ULTRASTRUCTURAL AND PALEOBIOCHEMICAL CORRELATIONS AMONG FOSSIL LEAF TISSUES FROM THE ST. MARIES RIVER (CLARKIA) AREA,NORTHERN IDAHO,USA

Miocene angiosperm leaf tissues of Betula, Hydrangea, Platanus, and Quercus, and of Castanea, Persea, and gymnospermous tissues from offshore and onshore lacustrine sediments, respectively, reveal various states of ultrastructural detail in preservation which correlate with their paleobiochemical profiles. Excellent cytologic preservation of membrane-bound organelles in offshore tissue samples is correlated with relatively mild chlorophyll and fatty acid degradation (chlorins, unsaturated hydrocarbons), while progressive deterioration of ultrastructure seen in onshore specimens is concomitant with extensive chlorophyll degradation and saturation of hydrocarbons. Comparative studies between fossils found in pyroclastic (Succor Creek Flora, Miocene) and lacustrine (Clarkia Flora) environments indicate that the degree of pre- and post-depositional hydration of tissues is a less significant factor in determining preservation than redox potential and secondary metabolites (tannic acids, chlorophyll derivatives). A sequence of organelle degradation in leaf tissues is given, and it is suggested that chloroplasts and cell walls are the most stable cellular constituents, while the endoplasmic reticulum, nuclei, and mitochondria are the most labile.     

LIRIODENDRON (MAGNOLIACEAE) FROM THE MIOCENE CLARKIA FLORA OF IDAHO

Miocene Liriodendron carpels, whole fruiting structures and leaves from Clarkia and Oviatt Creek sites in northern Idaho are preserved as imprints and compressed fossils in soft lacustrine clays. The isolated carpels are indistinguishable from those described as L. hesperia Berry from the Spokane Latah flora. Fruit aggregates from the type Clarkia and Oviatt Creek localities and leaves from three Clarkia sites are considered to be within the range of variation of the single species L. hesperia. Comparisons were made regarding leaf architecture, lower leaf epidermal structures, leaf flavonoid and steroid analysis, morphological features of receptacles and carpels, and the venation pattern of carpels of the fossil material to the two extant species, L. tulipifera L. (native to southeastern United States) and L. chinense Sarg. (native to southeastern Asia). Leaf architecture features analyzed by standard statistical and canonical tests and marginal venation patterns near the base of leaves suggest that L. hesperia is more similar to L. tulipifera, whereas the size dimensions of lower epidermal cells and the common presence of two sterane compounds imply that L. hesperia is more similar to L. chinense. The fossil species, however, is a distinct taxon indicated by statistical discriminant and canonical tests, leaf base shape, often smaller epidermal cell dimensions, and the shape of round receptacle carpel scars. Both the fossil and the two living Liriodendron species are associated with comparable mixed mesophytic floras.     

The flora of the early Miocene Brandon Lignite, Vermont, USA. VIII. Caldesia (Alismataceae)

Caldesia, a genus of aquatic monocotyledons, is represented by four living species, which are widely distributed in the temperate and tropical Old World. The genus has an extensive Oligocene through Pleistocene fossil record in Eurasia. We survey the morphology of the extant and fossil fruits of the Alismataceae, and provide a detailed review of the morphology and anatomy of living and fossil Caldesia fruits. The latter exhibit substantial similarity, making the recognition of separate species on the basis of fruit morphology difficult. We erect the new species Caldesia brandoniana from the Early Miocene Brandon Lignite of Vermont primarily on the basis of its geographic isolation; careful revision of all fossil fruiting material of Caldesia might require placement of the Brandon specimens in a more inclusive form species. Together with leaves of Caldesia from the Miocene Clarkia flora of Idaho, this occurrence indicates that Caldesia was in the New World as recently as the Early Miocene.     

Paleobiochemistry of North American fossil Liriodendron sp.

Organic geochemical analyses are presented for a fossil Liriodendron sp. from the Miocene, Clarkia Flora of Northern Idaho. Flavonoid profiles determined for the fossil and two extent species of Liriodendron (L. chinense and L. tulipifera) confirm the generic status of the fossil material, but owing to a generic uniformity in flavonoid composition, fail to resolve taxonomic affinities at the species level. Steroid and other cycloalkane-alkene profiles indicate that the fossil taxon has a greater chemical similarity with L. chinense than L. tulipifera, despite the general leaf outline similarity between the fossil species and extent L. tulipifera. The morphologic and chemical data are interpreted as evidence for mosaic evolution within the genus, and the non-canalization of character states in some Miocene species.     

Leaf beds in the Early Miocene lacustrine deposits of the Geumgwangdong Formation,Korea: Occurrence,plant–insect interaction records,taphonomy and palaeoenvironmental implications

Occurrence, preservation and evidence of plant–insect interactions in the leaf deposits of the early Miocene Geumgwangdong Formation are described, and the taphonomy and palaeoenvironmental implications are interpreted. The Geumgwangdong leaf beds are tuffaceous lacustrine deposits consisting mainly of thin-bedded sediments, including shale. Deposition was dominated through the vertical aggradation of fine-grained sediments by suspension sedimentation, rather than by the fluvial deposition of coarse-grained sediments. The majority of the fossil leaves were preserved by compression rather than merely preserved as impressions. The Geumgwangdong leaf deposits can be characterised as a wind-transported, dysaerobic, deep-water, lake taphofacies with some influence of water-transport. The fossil flora of the Geumgwandong Formation consists of 64 taxa belonging to 27 families and 43 genera. The dominant taxa were Metasequoia, Fagus, Betula, Quercus, Acer, Zelkova, and Leguminosae, which is comparable to the Early Miocene cool–temperate Aniai-type Flora of north-east Japan. The similarity between the lake settings of the Geumgwangdong Formation and the Aniai Coal-bearing Formation might have been a factor in the development of similar plant–fossil assemblages. Although traces of insect damage in the fossil leaves of the Geumgwangdong Formation were commonly observed, more than 90% of the damaged leaves showed a low level of diversity and degree of insect damage (< 10%), which is indicative of a cool–temperate palaeoclimatic condition. Despite latitudinal differences and geographic separation, the development of similar floras in the Geumgwangdong Formation of south-east Korea and the Aniai Coal-bearing Formation of north-east Japan during the early Miocene could have been influenced by the incipient NW–SE sea-floor spreading that resulted in the opening of the East Sea (Sea of Japan), which might have enabled floral migration between the two regions. This study provides useful data for understanding not only the taphonomy and palaeoenviroments of the leaf deposits, but also the spatial development of the flora resulting from palaeogeographic changes driven by tectonic movement during the early Miocene in Far East Asia.     

An appraisal of the fossil record for the Cirolanidae (Malacostraca: Peracarida: Isopoda: Cymothoida), with a description of a new cirolanid isopod crustacean from the early Miocene of the Vienna Basin (Western Carpathians)

Abstract:  Isopod crustaceans are rarely preserved in the fossil record. Herein, an appraisal of the fossil record for the cirolanid isopods is presented. Five genera are briefly discussed, including Bathynomus, Brunnaega, Palaega, Pseudopalaega and Cirolana. A key for the cirolanid genera known to date from the fossil record is provided based mostly on pleotelson characters. From the early Miocene of the Slovak part of the Vienna Basin, Cirolana feldmanni sp. nov. is described being only the fifth fossil Cirolana species known to date and one of the few with preserved appendages. The material exhibits preservation suggesting biphasic moulting; the mode of preservation suggests a rather short time between shedding the posterior and anterior parts of the exoskeleton instead of hours or even days known in extant taxa. As no subsequent transport or physical disturbance was inferred, the specimens can be stated as in situ preservation. From the palaeoecological point of view, it is concluded that Cirolana feldmanni sp. nov. is the first unequivocal fossil deep‐water Cirolana as suggested by the accompanied fauna.     

Fossilization of melanosomes via sulfurization

Fossil melanin granules (melanosomes) are an important resource for inferring the evolutionary history of colour and its functions in animals. The taphonomy of melanin and melanosomes, however, is incompletely understood. In particular, the chemical processes responsible for melanosome preservation have not been investigated. As a result, the origins of sulfur‐bearing compounds in fossil melanosomes are difficult to resolve. This has implications for interpretations of original colour in fossils based on potential sulfur‐rich phaeomelanosomes. Here we use pyrolysis gas chromatography mass spectrometry (Py‐GCMS), fourier transform infrared spectroscopy (FTIR) and time of flight secondary ion mass spectrometry (ToF‐SIMS) to assess the mode of preservation of fossil microstructures, confirmed as melanosomes based on the presence of melanin, preserved in frogs from the Late Miocene Libros biota (NE Spain). Our results reveal a high abundance of organosulfur compounds and non‐sulfurized fatty acid methyl esters in both the fossil tissues and host sediment; chemical signatures in the fossil tissues are inconsistent with preservation of phaeomelanin. Our results reflect preservation via the diagenetic incorporation of sulfur, i.e. sulfurization (natural vulcanization), and other polymerization processes. Organosulfur compounds and/or elevated concentrations of sulfur have been reported from melanosomes preserved in various invertebrate and vertebrate fossils and depositional settings, suggesting that preservation through sulfurization is likely to be widespread. Future studies of sulfur‐rich fossil melanosomes require that the geochemistry of the host sediment is tested for evidence of sulfurization in order to constrain interpretations of potential phaeomelanosomes and thus of original integumentary colour in fossils.     

Flavonoids of fossil miocene Platanus and its extant relatives

Flavonoids of seven extant Platanus species and a fossil Platanus species from the Miocene Clarkia Flora of northern Idaho were compared. Sixteen flavonoids were isolated of which 15 were either wholly or partially identified. Flavonoids of Platanus are based on kaempferol and quercetin and most glycosides are linked at position 3. Because of an extremely high degree of overall chemical similarity and the presence of minor variation within some species, flavonoid data were of limited value in clarifying relationships among extant species. Flavonoid data suggest a closer chemical similarity of the fossil Platanus species to the Asiatic P. orientalis, rather than to the six investigated North American species. Morphologically, however, the fossil Platanus is very similar to P.occidentalis from eastern North America. These findings are similar to those reported in a paleobiochemical study of a fossil Liriodendron species from the same Miocene Flora.     

Reassembly of living cells from dissociated components in Bryopsis

Protoplasm from Bryopsis maxima, a coenocytic green alga, wasdissociated into two fractions: chloroplasts, and protoplasmicfraction without chloroplasts (PF). The protoplasmic fraction(PF) included nuclei, mitochondria, dictyosomes, endoplasmicreticuli, etc. These two fractions were reassembled and formedprotoplasts, which developed into mature plants. (Received June 9, 1977; )     

Palaeontological evidence for membrane fusion between a unit membrane and a half-unit membrane

Membrane fusion is of fundamental importance for many biological processes and has been a topic of intensive research in past decades with several models being proposed for it. Fossils had previously not been considered relevant to studies on membrane fusion. But here two different membrane fusion patterns are reported in the same well-preserved fossil plant from the Miocene (15–20 million years old) at Clarkia, Idaho, US. Scanning electron microscope, transmission electron microscope, and traditional studies reveal the vesicles in various states (even transient semi-fusion) of membrane fusion, and thus shed new light on their membrane structure and fusion during exocytoses. The new evidence suggests that vesicles in plant cells may have not only a unit membrane but also a half-unit membrane, and that a previously overlooked membrane fusion pattern exists in plant cells. This unexpected result from an unexpected material not only marks the first evidence of on-going physiological activities in fossil plants, but also raises questions on membrane fusion in recent plants.     

Paleontological evidence for membrane fusion between a unit membrane and a half-unit membrane

Membrane fusion is of fundamental importance for many biological processes and has been a topic of intensive research in past decades with several models being proposed for it. Fossils had previously not been considered relevant to studies on membrane fusion. But here two different membrane fusion patterns are reported in the same well-preserved fossil plant from the Miocene (15-20 million years old) at Clarkia, Idaho, US. Scanning electron microscope, transmission electron microscope, and traditional studies reveal the vesicles in various states (even transient semi-fusion) of membrane fusion, and thus shed new light on their membrane structure and fusion during exocytoses. The new evidence suggests that vesicles in plant cells may have not only a unit membrane but also a half-unit membrane, and that a previously overlooked membrane fusion pattern exists in plant cells. This unexpected result from an unexpected material not only marks the first evidence of on-going physiological activities in fossil plants, but also raises questions on membrane fusion in recent plants.     

PICEA WOLFEI,A NEW SPECIES OF PETRIFIED CONE FROM THE MIOCENE OF NORTHWESTERN NEVADA

Several silicified ovulate cones from the late middle Miocene (Barstovian) represent a new species, Picea wolfei Crabtree. This is the second species of Picea for which structurally preserved seed cones are known to be reported from the Tertiary. The cones are 5.0–8.0 cm long and 1.5–2.0 cm at their greatest diameter. Ovuliferous scales are inserted helically around the cone axis and are recurved at their point of divergence. Each scale is broadly obovate to spatulate with a rounded apex and bore two seeds adaxially. The bract subtending the scale is 4.5–7.3 mm long and is fused to the scale for 1.4–2.0 mm. Each bract has an inflated keel-like base which projects abaxially between the seeds of adjacent scales. The fossil cones superficially resemble those of the extant Picea breweriana, yet differ from them anatomically. The new species also resembles Picea lahontense, a fossil compression from the Miocene Trout Creek Flora of south-central Oregon, but the different modes of preservation preclude meaningful comparison. Picea diettertiana, the only structurally preserved fossil cone of this genus previously described, is quite dissimilar in that it lacks a sclerotic pith.     

云南中新世杉科化石木研究

利用光学显微镜和扫描电镜首次对云南省楚雄州晚中新世石灰坝组石鼓村层的钙化木材进行了解剖学研究.鉴定出两种类型的木材:柳杉型落羽杉型木(Taxodioxylon cryptomeripsoides Schonfeld)和杉木型落羽杉型木(Taxodioxylon cunninghamioides Watari).二者分别与现代柳杉属和杉木属具有最接近的亲缘关系.根据这两种杉科化石木现存最近亲缘种的生态环境,并综合其他资料,推测该地区在晚中新世为温暖湿润的亚热带气候环境.     

Cryopreservation of chloroplasts and thylakoids for studies of protein import and integration

A method is presented for preservation of isolated intact chloroplasts and isolated thylakoids for use in chloroplast protein import and thylakoid protein integration studies. Chloroplasts of pea (Pisum sativum) were preserved by storage in liquid nitrogen in the presence of a cryoprotective agent. Dimethyl sulfoxide was the most effective of several cryoprotectants examined. Approximately 65 to 70% of chloroplasts stored in liquid nitrogen in the presence of dimethyl sulfoxide remained intact upon thawing and were fully functional for the import of precursor proteins. Imported proteins were correctly localized within these chloroplasts, a process that for two of the proteins tested involved transport into the thylakoids. Lysate obtained from preserved chloroplasts was functional for protein integration assays. Preserved chloroplasts retained import and localization capability for up to 6 months of storage. Thylakoids were preserved by a modification of a method previously described (Farkas DL, Malkin S [1979] Plant Physiol 64: 942-947) for preservation of photosynthetic competence. Preserved thylakoids were nearly as active for protein integration studies as freshly prepared thylakoids. The ability to store chloroplasts and subfractions for extended periods will facilitate investigations of plastid protein biogenesis.     

Plant cytoplasm preserved by lightning

Usually only an organism with hard parts may be preserved in the fossil record. Cytoplasm, which is a physiologically active part of a plant, is rarely seen in the fossil record. Two Cretaceous plant fossils older than 100 million years with exceptional preservation of cytoplasm are reported here. Some cytoplasm is well preserved with subcellular details while other cytoplasm is highly hydrolyzed in the cortex of the same fossil even though both of preservations may be less than 2 microm away. The unique preservation pattern, sharp contrast of preservation in adjacent cells and the exceptional preservation of cytoplasm in the cortex suggest that lightning should play an important role in the preservation of cytoplasm and that cytoplasmic membranes may be more stable than the cell contents. Interpreting the preservation needs knowledge scattering in several formerly unrelated fields of science, including geophysics, botany, biophysics, cytology and microwave fixation technology. This new interpretation of fossilization will shed new light on preservation of cytoplasm and promote cytoplasm fossils from a position of rarity to a position of common research objects available for biological research. The importance of the identification of cytoplasm in fossil lies not in itself but in how much it influences the future research in paleobotany.     

LIGHT AND ELECTRON MICROSCOPIC OBSERVATIONS OF PREFERENTIAL DESTRUCTION OF CHLOROPLAST AND MITOCHONDRIAL DNA AT EARLY MALE GAMETOGENESIS OF THE ANISOGAMOUS GREEN ALGA DERBESIA TENUISSIMA (CHLOROPHYTA)1

Gametogenesis in male and female gametophytes was studied by light microscopy and EM in the dioecious multinucleate green alga Derbesia tenuissima (Moris & De Notaris) P. Crouan & H. Crouan, where male and female gametes differ in size. Gametogenesis was divided into five stages: 32 h (stage 1), 24 h (stage 2), 16 h (stage 3), 8 h (stage 4), and 0.5 h (stage 5) before gamete release. At stage 1, the first sign of gametogenesis observed was the aggregation of gametophyte protoplasm to form putative gametangia. At stage 2, gametangia were separated from the vegetative protoplasm of gametophytes. Morphological changes of nuclei and organelles occurred at this early stage of male gametogenesis, and organelle DNA degenerated. At stage 3, male organelle DNA had completely degenerated, whereas in female gametangia, organelle DNA continued to exist in both chloroplasts and mitochondria. Gametogenesis was almost completed at stage 4 and fully at stage 5. Small male gametes had a DNA‐containing nucleus and a large mitochondrion and one or several degenerated chloroplasts. The mitochondria and plastids were devoid of DNA. The large female gametes had a nucleus and multiple organelles, all of which contained their own DNA. Thus, degeneration of chloroplast DNA along with morphological changes of organelles occurred at male gametogenesis in anisogamous green algae (Bryopsis and D. tenuissima), in contrast with previous studies in isogamous green algae (Chlamydomonas, Acetabularia caliculus, and Dictyosphaeria cavernosa) in which degeneration of chloroplast DNA occurred after zygote formation.     

福建漳浦中中新世几种藓类植物研究*

亚洲新生代藓类植物化石非常稀少,漳浦琥珀是目前已知的我国低纬度地区唯一含苔藓植物化石的新生代琥珀矿床。漳浦琥珀源自中中新世气候适宜期(~14-17 Ma)的龙脑香树脂,温暖潮湿的热带季雨林气候和广泛分布的龙脑香科植物,为藓类植物的生长、多样性演化和三维立体保存提供了条件。本研究共报道了漳浦县中中新世藓类植物化石3个属种,包括:白发藓属Leucobryum Hampe、牛舌藓属Anomodon Hook.et Taylor和扁枝藓属Homalia(Brid.)B.S.G.。首次利用三维X射线断层扫描技术(Micro-CT)研究了白发藓属化石,发现其与现生种短枝白发藓Leucobryum humillimum Cardot非常相似,因此将其命名为短枝白发藓(相似种)Leucobryum cf.humillimum。此外,当前牛舌藓属Anomodon和扁枝藓属Homalia化石是东亚地区的首例记录。漳浦琥珀中的藓类植物化石揭示了中中新世时期苔藓植物的多样性,丰富了东亚低纬度地区新生代苔藓植物的化石记录。     

Reunification of sub-cellular fractions of bryopsis into viable cells

Protoplasm from Bryopsis maxima, a coenocytic green alga, was dissociated into two fractions; chloroplasts and a protoplasmic fraction without chloroplasts (PF). PF induced nuclei, mitochondria, dictyosome, endplasmic reticulum, etc. These two fractions were reunited and protoplasts with complete plasmamembrane were reformed within 10 h. Cell wall regeneration was observed 24–30 h after reuniting. New cells began budding 2–3 days after, and 1 month after reunification, they had developed into mature plants.     

玉米叶片原形成层细胞衰退过程的超微结构研究

在玉米（ＺｅａｍａｙｓＬ．）叶片原形成层发育的不同阶段常出现细胞衰退的现象,其衰退方式可分为自溶型和凝缩型。自溶型衰退的特点是细胞发生一系列降解活动最后导致细胞自溶死亡。衰退早期的细胞出现明显的自体吞噬活动,伴随核糖体和细胞质电子密度下降。衰退最后阶段的细胞自溶导致所有原生质组分的解体和消失,其中细胞核和质膜是最后消失的组分。凝缩型衰退的起动则伴随细胞质密度的增大。随着衰退的进行,原生质组分以一定顺序逐步退化解体：首先是高尔基体和内质网,接着是质体、细胞核和部分线粒体。但到衰退后期当细胞被挤压塌陷时仍有质膜、核糖体和线粒体存在。