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1.
The article reports the finding of some late Paleocene (Thanetian) species of Phaeodarian Radiolaria in phosphorite concretions occurring in the Holmehus Formation of Denmark. These species are associated with a rich assemblage of diatoms and sparse spherical radiolarians. Phaeodarians are very well-preserved in celestobarite (BaSrSO4) and consist of representatives of the families Challengeridae (Challengerebium triangulovum nov. sp. and Challengerebium sp.) and particularly Medusettidae (Medusetta danica nov. sp. and M. densicostata nov. sp.), which are the most frequent. A new genus of medusettid phaeodarians (Pseudochallengeranium nov. gen.) is also described. 相似文献
2.
Abstract: A new species of the genus Epiphaxum (family Lithotelestidae) is described and illustrated in detail, and compared to other species. Epiphaxum arbuscula sp. nov. has been collected from Upper Eocene (Priabonian), Upper Oligocene (Chattian) and Lower Miocene (Upper Burdigalian) deposits of the Aquitaine Basin, south-west France. Epiphaxum is a poorly documented genus but its fossil record extends back to the Late Cretaceous; it was previously known only from the Paleocene (Danian). Epiphaxum arbuscula differs from all others species of the genus in the form of its colony. In contrast to the creeping colonies of previously known species, it has branched colonies. It is very common at one Upper Oligocene outcrop from which an assemblage with submarine cave remains has been described. A close relationship between the three extant species (two from the Caribbean Sea and one from the Indo-West Pacific region) and the Paleogene species is also noted. These constitute a group that has not undergone any important morphological changes for the last 65 million years. 相似文献
3.
- 1 The history of a forest stand over the last 6000 years has been reconstructed by studying pollen, macrofossils and charcoal from a small, wet hollow in Suserup Skov on the island of Sjælland in eastern Denmark.
- 2 The earliest recorded forest was Tilia‐dominated but contained an intimate mixture of many different tree species that included Acer campestre, A. platanoides, Alnus glutinosa, Betula pubescens, Corylus avellana, Frangula alnus, Fraxinus excelsior, Malus sylvestris, Populus tremula, Pinus sylvestris, Quercus robur, Q. petraea, Salix spp., Sorbus aucuparia, Tilia cordata and T. platyphyllos. The preserved fruits of T. platyphyllos confirm its hitherto doubtful status as a native member of the Danish flora.
- 3 The present‐day woodland developed after a period of intensive anthropogenic disturbance between ≈ 600 bc and ad 900, during which time open canopy conditions prevailed at Suserup. Fagus sylvatica and Fraxinus excelsior are the dominant trees at present, together with some Quercus robur and Ulmus glabra. 4 Charcoal was present in the sediments from most time periods except at the Ulmus decline. In the last 1000 years of the sequence — the period of Fagus dominance — charcoal counts were consistently low.
- 5 Pinus sylvestris was a natural component of this primarily deciduous forest, and the last macrofossil find dates from c. ad 900. Macrofossil Pinus cone scales recorded c. ad 1800 originate from planted individuals. Prior to Fagus dominance, the forest had an open structure partly caused by frequent, low‐intensity fires associated with the presence of Pinus sylvestris.
- 6 The replacement of Tilia by Fagus in this forest was catalysed by human activity. If the forest had not been so disturbed, the rich diversity of trees would most probably have persisted up to the present time, with only a moderate‐sized Fagus population.
4.
Deutsch JS 《Development genes and evolution》2006,216(7-8):357-362
In the present essay, I first recall the genealogical concept of classification settled by Charles Darwin in the Origin of Species. Darwin tightly linked what we now call phylogeny and development. He often insisted to take into account embryonic and larval characters, most often using as examples his favourite animals, the cirripedes. Then I discuss remaining problems, and also perspectives, to address the link between phylogeny and development in the modern terms of molecular and cladistic phylogenetics and of molecular and genetic developmental biology. 相似文献
5.
Jean Deutsch 《Comptes rendus biologies》2010,333(2):99-106
In this essay, I discuss the origin of Charles Darwin's interest in cirripedes (barnacles). Indeed, he worked intensively on cirripedes during the years in which he was developing the theory that eventually led to the publication of The Origin of Species. In the light of our present knowledge, I present Darwin's achievements in the morphology, systematics and biology of these small marine invertebrates, and also his mistakes. I suggest that the word that sheds the most light here is homology, and that his mistakes were due to following Richard Owen's method of determining homologies by reference to an ideal archetype. I discuss the ways in which his studies on cirripedes influenced the writing of The Origin. 相似文献
6.
Pachycondyla rebekkae sp. nov. (Formicidae, Ponerinae) is described from the Fur and Ø1st Formations (transitional between Paleocene and Eocene, Denmark). About 95 complete or fragmentary gyne specimens and one almost complete male specimen were examined, revealing characters which permit classification and placement of the fossil species in the phylogenetic system of extant Formicidae. The palaeoecology and taphonomy of the insect fauna of the Fur and Ø1st Formations are discussed. Finally, the significance of the new species is discussed in light of the fossil history and early evolution of ants. 相似文献
7.
William I. Ausich David F. Wright Selina R. Cole George D. Sevastopulo 《Palaeontology》2020,63(4):525-545
Despite their importance for understanding phylogeny, character evolution and classification, well-constrained homology relationships for posterior plating in crinoids have only recently been attempted. Here, we re-evaluate posterior plate homologies in all major crinoid lineages using development, fossil ontogenies and phylogenetic evidence. Based on these lines of evidence, we change terminology for some posterior plates to correct misnomers and make recommendations for updated terminology of others to better reflect homology. Among pentacrinoids (disparids, hybocrinids, eucladids, flexibles and articulates) the relative position of posterior interray plates, not their topology, reflects homology. From proximal to distal, pentacrinoid posterior plates are the radianal, anal X and right sac plate, regardless of the total number of plates in the adult calyx. Camerate posterior plating contrasts with pentacrinoids, but insufficient data are available to resolve homology relationships between these two clades. More examples of early post-larval ontogeny are needed in camerates and other Palaeozoic crinoids. 相似文献
8.
JAMES SPRINKLE DESMOND COLLINS 《Lethaia: An International Journal of Palaeontology and Stratigraphy》1998,31(4):269-282
Echmatocrinus from the Middle Cambrian Burgess Shale of British Columbia was originally described as the earliest crinoid(?) known from the fossil record. Recently, Conway Morris and Ausich & Babcock have questioned whether Echmatocrinus is in fact an echinoderm, comparing it instead to cnidarians with a polyp-like body and pinnate tentacles, and other authors are beginning to use this reinterpretation. We studied the well-preserved holotype of Echmatocrinus brachiatus, two paratypes, and 18 new specimens recovered from different levels in the Burgess Shale sequence at three localities. All are preserved as pyrite films in dark shale with relatively little relief, suggesting a lightly skeletized body. Complete specimens have a long, slightly tapering, large-plated attachment stalk, a conical cup or calyx with numerous small to medium-sized irregular plates, and 7–10 short arms with heavier plating and (in the holotype) soft appendages alternating from opposite sides of several arms. Several morphologic features indicate that Echmatocrinus is an echinoderm and has crinoid affinities: (1) Sutured plates, shown by darker depressed sutures, slightly raised plate centers, and oriented plate ornament, cover all major parts of the body; (2) reticulate surface ornament in the pyrite film on the plates of all specimens matches the ornament in the Burgess Shale edrioasteroid Walcottidiscus, an undoubted echinoderm, but not the pyritized surfaces of other metazoans in the fauna; (3) this distinctive ornament may represent the surface expression of microporous stereom; (4) possible ligament or muscle pads are present between the arm ossicles to fold and unfurl the more heavily plated arms. Within the echinoderms, only crinoids commonly have a calyx attached by a stalk or stem to the substrate and bear erect, moveable, uniserial arms for feeding. Although Echmatocrinus shows some resemblance to octocorals in overall body shape as an attached suspension feeder, almost all the details are different, indicating that Echmatocrinus is most likely unrelated to this group. All complete specimens of Echmatocrinus are attached to hard substrates, either another fossil or skeletal debris. The new specimens indicate that Echmatocrinus was twice as common (about 0.02%) in the Burgess Shale fauna as previously recorded and represents one of the earliest attached, medium-level, skeletized, suspension feeders or microcarnivores in the fossil record. 相似文献
9.
E. David Morgan Colin R. Bielby Ian D. Wilson 《Journal of experimental marine biology and ecology》2005,321(2):125-134
An analytical procedure for the quantification of ecdysteroids (crustacean moulting hormone) in barnacles was devised so that minimum sample size could be used. A combination of solvent partitions, Sephadex chromatography, silylation and gas chromatography with electron capture detection was devised, enabling ecdysteroids to be determined down to 20 pg. This was used to determine the amount of moulting hormone in a population of barnacles over a 30 month period. Levels varied from barely detectable in winter months to a maximum value of 1.5 μg kg− 1 of wet weight of barnacles in September. Polar conjugates of 20-hydroxyecdysone were detected only during the winter months. The number of barnacles moulting at any time corresponded roughly to the titre of hormone present at that time. 相似文献
10.
Abstract: A systematic account of highly diverse cyrtocrinid faunules from Upper Jurassic strata of ?tramberk type (Oxfordian–Tithonian) in southern Poland (Polish Carpathians) is presented. Fourteen taxa (Phyllocrinus malbosianus, Ph. stellaris, Ph. sp., Psalidocrinus armatus, Sclerocrinus compressus, S. polonicus sp. nov., Hemicrinus aff. kabanovi, Ancepsicrinus parvus gen. et sp. nov., Tetracrinus baumilleri sp. nov., Eugeniacrinites alexandrowiczi, E. cf. moravicus, E. sp., Eudesicrinus gluchowskii sp. nov. and Hemibrachiocrinus tithonicus sp. nov. are described and illustrated. Representatives of the genus Eudesicrinus, previously recorded only from the Lower Jurassic, are here shown to extend into the uppermost Jurassic. Other cyrtocrinids considered are common in Jurassic/Cretaceous strata across Europe. In the present faunules, isocrinid (Isocrinida), comatulid (Comatulida) and roveacrinid (Roveacrinida sensu Rasmussen, inclusive of Saccocoma) crinoids are associated. 相似文献
11.
Mariusz A. Salamon 《Pal?ontologische Zeitschrift》2008,82(3):269-278
Callovian strata in northern Lithuania (Papilė area) have yielded some crinoid taxa[Chariocrinus andreae (Desor),Balanocrinus berchteni Hess —Pugin,B. subteres (Münster inGoldfuss) andIsocrinus nicoleti (Desor)], which have not been described from this area. The only form known previously wasBalanocrinus pentagonalis (Goldfuss).Palaeocomaster jaegeri n. sp. is the first free-living crinoid recorded from the Callovian of eastern Europe. It is characterized by possessing a very low, strongly flattened and narrow radial cavity. A very similar crinoid assemblage is known from the Callovian glacially-derived clays exposed in the Łuków region (eastern Poland), which were originally located near the Baltic Sea during the Middle Jurassic. It is considered that the allochthonous Callovian deposits from Poland are facies equivalents of the deposits known from Lithuania. The sole significant exception is the domination of free-moving comatulids (Comatulida) in the sediments known from the Papilė region, which may suggest that the Lithuanian sea basin was a little shallower than that located farther west in the Baltic area. 相似文献
12.
Floréal Solé Jocelyn Falconnet Laurent Yves 《Zoological Journal of the Linnean Society》2014,171(4):878-917
We describe six proviverrine species from the Early Eocene of France. Three species are new: M inimovellentodon russelli sp. nov. from Mutigny [mammal palaeogene (MP)8 + 9], B oritia duffaudi sp. nov. from La Borie (MP8 + 9), and L eonhardtina godinoti sp. nov. from Grauves (MP10). We describe new specimens and propose new generic combinations for three species from MP10: Protoproviverra palaeonictides, Matthodon menui, and Oxyaenoides lindgreni. We also propose a new generic combination for the primitive Eoproviverra eisenmanni (MP7). Matthodon menui was previously considered as a possible oxyaenodontan, but the new fossils clearly support its reference to Hyaenodontida. Leonhardtina godinoti and Ma. menui are the oldest occurrences for these genera, which were previously unknown before the Middle Eocene. Moreover, the discovery of the proviverrine Mi. russelli in Mutigny implies that the Proviverrinae dispersed in Northern Europe between biozone Palaeocene‐Eocene (PE) III (Abbey Wood) and biozone PE IV (Mutigny). This also supports a homogenization of the European faunas during the Early Eocene. The dispersal is concomitant with the disappearance of the oxyaenodontans, arfiines, and sinopines (Hyaenodontida) from Europe. The proviverrines may have filled the ecological niches left vacant by the disappearance of the other carnivorous mammals. With 20 genera and over 30 species, proviverrines were successful in Europe. We performed the first phylogenetic analysis comprising almost all the Proviverrinae. Our analyses indicate that the Proviverrinae diversified greatly during the Early Eocene Climatic Optimum and show a general trend towards specialization throughout the Eocene. © 2014 The Linnean Society of London 相似文献
13.
F. W. E. ROWE A. K. HOGGETT R. A. BIRTLES† L. L. VAIL 《Zoological Journal of the Linnean Society》1986,86(3):197-277
Morphological characters used in comasterid taxonomy are reappraised. As a result, form and distribution of pinnule combs are newly promoted as primary characters of generic recognition. Form and arrangement of cirri and division series, as used by A. H. Clark (1931), are rejected as characters important in recognizing taxa higher than species. Five of 12 comasterid genera reported as occurring in Australian waters (H. L. Clark, 1946) are critically examined. Of these genera, Comantheria A. H. Clark, 1909b is referred to the synonymy of Comanthus A. H. Clark, 1908a, Comanlhoides A. H. Clark, 1931 is referred to the synonymy of Cenolia A. H. Clark, 1916b, and Comanthina A. H. Clark, 1909b is maintained. In addition, two new genera are described. These genera are related by the occurence of the first brachial syzygy at 3 + 4 on all arms. Twenty-six species within the five genera are now recognized in Australian waters. Nine new species are described, and the 17 existing species are rediagnosed and critically reappraised. The revision involves taxa distributed throughout the Indo-west Pacific region, as far west as S Africa. 相似文献
14.
Early Permian crinoids and blastoids from Oman show relationship with Late Paleozoic Tethyan faunas of Timor and Western Australia and support an Early Permian age for part of the Basleo fauna of Timor. The camerate crinoidPlatycrinites omanensis n. sp. and the blastoidsTimoroblastus andDeltoblastus are reported for the first time from Sakmarian strata of northeastern Oman, doubling the known Permian echinoderms from Oman. The blastoids suggest an offshore lower energy shelf environment of deposition. 相似文献
15.
古新世晚期裂齿类———丁氏豫裂兽 (新属、新种 ) (Yuesthonyxtingaegen .etsp .nov.)的发现表明了裂齿目在亚洲古新世已相当分化 ,在臼齿形态上有与北美始新世Esthonyx相近的小尖兽 (Meiostylogon)和中间兽 (Interogale) ,也有与北美Megalesthonyx接近的豫裂兽等。根据豫裂兽、Megalesthonyx、和亚洲的Adapidium的上臼齿都具有明显的中附尖等特征可与其他裂齿类相区别 ,新建了豫裂兽科 (YuesthoncidaeFam .nov.)。 相似文献
16.
中国东北古新世乌云植物群：榆科叉脉榆 总被引：1，自引：0，他引：1
根据叶结构特征。将黑龙江省古新世乌云植物群中的榆科叶化石确定为叉脉榆（Umus furcinervis(Borsuk)Ablaev)。叶化石二级脉达缘且在叶缘区分叉,三级脉及顶,叶缘锯齿两侧边凸出。重新研究了前人鉴定为小叶普拉榆（Planera cf.microphylla auct.non Newberry)和乌云珍珠梅（Sorbaria wuyungensis Tao et Xiong)的叶化石并将其归入叉脉榆。 相似文献
17.
JAMES D. ECKERT 《Lethaia: An International Journal of Palaeontology and Stratigraphy》1988,21(2):147-167
After reaching a diversity peak in the Caradocian, North American Ordovician crinoids underwent a gradual decline to a nadir in the early Ashgillian (Maysvillian). This interval, recording extinction of the Cleiocrinidae, Merocrinidae, Ottawacrinidae, Hybocystitidae, and several lineages of camerate crinoids, was apparently caused by major environmental shifts in seas of eastern North America resulting from a westward-prograding wedge of terrigenous clastics derived from the Taconic Highlands, possibly coupled with a marine transgression in the Maysvillian that allowed colder water slope biofacies to invade the craton. Crinoids suffered a major episode of extinction in the late Ashgillian (late Richmondian/Rawtheyan). This event, preceding the end of the Ordovician by at least one stage or 2 to 4 million years, resulted in extinction of 12 families of crinoids including the Xenocrinidae, Tanaocrinidae, Reteocrinidae, Archaeocrinidae, Anthracocrinidae, Cincinnaticrinidae, Iocrinidae, Anomalocrinidae, Carabocrinidae, Cupulocrinidae, Porocrinidae, and Hybocrinidae. Glacio-eustatic lowering of sea level may have triggered this crisis by partially draining the North American craton, resulting in changes in oceanic circulation, salinity, and temperature. Latest Ordovician (Hirnantian) carbonates of the North American mid-continent region contain pelmatozoan assemblages from which Silurian crinoids radiated. These taxa were largely unaffected by a minor extinction event at the Ordovician/Silurian boundary. 相似文献
18.
根据叶结构特征,将黑龙江省古新世乌云植物群中的榆科叶化石确定为叉脉榆(Ulmus furcinervis (Borsuk) Ablaev),叶化石二级脉达缘且在叶缘区分叉、三级脉及顶、叶缘锯齿两侧边凸出.重新研究了前人鉴定为小叶普拉榆(Planera cf. microphylla auct. non Newberry)和乌云珍珠梅(Sorbaria wuyungensis Tao et Xiong)的叶化石并将其归入叉脉榆. 相似文献
19.
描述并厘定了黑龙江省嘉荫县古新世乌云植物群中的广义山茱萸科绝灭类型镘形美中果 (Amersiniaobtrul lataManchester,CraneetGolovneva)和假古老白令叶 (Beringiaphyllumpseudoantiquum (Golovneva)Manchester,CraneetGolovneva)。将前人鉴定为昆栏树属 (未定种 ) (Trochodendronsp .)的果序化石归入镘形美中果 ;将前人确定为鲜艳杨 (Populuscarneosa)、假原始叶南蛇藤 (Celastrophyllumsubprotophyllum)、古老荚 (Viburnumantiquum)、粗糙荚 (V .asperum)、疏齿荚叶 (Viburniphyllumfinale)、乌云原始叶 (Potophyllumwuyunense)、海丹原始叶 (近似种 ) (P .cf.hay denii)、卵圆原始叶 (P .ovatifolium)和不规则克里木 (Credneriainordinata)等归入假古老白令叶 相似文献
20.
Fossil seeds and seedlings of a Metasequoia-like taxodiaceous conifer occur in Paleocene deposits at the Munce's Hill and Gao Mine localities of central Alberta, Canada. Compression/impression specimens are preserved in upright growth positions among seedlings of the cercidiphyllaceous dicot Joffrea speirsii Crane & Stockey. There are a large number of seeds, a few of which were buried while germinating and show a radicle or short primary root. More than 500 Metasequoia-like seedlings have been identified that have two linear cotyledons with parallel margins and rounded tips. Three specimens have been found that display three cotyledons. Slightly older seedlings show decussate pairs of leaves attached to the stem distal to the cotyledons. Still older seedlings have axillary branches that show varying sizes and numbers of opposite leaves arranged in a single plane distal to the opposite pairs. These specimens reveal that both Joffrea and this extinct taxodiaceous conifer were early colonizers of North American floodplain communities at the beginning of the Tertiary. 相似文献