowers, the sepals 7～10 in number, mod erate in size, and petaloid, the petals slightly smaller than sepals, the tricolpate pollen grains, the carpels 2～4 per flower, stalked, when mature forming dry oblong follicles with transverse veins on the surface, and the seeds with scaly membranous wings. Cimicifuga is distinguished by the normally developed basal leaf, the caducous, small, often sepaloid sepa ls, the organs of the second floral whorl sometimes with empty sterile anthers being stamin odes not petals, the tricolpate pollen grains, the carpels 1～8 per flower, when mature form ing dry oblong or ovoid follicles with transverse veins on the surface, and the seeds usually with scaly membranous wings. The last genus Actaea is different by the basal leaf trans formed into a small scale, the caducous, small, often sepaloid sepals, the organs of the sec ond floral whorl being clawed petals, the pollen grains with 3(4～6) colpi, carpel 1 per flow er, when mature forming a fleshy indehiscent berry smooth on the surface and without any veins, the seeds roughish or slightly rugose, neither foveolate nor winged on the surface, and the advanced most asymmetric karyotype. According to the diagnostic characters given above, we believe that Beesia, Souliea, Anemopsis, Cimicifuga, and Actaea do represent five independent genera, and the treatment of the tribe Cimicifugeae including these five genera in it by Hutchinson (1923), Janchen (1949) and some other authors, has precisely shown the taxonomic diversity within the tribe. We are therefore unable to accept the treatment published by Compton et al. (1998) to lump the two genera, Souliea and Cimicifuga, into the genus Actaea. (2) Compton et al. (1998, 1997) found out that the Chinese plants previously identified by various authors as Cimicifuga foetida L., in which the terminal and lateral racemes of the compound raceme flower more or less simultaneously, differ from the true C. foetida L. in northern Asia, in which the terminal raceme of the compound raceme flowers before the lateral ones, and thus restored the species name Cimicifuga mairei Lévl. , which was formerly reduced to the synonymy of C. foetida L. , for the Chinese plants. After examining the specimens collected from Siberia and from Southwest China we failed to find out any other differences in both vegetative and reproductive organs between the plants of the two regions, and we consider that it is better to treat the populations in Southwest and Central China as a geographical variety of Cimicifuga foetida L. A new combination, Cimicifuga foetida L. var. mairei (Lévl.) W. T. Wang & Zh. Wang, is thus made. (3) 3 species of Delphinium, 1 species and 1 variety of Clematis are described as new.     

贵州罗甸纳水上石炭统(宾夕法尼亚亚系)地层的再研究

本文详细描述了贵州罗甸纳水上石炭统(宾夕法尼亚亚系)剖面的生物地层和年代地层,其牙形刺序列自上而下可详细划分为：Streptognathodus isolatus, S. wabaunsensis, S. tenuialveus, S. firmus, Idiognathodus nashuiensis , Streptognathodus simulator, S. guizhouensis , S. gracilis-S, excelsus , S. cancellosus , S. clavatulus , S. nodocarinatus , Idiognathodus podolskensis , Mesogondolella clarki -Idiognathodus robustus , Diplognathodus ophanus-D, ellesmerensis, Idiognathoides ouachitensis, Streptognathodus expansus, Idiognathoides sulcatus parva, Idiognathodus primulus-Neognathodus bassleri, Idiognathodus primulus-Neognathodus symmetricus, Neognathodus symmetricus, Idiognathoides corrugatus-I, pacificus, I. sinuatus, I. sulcatus sulcatus, Declinognathodus noduli ferus 和 Gnathodus bilineatus bollandensis 等带。 Declinognathodus noduliferus 和 Streptognathodus isolatus 的首次出现分别代表上石炭统(宾夕法尼亚亚系)和二叠系的开始。根据牙形刺和有孔虫的序列,罗甸纳水剖面的上石炭统(宾夕法尼亚亚系)地层自下而上可划分为罗苏阶(Luosuan)、滑石板阶(Huashibanian)、达拉阶(Dalaan)和马平阶(Mapingian),并可与俄罗斯的巴什基尔阶(Bashkirian)、莫斯科阶(Moscovian)、卡西莫夫阶(Kasimovian)和格舍尔阶(Gzhelian),北美的莫罗阶(Morrowan)、阿托克阶(Atokan)、得梅因阶(Desmoinesian)、密苏里阶(Missourian)和弗吉尔阶(Virgilian)进行对比。另外,本文也详细讨论了剖面中的石炭系中间界线及石炭-二叠系界线。     

Early Cretaceous Palynofloras from Tarim Basin,Xinjiang

One hundred and eight species of fossil spores and pollen referred to 55 genera found from the Lower Cretaceous Kapushaliang (Kizilsu) Group in the Tarim Basin of Xinjiang have been studied in this paper. The Kapushaliang Group may be divided into the Yageliemu Formation, the Shushanhe Formation and Baxigai Formation in ascending order. The Yageliemu palynoflora is characterized by the predominance of gymnospermous pollen, the relative abundance of pteridophytic spores and the absence of angiospermous pollen. Coniferae is dominant, while Lygodiaceae and Schizaeaceae are important in the flora. The most common species of palynomorphs are Todisporites minor, Cicatricosisporites dorogensis, C. australiensis, Lygodiumsporites subsimplex, Schizaeoisporites cretacius, S. zizyphinus, S. certus. Cibotiumspora paradoxa, Cyathidites australis, C. minor, Biretisporites potoniael, Cycadopites minimus, Pseudowalchia hiangulina, Parvisaccites radiatus, Podocarpidites multesimus, P. canadensis, Alisporites bilateralis, Cedripites cretaceus, C. canadenris, Abietineaepollenites microalatus, Clarsopollis classoides, C annulatus, C. xinjiangensis (sp. nov.), Ephedripites multicostatus, E. tarimensis (sp. nov.), etc . The palynoflora is comparable with those of the lower part of the Lower Xinminbu Formation in northwestern China and the lower part of the Lower Mannville Formation in western Canada, which is considered corresponding from Berriasian to Valanginian in age. The Shushanhe palynoflora is also characterized by dominance of gymnosperms and subdominance of pteridophyta. Some primitive angiospermons pollen grains are found in the upper part of the formation. In addition to the most common species of the above mentioned palynoflora, the important species in the present palynoflora comprise Cicatricosisporites potomacensis, C. orbiculatus, C. subrotundus, Concavissimisporites punctatus, C. verrucosus, C. globosus, lmpardecispora apiverrucata, Trilobosporites crassus, T. trioreticulosus, Pilosisporites verus, P. trichopapillosus, Klukisporites pseudoreticulatus, Verrucosisporites obscurilaesuratur, Converrucosisporites saskatchewanensis, Foraminisporis wonthaggiensis, Cingulatisporites valdensis, C. ruginosus, Jiaohepollis verus, Pityosporites constrictus, etc. More than 40 in dicative species of Early Cretaceous occur in the assemblage. The palynoflora compares clcsely with those of the middle part of the Lower Xinminbu Formation and the Quartz Sand Member of the Lower Mannville Formatton. It is suggested that the Shushanhe Formation should belong to Hauterivian of Barremian in age. The Baxigai palynoflora is basically similar to the Shushanhe palynoflora. But the palynoflora shows an obvious increase in abundance of lygodiaceous spores and angiospermous pollen accompanied by a great reduction of Classopollis and Ephedripltes. Most of the Early Cretaceous species occurring in the above mentioned palynofloras are present. In addition, some Cretaceous species recorded from Aptian and Albian Stages in Europe, North America and Australia, such as Trilobosporites tribotrys, T. trioreticulosus, Coptospora paradoxa, Camarozonosporites insignis, Crybelosporites punctatus, etc., appear in the assemblage. In comparison with the microfloras of the upper part of the Lower Xinminbu Formation, the Upper Mannville Formation and the lower part of the Lower Colorado Group, the Baxigai Forma- tion should be referred to Aptian to Albian in age. Judging from the palynofloras, the early Cretaceous palaeoclimate in the basin should belong to the arid or semi-arid type of the subtropic zone. However, from Barremtan through Albian the climatic conditions might appear relatively wet.     

Importance of biological and abiotic factors for geochemical cycling in a freshwater eutrophic lake

Here we report the results of a comprehensive biogeochemical monitoring of Rostherne Mere in 1998, including changes in dissolved oxygen, organic carbon and nitrogen, nitrate/nitrite, ammonia, Al, Na, S, K, Mg, Ca, Si, Fe, Mn, orthophosphate, particulate N & P, suspended solids, temperature, pH, chlorophyll-a and zooplankton. The results demonstrated the major influence of primary producers on the overall geochemical cycling of N, P and Si, and suggested that the significance of zooplankton might have been previously underestimated. For major anions and cations, however, the influence of biota on lake water concentrations appeared to be negligible, reflecting the fact that these chemicals were present far in excess of plankton requirements. Thus changes in concentrations of Ca, K, Na, Mg and S were rather limited and must have reflected changes in hydrological and meteorological parameters. K, however, demonstrated a transitional pattern, reflecting some influence of biological uptake. During the stratification period, the slow processes of bacterial decomposition in the hypolimnion gradually released chemicals contained in the materials accumulated in the bottom layer, remarkably increasing the concentrations of dissolved compounds of those elements present in amounts comparable with the pool stored in the sedimenting detritus (e.g. orthophosphate P, ammonia N, Si and DOC). The decomposition also resulted in a drop in the redox potential, followed by partial denitrification and chemical release from the sediments. The hypolimnion of the Mere was confirmed to remain at the stage of Mn release, characterised by accumulation of DOC, orthophosphates, ammonia and initial stages of denitrification. High levels of P released from the sediments during the stratification period suggest that the lake’s recovery after sewage diversion might be further delayed.     

Embryology of Swertia (Gentianaceae) relative to taxonomy

The embryological features of three species of Swertia ( s.l.) – S. erythrosticta , S. franchetiana , and S. tetraptera – were characterized, and the observations were used, together with previously gathered data on other species, to evaluate a recently proposed polyphyly, based on molecular data, of Swertia s.l. Comparisons of species within the genus showed that they have diversified embryologically, and there are significant between-species differences. Notable features that vary between species include the number of cell layers that form the anther locule wall, the construction of the wall of the mature anther, tapetum origin, the cell number in mature pollen grains, the structure of the fused margins of the two carpels, the ovule numbers in placental cross-sections, the shape of the mature embryo sac, the degree of ovule curvature, antipodal variation and the presence of a hypostase, and seed appendages. They share characters that are widely distributed in the tribe Gentianeae, such as a dicotyledonous type of anther wall formation, a glandular tapetum with uninucleate cells, simultaneous cytokinesis following the meiosis of the microsporocytes, tetrahedral microspore tetrads, superior, bicarpellary and unilocular ovaries, unitegmic and tenuinucellar ovules, Polygonum -type megagametophytes, progamous fertilization, nuclear endosperm, and Solanad-type embryogeny. The presence of variation in embryological characters amongst the species of Swertia s.l. strongly supports the view that Swertia s.l. is not a monophyletic group. Frasera is better separated from Swertia s.l. as an independent genus, and is only distantly related to Swertia s.s. judging from the numerous differences in embryology. Swertia tetraptera is very closely related to Halenia , as they show identical embryology.  © 2007 The Linnean Society of London, Botanical Journal of the Linnean Society , 2007, 155 , 383–400.     

小鼠基因组中的微卫星重复序列的数量、分布和密度

作者分析了老鼠基因组中各染色体及其内含子、外显子和基因间区上各种类型的微卫星(1-6个碱基的重复序列)的数量及其密度。SSR约占老鼠基因组的2.85%,其中46.2%存在于基因间区,4.75%存在于外显子,49.05%在内含子区域,即非编码区富含微卫星。微卫星的数量与染色体或基因区域的大小有关,但密度与染色体或基因区域的大小的关系并不十分密切。第4染色体的外显子区域中6种类型的SSR含量都比其它区域少。A,T,AC,AG,AT,AAC,AAG,AGG,AAAC,AAAG,AAAT,AACC,AAAAC,AAAAG,AAAAT,AAACC,AAAGG,AAGAG,AAAAAC,AAAAAG,AAAAAT,AAAGAG,ACACAT,ACAGAG,ACAGGC,ACATAT是老鼠基因组中主要的SSR类型,而一些5碱基重复单元的SSR在老鼠基因组的某一条甚至某几条染色体都不存在     

Patterns and processes of heterochrony in Mesozoic goniasterid sea-stars

Heterochronic processes are obvious in the most common family of Mesozoic asteroids, the Goniasteridae, whether studied from entire fossils or, as is more frequently the case, from isolated ossicles. When phylogeny is poorly known, comparison between species leads to such unsatisfactory interpretations as 'A is more paedomorphic than B' or 'C, compared with other species, has many peramorphic characters'. When the phylogeny is known, heterochronic trends appear amongst the lineages. The peramorphocline Metopaster parkinsoni - M. loirensis-M. trichilae-M. chilipora-M. hypertelicus is studied here from the Cenomanian to the Upper Campanian of France. Different morphological characters evolved at different speeds. Among each polymorphous population, some morphotypes foreshadowed the next step. Juveniles of one species look like the adults of one of the ascendants. The cline developed irrespective of the substrate, and proceeded together with a migration from the Anglo-Paris Basin to the Aquitanian Basin. Metopaster hunteri , during the Coniacian, and Metopaster meudonensis , during the Upper Campanian, both evolved from Metopaster parkinsoni by neoteny, and provide a good example of reiterated and canalized morphological evolution. Some non-heterochronic canalizations are described.     

Occluded Umbilicus In The Pinacitinae (Devonian) And Its Palaeoecological Implications

Eifelian (Middle Devonian) ammonoids of the Pinacitinae Hyatt, 1900 ( Exopinacites , Pinacites )with preserved shell structures from the eastern Anti–Atlas (Morocco) have revealed unusual morphological features. The Pinacitinae belong to the earliest ammonoids which closed their umbilici. As an approach to an interpretation of these structures, the representatives of the subfamily Pinacitinae ( Exopinacites singularis , Pinacites jugleri , P. eminens ) are compared with other ammonoids, e.g. Acrimeroceras , Araucanites , Clistoceras , Gaudryceras , Nathorstites , Prolobites , and Synpharciceras , which produced umbilical plugs and covers. Some of these are comparable in structure to Nautilus pompilius and N. belauensis . In contrast to all of these taxa, the lateral shell wall of the Pinacitinae reached the centre of the umbilicus and formed an umbilical lid. The umbilical shell wall rests on the umbilical lid of the previous whorl. This construction probably had the advantage that it improved the hydrodynamic properties of the conch, along with the oxyconic conch shape and the approximately horizontal orientation of the aperture.     

Comparative morphology of male reproductive systems in Mediterranean blennies (Blenniidae)

The male reproductive organs of 16 species of Mediterranean Blenniidae ( Aidablennius sphynx, Blennius ocellaris, Coryphoblennius galerita, Lipophrys adriaticus, L. canevae, L. dalmatinus, L. nigriceps, Parablennius gattorugine, P. incognitus, P. sanguinolentus, P. rouxi, P. tentacularis, P. zvonimiri, Paralipophrys trigloides, Salaria pavo and Scartella cristata ) consist of pairs of testes, testicular glands, spermatic ducts, and blind pouches. Three main types of accessory sex organs were found by comparing the external morphology of the male gonads. Differences between species were observed in the volume of the testicular gland in relation to the volume of the testis and in the size and length of the spermatic ducts, and blind pouches. The anatomy of the testicular glands of all species investigated do not differ. Each gland consists of ducts that appear to be tubules which terminate at the testis periphery on one side and at the spermatic duct on the other side. Contrary to previous claims, A. sphynx has no fat body in place of the testicular gland; the gland of this species was not distinguishable from that of the other species investigated. In the Lipophrys species, in P. trigloides , and in B. ocellaris , a transition zone between testis and testicular gland is present. The testicular blind pouches empty into the spermatic ducts, into the ureter, or separately on the genital papilla. In most species, the epithelium has no or low folds, while in S. pavo it possesses high folds that nearly fill the lumen of the blind pouches. The morphological results are discussed in connection with taxonomy, ecology, and behaviour of the fishes.     

Morphology of the gynoecium and systematic position of the Ochnaceae

The gynoecium is syncarpous in all Ochnaceae. In the Ochnoideae carpels are peltate with a conventional cross-zone bearing one ovule, or, in Lophira , a very broad cross-zone with an horizontal ovular row. In Ochna and Brackenridgea , the style is gynobasic, each carpel develops transmitting tissue on its morphologically dorsal surface, and this tissue lines a canal or originates a solid inner strand in each carpel at style level. The style is tubular, with an inner cuticle, and compound, each component with its own transmitting tissue. In Ouratea the style is solid with a single compound transmitting strand. In Lophira and Elvasia the transmitting tissue seems to be developed by the morphologically ventral carpellary surfaces. Ovules are unitegmic with a bivalent integument.
In the Sauvagesioideae carpels are peltate, but with ovules above the cross-zones, on margins of the symplicate zone. In Euthemis , there is one ovule on each side of, and close to, each cross-zone. The single stylar canal is bounded by the morphologically dorsal carpellary surfaces. In Sauvagesia ovules occur on both sides of the cross-zones but most of them are above on carpel margins, as are all ovules of Cespedesia. The stylar canal of Sauvagesia is bounded by the ventral carpel surfaces, three strips of the outer surface passing inside at the sutures and developing into transmitting tissue. The stylar canal of Cespedesia is bounded by the dorsal carpel surfaces. The gynoecium of Wallacea has two epeltate carpels with a laminar placentation, the carpel margins being displaced on to the topographically ventral carpel surfaces with a row of ovules along each margin. Ovules are bitegmic.
The Ochnoideae, which shows relationships with the Rutaceae, Meliaceae, Simaroubaceae and Hippocastanaceae, is more advanced than the Sauvagesioideae, which clearly belongs in the Violales. The Ochnaceae is to be placed in the Violales.