Durch Protophytobia cupressorum gen. nov., sp. nov. (Agromyzidae,Diptera) verursachte Markflecke in einem Holz von Juniperoxylon aus dem Tertiär von Süd-Limburg (Niederlande) und der Nachweis von Markflecken in einer rezenten Callitris-Art

From a cupressaceous wood described by Kräusel & Schönfeld (1974) of the Tertiary of South-Limburg (Netherlands) Greguss (1970) selected such pieces showing remains of insect food. In a recent Callitris species from Australia he found the some phenomenon (1970). Indeed Greguss considered these phenomena as a natural specific wood element. Really these are pith flecks are caused by a cambium-mining insect. Both are described in the present paper. I name the pith flecks in the fossil coniferous wood of South-Limbourg Protophytobia cupressorum gen. nov., sp. nov. Under such name is considered an insect only represented by their characteristic food channals. In living angiospermous woods Phytobia Lioy (Agromyzidae, Diptera) is the only genus hitherto known. In coniferous woods recent species are unknown. The food channals in conifers in great part closed by changed tracheids.     

Paléoxylologie: Étude anatomique comparée de Scleromedulloxylon aveyronense nov. gen. nov. sp. du Permien de St-Affrique (Aveyron,France); considérations taxinomiques et stratigraphiques

The fossil woods studied in the present paper were collected by P. Béziat in the Permian Basin of St-Affrique (Southern Aveyron). They come from near Calmels. They are the first fossil woods collected and described in this basin.The secondary wood refers to the form genus Dadoxylon and more exactly to the speciesDadoxylon schrollianum (Goeppert, 1864–65) Frentzen, 1931, Frentzen, 1931. The pith is certainly related with the pith structure of Walchiapremnon valdajolenseFlorin, 1940.The association of a Dadoxylon secondary wood with an irregularly septate pith containinggroups of probably sclerotic cells can be found in Cedroxylon varollenseRenault, 1893–1896, Renault and Roche, 1894 from the Basin of Autun. It is not possible to conserve the species varollense in the genus Cedroxylon and we propose the form genus Scleromedulloxylon for the petrified structure from Autun and for the fossil woods of St-Affrique.Furthermore, a comparative anatomical study of the different Permo-Carboniferous structuresfrom the Euramerican province let us, when it is possible, distinguish structure-types related to Cordaitophyts or to Coniferophyts. In the present case, Scleromedulloxylo should rather correspond to the fossil wood of an Autunian Coniferophyt, that is to Walchia structure.     

Taxodioxylon gypsaceum (Göppert) Kräusel,legno fossile rinvenuto nel miocene dell'Italia centrale

Abstract

Taxodioxylon gypsaceum (Göppert) Kräusel, wood fossil discovered in the central italian miocene.—A sample of silicified wood fossil has been discovered in the miocenic formations of the Castellaro mountain in the neighbourhood of Pesaro a city in Central Italy. An anatomical study has made it possible to accept that the species is Taxodioxylon gypsaceum, which resembles the actual Sequoia sempervirens for its woody structure, conservative endemism of a coastal region in California. The fossil species that is known for its numerous tertiary deposits in the Northern, Central and Eastern Europe, is now indicated for the first time in Italy; the mount Castellaro station results to be the more south among those in Europe.

Various paleobotanical data concerning traces of leaves, fruits and seeds gathered in localities near to the deposit and in the region complies with the discovery of Taxodioxylon gypsaceum because of the presence of varions species of Sequoia and Taxodium and in particular of the Sequoia langsdorfii leaves which is considered as the ancient form of the Sequoia sempervirens.     

DEVELOPMENT OF CHAMBERED PITH IN STEMS OF PHYTOLACCA AMERICANA L. (PHYTOLACCACEAE)

An integrated microscopic (light and electron microscopy) and macroscopic investigation of chambered pith development was made of Phytolacca americana L. Terminal internodes have a solid pith cylinder in contrast to the alternating diaphragms and chambers occurring in subjacent pith. Macroscopically, chambers and diaphragms of any one internode are of equal size. Microscopically, diaphragms vary in height within an internode (from 1–6 cells high). Nevertheless, all diaphragms become thicker circumferentially (5–12 cells high) and connect with long files of intact peripheral pith cells. Diaphragm cells have a large centrally positioned vacuole with a thin, parietal layer of cytoplasm; nuclei, mitochondria, endoplasmic reticulum, and unidentified organelles differentiate in the cytoplasm of diaphragm cells. Although schizogenous activity has most often been implicated as the mechanism by which chambered pith develops in vegetative organs of angiosperms, the results of this study show that cavities in pokeweed result from both schizogenous and lysigenous mechanisms. Schizogeny is suggested by the fact that central pith cells of terminal internodes are longer and thinner walled than peripheral pith cells arranged in vertical files, thus indicating elongation of cells as a possible result of internode elongation. The precise developmental pattern and arrangement of chambers and diaphragms also suggest schizogenous processes. Lysigenous or enzymatic activity is indicated by the fact that cavities are bounded by broken cells, and wall fragments and organelles are often found within enlarging cavities. Chamber formation occurs continuously acropetally and centrifugally in the central pith. A comparison of diaphragms is made with Liriodendron tulipifera and Juglans nigra in an attempt to resolve differences in structure and terminology regarding the differentiation of chambered and diaphragmed pith.     

Ontogeny of the proventitious epicormic buds in Quercus petraea.

In the present work, we described the fate of proventitious epicormic buds on the trunks of 40-year-old Quercus petraea trees and in parallel the vascular trace they produced in the wood. Our results show that small and large individual epicormic buds can survive as buds for 40 years and that both are composed of a terminal meristem and scales. Meristematic areas are detected in the scale axils of small buds; in addition to these meristems the large buds also have secondary bud primordia. The small buds are connected to the pith of the main stem by a unique trace, whereas the large buds are connected by one or multiple traces. A single trace might imply that the whole bud is still alive and multiple traces might indicate that the terminal meristem has died. In the latter case, each trace is connected to a secondary bud of the large bud. The buds found in a cluster are composed of a terminal meristem and scales with axillary meristems in the scale axils. A cluster is connected to the pith of a stem either by a unique trace when it seems to be the result of partial abscission of an epicormic shoot or multiple traces when it might have originated from an epicormic bud in which the terminal meristem has died. Whatever the type of the bud, the vascular trace in the bark is composed of a cambium, secondary xylem and parenchyma cells and the trace present in the wood had parenchyma cells with vestiges of secondary xylem. Each year, the vascular trace should be produced in the bark by the cambium of the tree but not by the bud itself. On 40-year-old Q. petraea, we observed a proliferation of epicormic buds and in parallel a multiplication of the number of vascular traces in the trunk, but the knots caused by the traces of epicormic buds in the wood, either as individuals or in clusters, are minor since their colours are only slightly darker than those of woody rays and they are less than 2 mm in diameter. The knots will appear when epicormic buds develop into shoots. Received: 30 March 1999 / Accepted: 09 June 1999     

Paleobotanical remains from the Paleocene–lower Eocene Vagadkhol Formation, western India and their paleoclimatic and phytogeographic implications

A small assemblage of macro- and micro floral remains comprising fossil leaf impressions, silicified wood, spores, and pollen grains is reported from the Paleocene–lower Eocene Vagadkhol Formation (=Olpad Formation) exposed around Vagadkhol village in the Bharuch District of Gujarat, western India. The fossil leaves are represented by five genera and six species, namely, Polyalthia palaeosimiarum (Annonaceae), Acronychia siwalica (Rutaceae), Terminalia palaeocatapa and T. panandhroensis (Combretaceae), Lagerstroemia patelii (Lythraceae), and a new species, Gardenia vagadkholia (Rubiaceae). The lone fossil wood has been attributed to a new species, Schleicheroxylon bharuchense (Sapindaceae). The palynological assemblage, consisting of pollen grains and spores, comprises eleven taxa with more or less equal representation of pteridophytes, gymnosperms, and angiosperms. Angiospermous pollen grains include a new species Palmidites magnus. Spores are mostly pteridophytic but some fungal spores were also recovered. All the fossil species have been identified in the extant genera. The present day distribution of modern taxa comparable to the fossil assemblage recorded from the Vagadkhol area mostly indicate terrestrial lowland environment. Low frequency of pollen of two highland temperate taxa (Pinaceae) in the assemblage suggests that they may have been transported from a distant source. The wood and leaf taxa in the fossil assemblage are suggestive of tropical moist or wet forest with some deciduousness during the Paleocene–early Eocene. The presence of many fungal taxa further suggests the prevalence of enough humidity at the time of sedimentation.     

银杏营养器官解剖结构的观察

为了揭示不同树龄银杏的根、茎、叶解剖结构以及内生菌分布情况,本研究采用石蜡切片法对银杏(Ginkgo biloba L.)根、茎、叶显微解剖结构进行了观察。结果显示:(1)一年生银杏幼根不含树脂道,内生菌含量低,而皮层中含有大量蛋白细胞;多年生银杏老根含有较多树脂道,皮层细胞中含有大量内生菌并有针晶物质分布,未发现蛋白细胞。(2)一年生银杏幼茎有明显的角质层,皮层分布有大量蛋白细胞,韧皮射线及髓部发达,其中髓由大量薄壁细胞构成并且有蛋白细胞分布,未观察到树脂道但有簇晶物质存在。(3)多年生银杏叶片海绵组织疏松,具有树脂道,叶肉细胞含有簇晶物质;气孔下陷并具有耐旱的结构特点。本结果可为研究不同树龄银杏对环境的适应性变化以及内生菌特点提供参考。     

接骨草的显微结构及其绿原酸组织化学定位研究

运用石蜡切片法和荧光显微镜观察法研究了3个不同接骨草(Sambucus chinensis Lindl.)居群营养器官的显微结构及其绿原酸的分布规律。结果表明:(1)接骨草地上茎厚角组织明显,髓部由大小不等的两类薄壁细胞组成,且有单宁细胞分布;地下根状茎厚角组织细胞小,髓部薄壁细胞大小差异不明显,皮层及髓中有油细胞分布。(2)叶片为异面叶,栅栏组织细胞为短柱状,油细胞不明显。(3)绿原酸分布在根状茎皮层部分细胞、茎厚角组织部分细胞及叶片的海绵组织中,以海绵组织中含量最高。研究认为,髓部薄壁细胞大小的差异可作为接骨草的一个鉴别特征;荧光显微镜观察法可迅速准确显示绿原酸的分布;在所研究的3个接骨草居群中,怀化居群的绿原酸含量最高,若以绿原酸为有效成分来采收接骨草,可以只采收叶。     

Sclerospiroxylon xinjiangensis nov. sp., a gymnospermous wood from the Kungurian (lower Permian) southern Bogda Mountains,northwestern China: Systematics and palaeoecology

A new silicified wood, Sclerospiroxylon xinjiangensis Wan, Yang et Wang nov. sp., is described from the Cisuralian (lower Permian) Hongyanchi Formation in southeast Tarlong section, Turpan City, Xinjiang Uygur Autonomous Region, northwestern China. The fossil wood is composed of pith, primary xylem and Prototaxoxylon-type secondary xylem. The pith is solid, circular, heterocellular, with sclerenchyma and parenchyma. The primary xylem is endarch to mesarch, with scalariform thickenings on tracheid walls. The secondary xylem is pycnoxylic, composed of tracheids and parenchymatous rays. Growth rings are distinct. Tracheids have mostly uniseriate, partially biseriate araucarian pitting on their radial walls. Helical thickenings are always present on both the radial and the tangential walls. Rays are 2–14 cells high, with smooth walls. There are 2 to 7, commonly 2 to 4 cupressoid pits in each cross-field. Leaf traces suggest that S. xinjiangensis nov. sp. was evergreen with a leaf retention time of at least 15 years. Based on the sedimentological evidence, growth rings within the S. xinjiangensis nov. sp. could have been caused by seasonal climatic variations, with unfavorable seasons of drought or low temperature. Low percentage of latewood in each growth ring is probably due to the intensity of climatic seasonality and/or long leaf longevity.     

A SEASONAL STUDY OF THE VEGETATIVE SHOOT APEX AND THE PATTERN OF PITH DEVELOPMENT IN HIBISCUS SYRIACUS

Tolbert , Robert J. (West Virginia U., Morgantown.) A seasonal study of the vegetative shoot apex and the pattern of pith development in Hibiscus syriacus. Amer. Jour. Bot. 48(3): 249–255. Illus. 1961.—The shoot apex of Hibiscus syriacus L. is described as having a cytohistological zonation superimposed on a tunica-corpus configuration. The apex is flat-topped or may have a saddle-back or concave appearance as seen in median longitudinal section. The metrameristem, consisting of the tunica and corpus initials, is comprised of large, light-staining, vacuolate cells that have thick cell walls and exhibit much dark-staining intercellular substance. Surrounding the metrameristem is the flanking meristem, which is responsible for the outer layers of the shoot, and from which the leaf primordia arise. The pith rib meristem lies below the metrameristem and consists of files of cells that are responsible for the pith. There are no major seasonal changes in the structure of the apex during the yearly cycle. The pith displays a long-shoot type of development with the cells remaining in distinct files during the first flush of growth in the spring. As growth slows and internode elongation is gradually reduced, the pith displays the characteristic short-shoot type of development, consisting of a spongy tissue of rounded cells with many intercellular spaces and no distinct files of cells. A crown is differentiated across the top of the pith at the end of the growth period. This consists of a band of cells with thick, dark-staining cell walls, which separates by the apex from the last year's growth. In contrast to many gymnosperms, this crown is dispersed by renewed cell activity the following spring.     

Comparative wood anatomy of Andromedeae s.s., Gaultherieae, Lyonieae and Oxydendreae (Vaccinioideae, Ericaceae s.l.)

The wood anatomical structure of 11 out of 13 genera from four tribes of the Vaccinioideae, namely Andromedeae s.s. , Gaultherieae, Lyonieae and Oxydendreae (Ericaceae s.l. ), is described using light and scanning electron microscopy. Several features of the secondary xylem support the tribal classification based on molecular data: arrangement of vessel-ray pitting, height of multiseriate rays and the shape of the body ray cells. Oxydendreae are clearly defined from the other representatives by various wood anatomical features. Gaultherieae can be distinguished from Lyonieae by differences in vessel perforation plates, vessel-ray pitting, height and structure of multiseriate rays, and occurrence of prismatic crystals, but the wood of Andromedeae s.s. is similar to Gaultherieae. Moreover, Andromedeae s.s. , Oxydendreae and Vaccinieae are characterized by their pith structure, whereas considerable variation in the pith cells is found in Lyonieae and Gaultherieae.  © 2004 The Linnean Society of London, Botanical Journal of the Linnean Society , 2004, 144 , 161–179.     

An ancient example of Platycladus (Cupressceae) from the early Miocene of northern China: origin and biogeographical implications

A number of cupressaceous fossil leaves are described in this paper that come from the lower Miocene of Inner Mongolia, northern China. These new examples of fossil leaves are compressed, have their branchlets arranged in a plane, either spreading or ascending, and are flat. These specimens also possess scale-like leaves that are dimorphic, preserved facial leaves that are rhomboidal and have obtuse apices, and lateral leaves that are boat-shaped and have slightly incurved apices. The epidermal cells of these fossils are quadrangular, rectangular, or narrowly rectangular, while the leaves are amphistomatic, and stomata are elliptical or oblong, and monocyclic. In comparison with both living and related fossil taxa, we identify the new fossils as Platycladus preorientalis sp. nov. Taken in combination with a molecular phylogenetic analysis, the new fossils suggest that the genus Platycladus originated in the Oligocene in mid and high Asian latitudes. Thus, the ancient Platycladus lineage probably migrated from Europe to Asia following the closure of the Turgai strait during the Oligocene.     

Fossil wood of Euphorbiaceae from the Tertiary of West Bengal,India

The paper describes a new species of fossil wood of Euphorbiaceae, Mallotoxylon cleidionoides sp. nov. from the Tertiary Laterites near Santiniketan, Birbhum District of West Bengal. The structure of the fossil wood closely resembles the wood anatomy of the extant genus Mallotus Lour. This is the first record of the occurrence of an euphorbiaceous wood from the Tertiary of West Bengal.     

ANATOMICALLY PRESERVED GLOSSOPTERIS STEMS WITH ATTACHED LEAVES FROM THE CENTRAL TRANSANTARCTIC MOUNTAINS,ANTARCTICA

Stems and buds of Glossopteris skaarensis Pigg and buds of G. schopfii Pigg from the Permian Skaar Ridge locality in the central Transantarctic Mountains, Antarctica demonstrate the first anatomically preserved glossopterids known with stem/leaf attachment. Stems of G. skaarensis are 1–12 mm in diameter ( = 3.1 mm) with a broad pith, poorly defined primary xylem, and a zone of secondary xylem up to 6 mm thick. Pycnoxylic wood conforming to Araucarioxylon Kraus is composed of tracheids with uni- to biseriate oval to hexagonal bordered pits on radial walls, uniseriate rays one to a few cells high, and cupressoid to taxodioid cross-field pitting. Stems have a narrow zone of secondary phloem, aerenchymatous cortex with scattered sclereids, and sometimes a narrow periderm. Two wedge-shaped leaf traces each bifurcate to form four strands in the base of each petiole. Small axillary branches are vascularized by double branch traces that fuse at the margin of the main axis. Buds of G. skaarensis have leaves with narrow lateral laminae and a thickened midrib containing a wide lacuna, delicate vascular strands, and a prominent hypodermis. In contrast, buds of G. schopfii have uniformly thick leaves with prominent, circular vascular bundle sheaths. These anatomical details are used to reconstruct individual types of glossopterid plants, providing new information toward understanding the ecology and evolution of this important group of Permian seed plants.     

Nageiaceae—A New Gymnosperm Family

A new monotypic gymnosperm family, Nageiaceae D. Z. Fu, is separated from Podocarpaceae. It is characterized by having multinerved leaves without costae, and primitive shoot-like female reproductive organs (female strobili). The new family contains a single genus consisting of 2 sections, 5 species and is distributed along the western coast of the Pacific, from low coastal mountains of eastern and southern Asia to the Phillipines and Papua New Guinea. The first species in the Nageiaceae was described as an angiosperm, Myrica nagi Thunb. (1784), but it was soon recognized to be a gymnosperm belonging to a new genus, and was renamed as Nageia japonica Gaert. (1788). The generic name, Nageia, however, has seldom been used, and the members of Nageia have generally been treated as an isolated section of Podocarpus in the Podocarpaceae. When revising the Podocarpaceae, De Laubenfels (1969) established a new genus Decussocarpus based on Nageia, but several years later (1987) he revived the old generic name, Nageia. Page ( 1988,1990)considered Nageia to be a valid generic name and redefined it as a natural genus. The distinctive,broadly lanceolate, multinerved leaves (without costae) of Nageia are rather unusual in gymnosperms,only being similar to those of Agathis in the Araucariaceae, their leaves are also similar to each other in anatomy. For example, there are many single vascular bundles arranged parallelly, between which occur sclerenchyma cells in the mesophyll. Apparently,leaves in Nageia are rather similar both externally and internally to paleogymnosperm cordaitean leaves, and sclerenchyma cells found in Nageia might be the remains of straps between veins in cordaitean leaves. In addition to leaf characters, the large and nearly round pith of the young shoot in Nageia appears to be a reminiscent of the large pith in cordaitean stem. The female reproductive organs (female strobili ) in Nageia are shoot-like. The female strobilus has a sterile terminal bud, and several opposite or subopposite sterile scaly bracts on its axis; two opposite megasporophylls are found near the axis apex and both have an anatropous ovule which is almost entirely covered by the megasporophyll; a bract is partly adnate to the lower back of the megasporophyll;mature arillate seeds are 1-2 or occasionally 3 in number; the axis becomes woody when the seeds mature, but in some species (N. wallichiana) the upper part of the axis becomes fleshy (in the shape of a receptacle), in which no distinct boundary was found between the fleshy receptacle and the woody part, and both have the same scaly bracts or traces. Many characters in Nageia are distinctly different from those in Podocarpus. Leaves in the Podocarpaceae have distinct midribs; in Podocarpus, the reproductive organ, which was generally thought to be similar to that in Nageia, has no terminal bud, and its bract is entirely free from the lower back of the megasporophyll, the fleshy receptacle is derived from both the axis and the sterile bracts (except the lowest two), and the female strobilus at the seed stage has a secondary stalk. The multinerved leaf in Nageia can rarely be found in most of the living gymnosperms except in some rather isolated groups, such as Araucariaceae, Ephedraceae,Ginkgoaceae and Welwitschiaceae. Paleobotanical evidence shows that multinerved leaves have been found in all of the geological ages from the Paleozoic to the present, and such a shoot-like female reproductive organ as in Nageia was found in some paleogymnosperms. It is very difficult to determine the systematic positions of these fossil plants because of lacks adequate material of reproductive organs or even lack of complete vegetative organs. The vascular system and leaf characters of gymnosperms are considered to be very conservative, and the fact that the common leaf shape and venation exist in both fossil and living gymnosperms could imply that there exists a multinerved-leaved evolutionary line ( M-line ) in gymnosperms, which could be traced back to the paleogymnosperm cordaitean plants or even older ones with multinerved leaves. The different types of the female strobili (female reproductive organs) of living gymnosperms, regardless of having one or only several seeds without a typical cone or many seeds with a cone, might have been derived from shoot-like or spikelike female reproductive organs possessed by their common ancestor.The fossil eviden ce shows that the typical cone similar to those of living gymnosperms first appeared in the Jurassic, much later than the single-seeded fossil plant without cones. The seed fossil appeared in the late Devonian Period. It is very difficult to infer the relationships among living gymnosperms, which are hardly derived from one another. But an analysis of the strobili, including the axis structure and position, number, morphology and degree of adnation of the phyllomes on them, would be helpful to the study of their phylogeny. It is evident, therefore, that the gymnosperms with leaves having a midrib might also have a rather long evolutionary course,but no transition between the midrib and multinerved patterns of leaf venation has so far been found in both living and fossil plants. Finally, it is noteworthy that the Nageiaceae are distributed along the western coast of the Pacific, where many primitive representatives, both in gymnosperms and angiosperms, still survive. This would be advantageous to the consideration of Nageiaceae as a primitive representative, or a descendant of fhe paleogymnos-perm cordaitean plants.     

濒危植物海南风吹楠营养器官解剖结构特征

该研究采用石蜡切片和光学显微技术,对海南风吹楠营养器官的解剖结构及其对环境的适应性进行了探讨。结果表明:海南风吹楠为典型异面叶,叶片中脉发达,中部分化出髓,上表皮外侧具角质层,内侧具1层内皮层,下表皮外侧无角质层,有气孔器分布,气孔器为双环型,略下陷;栅栏组织3~4层细胞,海绵组织4~6层细胞。茎的初生结构中表皮轻微角质化,维管束为外韧型,8~10个初生维管束围绕髓排列为1轮;茎的次生结构中,表皮外部角质层加厚,维管柱紧密排列连成环状,次生韧皮部和次生木质部发达,形成层细胞3~5层。根的初生结构中表皮细胞外壁加厚,外皮层细胞体积大,形状不规则,内侧具1层形成层,内皮层具凯氏带,初生木质部为多原型,呈辐射状排列。根的次生结构中木栓层细胞5~6层,木栓层内侧具1层木栓形成层,栓内层细胞3层。海南风吹楠营养器官具有一定耐阴和耐旱结构特征,同时与其生活的热带雨林沟谷中高温荫湿的环境相适应。     

CHATTAWAYA (STERCULIACEAE): A NEW GENUS OF WOOD FROM THE EOCENE OF OREGON AND ITS IMPLICATIONS FOR XYLEM EVOLUTION OF THE EXTANT GENUS PTEROSPERMUM

A new sterculiaceous wood, Chattawaya paliformis gen. et sp. n., was collected from a Middle Eocene locality in the type area of the Clamo Formation of north central Oregon. The wood differs from all known extant woods in having very large and irregularly shaped tile cells. However, other features of the xylem indicate a close natural relationship between Chattawaya and the extant paleotropical genus, Pterospermum. It is suggested that the xylem organization of the Eocene fossil represents a more primitive condition than that observed in Pterospermum. Comparative xylotomy indicates three evolutionary trends within the complex to which Chattawaya and Pterospermum belong: development of storied structure, increased uniformity in shape and size of tile cells and loss of multiseriate rays. Chattawaya is part of a growing body of paleobotanical evidence indicating that the Sterculiaceae was well differentiated by the early Tertiary, but that the lineages leading to extant genera have undergone an appreciable amount of evolutionary change since the Eocene.     

Turonian Pinaceae of the Raritan Formation, New Jersey

 Fossil vegetative and reproductive structures from deposits of the Raritan Formation in New Jersey (Turonian, Upper Cretaceous, ∼90 MYBP) include ferns, gymnosperms, and angiosperms. Gymnosperms collected from this formation have been known since the beginning of the 20th century. Fossil leaves, wood and seed cones have been are identified as belonging to the Cupressaceae, Pinaceae, and Taxodiaceae. In the present contribution, we describe a series of fossil dwarf shoots, leaves and a pollen cone belonging to the family Pinaceae. Fossils are charcoalified with preserved three-dimensional structure and excellent cellular detail. The dwarf shoots are assigned to a new species Prepinus crossmanensis sp. nov. and to the previously described Pinus quinquefolia Jeffrey. The new species Prepinus crossmanensis differs in size, shape, presence of hypodermis, sclerenchyma and stomata in the cataphylls, and number and shape of needle leaves from previously known species. Also, isolated leaves were found that were assigned to the new species, Prepinus raritanensis sp. nov. The new species is differentiated by the size and shape of stomata, the presence of number of layers of the hypodermis; and the cell-shape and number of layers of the mesophyll and transfusion tissue. A previously undescribed male cone, Amboystrobus cretacicum gen. and sp. nov., has an axis with spirally attached microsporophylls, each bearing two abaxial ovoid microsporangia. The pollen grains are monosulcate and bisaccate (eusaccate), with an elliptical corpus, granulate exine sculpture, and honeycomb-like wall structure. Received March 21, 2000 Accepted November 13, 2000     

Tetracentron Wood from the Miocene of Noto Peninsula,Central Japan,with a short revision of homoxylic fossil woods

A vesselless fossil wood was discovered in the Miocene Yanagida Formation in the Noto Peninsula, central Japan. This fossil has distinct growth rings with gradual transition from the early- to the latewood ; tracheids, which are called 'usual traeheids' here, constitute the ground mass of the wood and have typical scalariform bordered pits on radial walls in the earlywood and circular sparse pits on those in the latewood ; rays are 1\2-4 cells wide and heterogeneous with low to high uniseriate wings; axial parenchyma strands are scattered in the latewood. This wood has a peculiar feature; sporadic radial files of broad tracheids whose tangential walls have crowded alternate bordered pits. The radial walls have crowded half-bordered pits to ray cells, but no pits to the usual tracheids. Among all of the extant and extinct angiosperms and gymnosperms, these unusual tracheids occur only in Tetracentron. From these features, we refer the fossil to the extant genus Tetracentron, and name it T. japonoxylum. A revision of homoxylic woods is made for comparision with the present fossil. Tetracentron japonoxylum is the only fossil wood of Tetracentron.