On the Fossil Proteaceous Pollen in China

In this paper, some results of the study on the Proteaceous pollen collected recently in China are reported. On the basis of their different evolutionary features in geological history, their evolution is subdivided four stages in the Late Cretaceous—Early Tertiary, namely Cenomanian-Turonian, Senonian-Danian, Paleocene-Eocene and Oligocene. Each of the stages is typified by its own representative elements of Pro- teaceous and a certain domain of their predominance. According to the geographical distribution of Proteaceous pollen in China, four predominant districts are recognized, i.e. Northeast district of Late Cretaceous, Northwest-North-Inner Mongolia district of Early Tertiary, Centrial district of Late Cretaceous and Early Tertiary and South district of Early Tertiary. In addition, the problems concerning the stratigraphical, palaeoecological and pa- laeoelimatic significances of the Proteaceous pollen, and its origin are discussed in this paper too. Three new species are discribed here and they are: Proteacidites partitus sp. nov., P. tenellus sp. nov., P. bullatus sp. nov.     

Interplate dispersal paths for megathermal angiosperms

The dispersal of megathermal angiosperms between tectonic plates is reviewed on the basis of fossil evidence for the Cretaceous and Tertiary periods, since the radiation of the angiosperms, and the period of break-up of Gondwana. The combination of tectonic plate disassembly and redistribution, coupled with phases of global warming followed by pronounced cooling, has resulted in the formation of intermittent dispersal opportunities for frost-intolerant plants, and has been a major factor in determining the direction of angiosperm diversification. The Early Cretaceous radiation of angiosperms seems to show little relationship to the formation of Tethys. However, for the Late Cretaceous and Tertiary nine relevant dispersal routes can be differentiated that can be divided into two distinct categories: routes which formed following the break-up of Gondwana during the Late Cretaceous and Earlier Tertiary, when warm climates encouraged dispersal of megathermal elements globally, and routes which formed since the Middle Eocene, following phases of plate collision, as global climates were cooling down, inhibiting such dispersal. Most inter-plate dispersal of megathermal angiosperms took place in the Late Cretaceous and Early Tertiary at a time when global climates were markedly different from those of today, and the global area of megathermal vegetation several times greater than at present. Under such a scenario, it is likely than opportunities for speciation were much higher than for present-day megathermal plants.     

大果榕亚组三种榕树传粉榕小蜂核型研究

研究了木瓜榕(Ficus auriculata Loureiro)、苹果榕(F.oligodon Miquel)及未知榕(Ficus sp.)3种榕树传粉榕小蜂的核型。结果表明:3种榕树对应的传粉榕小蜂具有非常相似的核型,染色体数目相同为2n=10,染色体全部为中着丝粒染色体;核型公式2n=2X=10=10M,核型均为Stebbins-1A型。以臂比不对称性系数Dc和相对长度不对称性系数Dt作二维散点图,Ceratosolen emarginatus Mayr(木瓜榕传粉榕小蜂)和C.emarginatus Mayr(苹果榕传粉榕小蜂)具有非常相近的核型不对称系数,核型不对称性大于Ceratosolen sp.(未知榕传粉榕小蜂),显示出两者更近的亲缘关系,而Ceratosolen sp.(未知榕)与前两者亲缘关系较远。此外,比较了Ceratosolen属和Blastophaga属在核型方面的差异,认为染色体数目包括染色体形态能够作为准确区分Ceratosolen属和Blastophaga属的依据,并对Ceratosolen属的核型进化进行了初步探讨。     

Phylogeny of the World Anthophorini (Hymenoptera: Apoidea: Apidae)

Abstract.  The phylogenetic relationships of members of the long-tongued bee tribe Anthophorini were investigated. Twenty-six ingroup taxa, representing all known genera and the most common subgenera of the Anthophorini, were included in a cladistic analysis of the tribe based on 51 morphological characters. The analysis yielded the generic relationships: (( Habrophorula , Elaphropoda ) ( Habropoda ( Deltoptila ( Pachymelus ( Amegilla , Anthophora ))))). The monophyly of the Anthophorini and each of its genera was confirmed. A second tribe, Habropodini, as postulated by some authors, is paraphyletic. On the basis of the results of the cladistic analysis and the biogeographical data of Anthophorini, an evolutionary scenario is postulated in which all genera of Anthophorini probably evolved in the Late Cretaceous, except Amegilla and Anthophora , which originated in the Oligocene. The northern part of south-east Asia (India to south-east China) is regarded as the most probable place of origin and radiation of the Anthophorini. The New World was probably colonized three times independently by Habropoda (upper Cretaceous to Tertiary), by an ancestral lineage of Deltoptila (upper Cretaceous to Tertiary) and by Anthophora (Tertiary to Quaternary).     

Fossil angiosperm wood: its role in the reconstruction of biodiversity and palaeoenvironment

Fossil wood is subject to different taphonomic, sampling and recognition biases in the palaeobotanical record when compared with leaves and palynomorphs. Wood therefore provides a systematically independent source of information that can increase our knowledge of past biodiversity and environments. Increase in fossil wood records from Cretaceous and Tertiary sediments helps further the understanding of trends in anatomical specialization through geological time. These data can then be used to distinguish such specialization from anatomical response to environmental change. Two case studies, a Late Cretaceous early Tertian' wood flora from Antarctica and a lower Tertiary w ood flora from southern England, have been used to exemplify the importance of studying the fossil wood component of palaeofloras.     

The Cretaceous and Tertiary Aquilapolles in China

The Aquilapolles are found in Northeast and Eastern part of China. 183 speices are selected from the world. These 183 speices include Aquilapollenites, Mancicorpus, Fibulapollis and Translucentipollis. It is showed that they appeared from Albian of Early Cretaceous to Early Oligocene(?) of Tertiary. They mainly appeared in Senonian. The Aquilapolles are the most flourishing in Cretaceous during Maestrichtian. Tile six speices of which appeared in Tertiary. They are Aquilapollenites granobaculus, A. punctatus, A. quadrilobus, A. spinulosus, Funk., A. spinulosus (Mtched.) n. corab. and Fibulapollis mirificus. There are two phytogeoprovinces of the sporo-pollen in the Northern Hemisphere during Late Cretaceous. One is "Aquilapolles District "-moist subtropical climatic, Circum-Pacific and Siberia. Another is “Normapolles District”-arid (or semiarid) sub- tropical climatic, Circum-Atlantic, Europ and India. The author related the process to form the two phytogeopovinees by distribution of continent and sea in that time. In one country, Tertiary Aquilapollenites is wider than Late Cretaceous Aquilapollenites in palaeogeographic range. The Tertiary speices of Aquilapollenites are Aquila-pollenites spinulosus Funk. and A. granobaculus Song in China. Their kinds, amount and distribution fully show an evidence of relict member. They are relict Aquilapollenires and are not recycled fossils .from Upper Cretaceous strata. On Aquilapollenites, the respective characters of the growth and distribution of each Tertiary Epochs are indicated. The author also explores the relations between the growth, distribution and evolution of paleoenvironment in this paper.     

Quantitative Analysis of the Timing of the Origin and Diversification of Extant Placental Orders

Fossil evidence is consistent with origination and diversification of extant placental orders in the early Tertiary (Explosive Model), and with the possibility of some orders having stem taxa extending into the Cretaceous (Long Fuse Model). Fossil evidence that 15 of 18 extant placental orders appeared and began diversification in the first 16 m.y. of the Cenozoic is, however, at odds with molecular studies arguing some orders diversified up to 40 m.y. earlier in the Early Cretaceous (Short Fuse Model). The quality of the fossil record was assessed by tabulating localities of all mammals in the last 105 m.y. Global locality data (except Africa) for 105 m.y. of eutherian evolution indicate discernible biogeographic patterns by the last 15 m.y. of the Cretaceous. Eutherian genera increase from 11 in latest Cretaceous to 139 in earliest Tertiary, although both are represented by about 50 localities. Yet even in the Late Cretaceous of North America and Asia where eutherians are abundant, none of the 18 extant orders are definitely known. A series of Monte Carlo simulations test whether the rapid appearance of most mammalian orders is statistically significant, and if so, whether it is a radiation event or an artifact of a limited fossil record. Monte Carlo tests affirm that the clustering of appearances in the early Cenozoic is statistically significant. Quantitative analysis of the locality data suggests that the number of genera described is a function of the number of localities sampled. In contrast, the number of orders is not a simple function of localities and thus does not appear to be limited by localities. A second set of Monte Carlo simulations confirms that the increase in orders cannot be explained by the limited number of localities sampled. Even for best-fit simulations, the observed pattern of ordinal appearances is steeper than expected under a variety of null models. These quantitative analyses of the fossil record demonstrate that the rapid ordinal appearances cannot be ascribed to limited Late Cretaceous sample sizes; thus, early Tertiary ordinal diversification is real. Although the fossil record is incomplete, it appears adequate to reject the hypothesis that orders of placentals began to diversify before the K/T boundary.     

Review of the monotreme fossil record and comparison of palaeontological and molecular data

Monotremes have traditionally been considered a remnant group of mammals descended from archaic Mesozoic stock, surviving to the present day on the relatively isolated Australian continent. Challenges to this orthodoxy have been spurred by discoveries of 'advanced' Cretaceous monotremes (Steropodon galmani, Archer, M., et al., 1985. First Mesozoic mammal from Australia-an Early Cretaceous monotreme, Nature. 318, 363-366) as well as by results from molecular data linking monotremes to therian mammals (specifically to marsupials in some studies). This paper reviews the monotreme fossil record and briefly discusses significant new information from additional Cretaceous Australian material. Mesozoic monotremes (including S. galmani) were a diverse group as evidenced by new material from the Early Cretaceous of New South Wales and Victoria currently under study. Although most of these new finds are edentulous jaws (limiting dental comparisons and determination of dietary niches), a range of sizes and forms has been determined. Some of these Cretaceous jaws exhibit archaic features-in particular evidence for the presence of a splenial bone in S. galmani-not seen in therian mammals or in post-Mesozoic (Tertiary and Quaternary) monotreme taxa. Tertiary monotremes were either archaic ornithorhynchids (toothed platypuses in the genera Monotrematum and Obdurodon) or tachyglossids (large echidnas in the genera Megalibgwilia and Zaglossus). Quaternary ornithorhynchid material is referable to the sole living platypus species Ornithorhynchus anatinus. Quaternary echidnas, however, were moderately diverse and several forms are known (Megalibgwilia species; 'Zaglossus' hacketti; Zaglossus species and Tachyglossus aculeatus).     

Nymphalid butterflies diversify following near demise at the Cretaceous/Tertiary boundary

The butterfly family Nymphalidae contains some of the most important non-drosophilid insect model systems for evolutionary and ecological studies, yet the evolutionary history of the group has remained shrouded in mystery. We have inferred a robust phylogenetic hypothesis based on sequences of 10 genes and 235 morphological characters for exemplars of 400 of the 540 valid nymphalid genera representing all major lineages of the family. By dating the branching events, we infer that Nymphalidae originated in the Cretaceous at 90 Ma, but that the ancestors of 10–12 lineages survived the end-Cretaceous catastrophe in the Neotropical and Oriental regions. Patterns of diversification suggest extinction of lineages at the Cretaceous/Tertiary boundary (65 Ma) and subsequent elevated speciation rates in the Tertiary.     

Concentration and composition of dissolved organic carbon in streams in relation to catchment soil properties

Two adjacent catchments in the Otway Ranges of Victoria, Australia (Redwater and Clearwater) produce water with markedly different concentrations of dissolved organic carbon (DOC) during summer. Water from Redwater Creek had a DOC concentration of 32 mg L^–1, while water from Clearwater Creek had a DOC concentration of 3.8 mg L^–1. Examination of the catchments revealed that while climate, topography, vegetation and land use were similar, the soils were different. The objective of this study was to examine the relationship between the concentration and chemical composition of DOC in stream waters and the nature of soils in the two catchments. Soil mapping determined that clayey soils formed on Cretaceous sediments (Cretaceous soils) occurred throughout both catchments, but that Redwater Catchment also contained a large area (39%) of sandy soils formed on Tertiary sediments (Tertiary soils). The concentration of DOC in forest floor leachate was high in both the Tertiary and Cretaceous areas; however, the concentration of DOC in water draining areas dominated by Tertiary soils was greater than that in water draining areas dominated by Cretaceous soils. Laboratory experiments showed that the Cretaceous soils had higher adsorption capacities for forest floor leachate DOC than the Tertiary soils. The difference in DOC concentrations of the streams was therefore attributed to the difference in adsorption capacity of catchment soils for DOC. Adsorption capacities of the soils were found to be a function of their clay contents and specific surface areas.Solid-state³C nuclear magnetic resonance spectroscopy and pyrolysis-mass spectrometry were used to determine the chemical structure of DOC found in streams and forest floor leachate samples and that remaining in solution after interaction with soil. Chemistry of DOC in forest floor leachate was similar before and after interaction with soil, indicating no preferential adsorption of a particular type of carbon. Thus, differences between the chemical structure of stream DOC and forest floor leachate DOC could be attributed to microbial modifications during its movement through soils and into the streams, rather than losses by adsorption.     

Seed Size, Fruit Size, and Dispersal Systems in Angiosperms from the Early Cretaceous to the Late Tertiary

Fossil data from 25 angiosperm floras from the Early Cretaceous ( approximately 124 million years ago) to the Pliocene ( approximately 2 million years ago) were compiled to estimate sizes of seeds and fruits and the relative proportion of two different seed-dispersal systems by animals and by wind. The results suggest that, first, seed and fruit sizes were generally small during most of the Cretaceous, in agreement with previous suggestions, but the trend of increasing sizes started before the Cretaceous-Tertiary boundary; second, there was a decrease in both seed and fruit sizes during late Eocene and Oligocene, reaching a level that has continued to the Late Tertiary; third, the fraction of animal dispersal was, in contrast to previous suggestions, rather high also during the Cretaceous but increased drastically in the Early Tertiary and declined congruently with the declining seed and fruit sizes from the late Eocene; and fourth, the fraction of wind dispersal showed a bimodal pattern, being high in the Late Cretaceous and in the Oligocene-Miocene but with a drop in between. We find that the observed trends are only weakly related to the availability of animal fruit dispersers. Instead, the trends are congruent with a climate-driven change in environmental conditions for recruitment, where larger seeds are favored by closed forest vegetation. The prevalence of semiopen, dry, and probably herbivore-disturbed vegetation during the Cretaceous, the development of closed multistratal forests in the Eocene, and the later development of a more open vegetation and grasslands starting in the Oligocene-Miocene, are reflected in the distribution of angiosperm seed and fruit sizes and in the dispersal systems.     

Paleocene reefs on the Maiella Platform Margin, Italy: An example of the effects of the cretaceous/tertiary boundary events on reefs and carbonate platforms

Summary Reef facies, reef types and their biotic associations in the Maiella platform margin (central Italy) provide qualitative evidence for a significant reef decline across the Cretaceous/Tertiary (K/T) boundary, and indicate two phases of reef recovery during the Paleocene. Rudists dominated the reef community until the latest Cretaceous. A significant sea-level fall around the time of the K/T boundary is documented by a truncation surface associated with emersion. During sea-level highstands in the Danian to Early Thanetian and, more extensively, during the Late Thanetian, coral-algal patch-reefs grew along the platform margin and top. Already in the Danian to Early Thanetian, the reef communities were more diverse and the constructional types more evolved than previously known from this time. Differences between the Danian to Early Thanetian coral association, the Late Thanetian association, and Late Cretaceous coral faunas may have ecological or evolutionary causes. Repeated emergence produced a complex diagenetic history in the Danian to Lower Thanetian limestones. All Paleocene reefs were displaced by gravitative redeposition. Coral-algal reefs are less important in the Early to mid Eocene, when alveolinid foraminifera dominated on the Maiella shelf. Reefs on the Maiella platform diversified and attained large sizes in the Late Eocene to Early Oligocene, as known from other Mediterranean platforms. The external controls on the Late Cretaceous to Oligocene evolution and demise of reef communities that are most easily demonstrated with our data are sealevel fluctuations and climate change. We propose that the change in reef biota and reef types across the K/T boundary and during the Early Tertiary were important causes of the parallel changes in platform growth style.     

A probable erroneous identification of Tricolporopollenites distinctus groot et penny from lowermost Cretaceous strata in the eastern Netherlands

The occurrence of Tricolporopollenites distinctus Groot et Penny 1960, recently mentioned by Burger in lowermost Cretaceous strata in the eastern Netherlands, is possibly due to contamination by material from Lower Tertiary deposits.     

<Emphasis Type="Italic">Protungulatum</Emphasis>, Confirmed Cretaceous Occurrence of an Otherwise Paleocene Eutherian (Placental?) Mammal

Neither pre-Cenozoic crown eutherian mammals (placentals) nor archaic ungulates (“condylarths”) are known with certainty based on the fossil record. Herein we report a new species of the Paleocene archaic ungulate (“condylarth”) Protungulatum from undisputed Late Cretaceous aged rocks in Montana USA based on an isolated last upper premolar, indicating rare representatives of these common early Tertiary mammals appeared in North America a minimum of 300 k  years before the extinction of non-avian dinosaurs. The other 1200 mammal specimens from the locality are characteristic Late Cretaceous taxa. This discovery overturns the current hypothesis that archaic ungulates did not appear in North America until after the Cretaceous/Tertiary (K/T) boundary and also suggests that other reports of North American Late Cretaceous archaic ungulates may be correct. Recent studies, including ours, cannot determine whether Protungulatum does or does not belong to the crown clade Placentalia.     

Illicioxylon, an Element of Gondwanan Polar Forests? Late Cretaceous and Early Tertiary Woods of Antarctica

The Late Cretaceous and early Tertiary sediments from the northernPeninsula region of Antarctica yield a rich assemblage of fossilwood with well preserved anatomy. Wood specimens of a previouslyrecognized morphotype are described. The woods are characterizedby diffuse porous wood, mainly solitary vessels with long scalariformperforation plates, scalariform and opposite vessel-ray pitting,generally uniseriate and biseriate heterogeneous rays, and tracheidswith obvious uniseriate, circulate, bordered pits. These fossilspecimens show greatest anatomical similarity to the organ genusIllicioxylon Gottwald and extant members of the Illiciaceae.The occurrence of illiciaceous-like wood in Gondwana suggeststhat the distribution of this family may have been more widespreadin the geological past and that a relatively warm temperateclimate prevailed over the northern Peninsula region of Antarcticaduring the Late Cretaceous and early Cenozoic. Copyright 2000Annals of Botany Company Fossil, wood, Illiciaceae, Illicioxylon, Illicium, Cretaceous, Tertiary, Gondwana, Antarctica     

木瓜榕传粉榕小蜂雌蜂触角感器的分布和超微形态

为探索木瓜榕传粉榕小蜂Ceratosolen emarginatus寄主定位机制, 应用扫描电镜和透射电镜观察了其雌蜂触角感器的类型、 分布和超微形态。结果显示： 木瓜榕传粉榕小蜂雌蜂触角呈膝状, 由柄节、 梗节和11个鞭小节组成的鞭节组成, 第3鞭小节着生一坚固的脊骨突。触角上共发现7类11种感器, 分别为毛形感器、 刺形感器、 锥形感器（包括单孔形和多孔形）、 多孔板形感器（包括长形和圆形）、 腔锥形感器（分为3种类型）、 栓锥形乳突状感器、 角锥形感器。结合表面特征和内部结构, 锥形感器、 多孔板形感器、 栓锥形乳突状感器和腔锥形感器类型1为有孔型, 为化学感器; 无孔型的毛形感器和刺形感器是机械感器, 但腔锥形感器类型2和3为本体感器或湿热压力感器; 最为特异的为角锥形感器, 其厚壁无孔, 逆向触角主轴, 为该科昆虫所特有, 推测可防止传粉榕小蜂进入榕果时滑脱。这些结果将有助于理解木瓜榕传粉榕小蜂特异性行为, 并为下一步开展电生理研究, 揭示其信息化学物质利用和分配模式奠定基础。     

Early penguin fossils, plus mitochondrial genomes, calibrate avian evolution

Testing models of macroevolution, and especially the sufficiency of microevolutionary processes, requires good collaboration between molecular biologists and paleontologists. We report such a test for events around the Late Cretaceous by describing the earliest penguin fossils, analyzing complete mitochondrial genomes from an albatross, a petrel, and a loon, and describe the gradual decline of pterosaurs at the same time modern birds radiate. The penguin fossils comprise four naturally associated skeletons from the New Zealand Waipara Greensand, a Paleocene (early Tertiary) formation just above a well-known Cretaceous/Tertiary boundary site. The fossils, in a new genus (Waimanu), provide a lower estimate of 61-62 Ma for the divergence between penguins and other birds and thus establish a reliable calibration point for avian evolution. Combining fossil calibration points, DNA sequences, maximum likelihood, and Bayesian analysis, the penguin calibrations imply a radiation of modern (crown group) birds in the Late Cretaceous. This includes a conservative estimate that modern sea and shorebird lineages diverged at least by the Late Cretaceous about 74 +/- 3 Ma (Campanian). It is clear that modern birds from at least the latest Cretaceous lived at the same time as archaic birds including Hesperornis, Ichthyornis, and the diverse Enantiornithiformes. Pterosaurs, which also coexisted with early crown birds, show notable changes through the Late Cretaceous. There was a decrease in taxonomic diversity, and small- to medium-sized species disappeared well before the end of the Cretaceous. A simple reading of the fossil record might suggest competitive interactions with birds, but much more needs to be understood about pterosaur life histories. Additional fossils and molecular data are still required to help understand the role of biotic interactions in the evolution of Late Cretaceous birds and thus to test that the mechanisms of microevolution are sufficient to explain macroevolution.     

EVOLUTIONARY TRENDS IN THE GENUS GINKGO

Three main independent phylogenetic groups within Ginkgoales , consisting of different families, are suggested. It is considered impossible to deduce the genus Ginkgo from any other genus by means of fossil evidence known at present.
The oldest finds of Ginkgo date from the Lower Jurassic. During the Cretaceous, increasing polymorphy in foliar remains indicates the rise of new species. During the Lower Cretaceous there also appears a type of leaf known both as G. adiantoides and as G. paradiantoides. This leaf is from the gross morphological and the anatomical point of view almost identical with the Tertiary and Recent Ginkgo populations, thus making a direct ancestry between the present-day Ginkgo and those of the Lower Cretaceous likely. By Lower Tertiary times a considerable reduction has taken place leaving only one gross morphological type of leaf, that of G. adiantoides. This is suggested to be identical with G. biloba. Although there is no positive evidence, it can be assumed that the final reduction of the genus, to its present-day East Asiatic home, has taken place during the Pleistocene period.     

中国植物区系中的特有性及其起源和分化

对中国植物区系中的239个特有属,分属67个科,进行了分析研究,列出了这些特有属在种子植物各个科的分布,现代地理分布范围。结果表明含特有属在10个以上的有5个科即Gesneriaceae,Compositae,Labiatae,Cruiciferae,Umbelliferae;其中以Gesneriaceae居榜首(27属),Compositae位居第二(20属),Labiatae有12属,居第三。含2属的科有15个,含1属的科有30个;其中Ginkgaceae,Davidiaceae,Eucommiaceae,Acanthochlamydaceae组成了中国植物区系最具古老性、特有性和代表性的4个单型科。在此基础上,从特有属在被子植物八纲系统各个纲的分布特点,以及在各个科组成和系统关系及已有地质、化石历史和系统学,形态,分子证据论述了这些特有属的起源、系统关系及在植物地理上的关系。在裸子植物中,特有属最为丰富,几乎皆是地质历史上北极-第三纪成分的残遗,起源时间较早,可追溯到白垩纪或更早。被子植物中,中国特有属存在于八纲被子植物的所有纲中,几乎在现代被子植物各个演化阶段均有古老残遗的特有类群存在,同时也不乏新特有类群尤其是在演化的高级阶段的类群。从起源上看,被子植物的古特有属主要发生于晚白垩纪和早第三纪,地质历史上大都占有广阔的分布区;新特有属多发生在新第三纪以后。其源头主要是北极第三纪、古热带第三纪(冈瓦纳第三纪)和古地中海第三纪的奇妙结合,不少类群是就地起源的;特有性是在第三纪中晚期以后北半球气候变迁,迁移途径(如北大西洋陆桥和白令陆桥)中断后形成的,这一时期是我国特有属形成发展的起始标志。     

Dicotyledonous woods from the Upper Cretaceous of southern Illinois

Dicotyledonous woods from the Upper Cretaceous of Southern IllinoiS. Five species of fossil dicotyledonous wood are described from an Upper Cretaceous (Maestrichtian; locality in Alexander County, IllinoiS. U.S. A. Paraquercimum cretaceum has structure similar to the Fagaceae (evergreen Oak- Lithocarpus ) and Casuarinaceae and represents the earliest known occurrence of this structural type (large solitary pores and uniseriate and large multiseriale rays). Paraphyltanthoxyhin illirioisense and Icacinoxylon alternipunctata are species of genera represented at other Cretaceous and Early Tertiary localities In large diameter trees. Parabombacaceoxylon magniporosum has large diameter pores and scalariform perforation plates, a combination of characters that is extremely rare in the extant flora. Paraapocynaceoxylon barghoorni has a combination of characters represented in extant Apocynaceae. These five species lack growth rings, have high vulnerability indices (mean vessel diameter divided by mean number of vessels per square millimeter, and a relatively high proportion of ray parenchyma. They lack specialized wood anatomical characters, and a compilation of vessel element lengths in these and other Cretaceous woods indicates that short vessel elements (a derived character) were less frequent in the Cretaceous than in extant dicotyledonous trees.