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1.
Abstract:  The first lobopodian known from the Ordovician is described from the Soom Shale Lagerstätte, South Africa. The organism shows features homologous to Palaeozoic marine lobopodians described from the Middle Cambrian Burgess Shale, the Lower Cambrian Chengjiang biota, the Lower Cambrian Sirius Passet Lagerstätte and the Lower Cambrian of the Baltic. The discovery provides a link between marine Cambrian lobopodians and younger forms from the Silurian and Carboniferous. The new fossil preserves an annulated trunk, lobopods with clear annulations, and curved claws. It represents a rare record of a benthic organism from the Soom Shale, and demonstrates intermittent water oxygenation during the deposition of the unit.  相似文献   

2.
Visual organs are widely distributed throughout the animal kingdom and exhibit a great diversity of morphologies. Compound eyes consisting of numerous visual units (ommatidia) are the oldest preserved visual systems of arthropods, but their origins are obscure and hypothetical models for their evolution have been difficult to test in the absence of unequivocal fossil evidence. Here we reveal the detailed eye structures of well-preserved Early Cambrian lobopodians Luolishania longicruris and Hallucigenia fortis from the Chengjiang Lagerstätte, China. These animals possess a pair of eyes composed of at least two visual units, interpreted as pigment cups. Contrary to previous suggestions that Cambrian lobopodians possessed ocellus-like eyes comparable to those of extant onychophorans, this multi-component structure is more similar to the lateral eyes of arthropods. Morphological comparison and phylogenetic analyses indicate that these lobopodian eyes may represent an early stage in the evolution of the ancestral visual system of euarthropods.  相似文献   

3.
Burgess Shale-type deposits are renowned for their exquisite preservation of soft-bodied organisms, representing a range of animal body plans that evolved during the Cambrian ‘explosion’. However, the rarity of these fossil deposits makes it difficult to reconstruct the broader-scale distributions of their constituent organisms. By contrast, microscopic skeletal elements represent an extensive chronicle of early animal evolution—but are difficult to interpret in the absence of corresponding whole-body fossils. Here, we provide new observations on the dorsal spines of the Cambrian lobopodian (panarthropod) worm Hallucigenia sparsa from the Burgess Shale (Cambrian Series 3, Stage 5). These exhibit a distinctive scaly microstructure and layered (cone-in-cone) construction that together identify a hitherto enigmatic suite of carbonaceous and phosphatic Cambrian microfossils—including material attributed to Mongolitubulus, Rushtonites and Rhombocorniculum—as spines of Hallucigenia-type lobopodians. Hallucigeniids are thus revealed as an important and widespread component of disparate Cambrian communities from late in the Terreneuvian (Cambrian Stage 2) through the ‘middle’ Cambrian (Series 3); their apparent decline in the latest Cambrian may be partly taphonomic. The cone-in-cone construction of hallucigeniid sclerites is shared with the sclerotized cuticular structures (jaws and claws) in modern onychophorans. More generally, our results emphasize the reciprocal importance and complementary roles of Burgess Shale-type fossils and isolated microfossils in documenting early animal evolution.  相似文献   

4.
Paleontological data on the evolution of aquatic beetles are reviewed. A total of 37 beetle families are regarded as aquatic; five of them are extinct; three other extinct families could have had aquatic larvae; seven families are not known from the fossil record. The earliest records of fossil representatives of Recent families of aquatic beetles are given. The geological distribution of extinct families is reviewed, and the data on the modes of life of their representatives and on their evolution are provided. The new name Coleocatiniidae nom. nov. is proposed for Catiniidae Ponomarenko, 1968, a junior homonym of Catiniidae Embelton, 1901 (Crustacaea, Copepoda).  相似文献   

5.
The discovery of a new dyrosaurid crocodylomorph from the well-dated Palaeocene deposits of northeastern Brazil sheds new light on the evolutionary history of this extinct group of marine crocodylomorphs that have survived the Cretaceous-Palaeogene (K-P) extinction crisis. Guarinisuchus munizi, the most complete member of this group collected in South America so far, is closely related to the African forms, and this fact suggests that dyrosaurids had crossed the Atlantic Ocean before the K-P boundary and dispersed from there to North America and other parts of South America. This discovery also suggests that on the coast of northeastern Brazil, dyrosaurids replaced the pre-existing Late Cretaceous fauna of diversified mosasaurs, a group of marine lizards, after the K-P extinction event, becoming the main predators, together with sharks, in shallow marine Palaeocene environments. More detailed stratigraphic records and detailed dating of the deposits with dyrosaurids are necessary to correlate this particular pattern found in the ancient northeastern Brazilian coast within the evolution of the group, especially in Africa.  相似文献   

6.
The data on fossil platanoids and hamamelids are generalized, their morphological diversity and probable patterns of the establishment of the extant families Platanaceae and Hamamelidaceae are analyzed. It is shown that morphological and epidermal characters of polymorphic leaves of typical platanoid appearance were formed in the Late Albian and remained essentially invariable to the present time, indicating the morphological stasis of these leaves combined with a wide variation range. In view of association with essentially different reproductive structures, it is proposed to classify these leaves by the morphological system irrespective of the natural system of angiosperms. A new system of extinct platanoids and hamamelids, which is based on reproductive structures and includes two orders, Hamamelidales and Sarbaicarpales ordo. nov., is proposed. Hamamelidales comprises two extant families, Platanaceae (with the subfamilies Platanoideae subfam. nov. and Gynoplatananthoideae subfam. nov.) and Hamamelidaceae, and the extinct family Bogutchanthaceae fam. nov.; the new extinct order Sarbaicarpales ordo. nov. consists of two new families, Sarbaicarpaceae fam. nov. and Kasicarpaceae fam. nov. In a system of flowering plants that is based on molecular data, the families Platanaceae and Hamamelidaceae are assigned to remote orders, excluding close relationship (APG, 2003). At the same time, the system of APG II often contradicts morphological and paleontological data, while traditional ideas of morphologists concerning the common origin of these families have recently been supported by paleobotanic evidence. Probable origin of the families Platanaceae and Hamamelidaceae from a common polymorphic ancestral group is discussed.  相似文献   

7.
The Triassic marine reptiles at the base of the extinct Order Sauropterygia, traditionally known as nothosaurs, represent an unnatural assemblage of superficially similar forms. The traditional grouping of these animals has generally relied on the flawed basis of “primitive” characteristics whereas two distinct nothosaurian lineages can now be identified through the use of cladistic methodology. The Pachypleurosauria are the most plesiomorphic, but not the earliest, sauropterygians known. The Nothosauriformes include not only ‘nothosaurs’ but also the monophyletic group Plesiosauria and seemingly also the Placodontia. Rigorous coding of characters for the recently described nothosaurian genusSilvestrosaurus allows expansion of the phylogenetic data base for the Sauropterygia. The revised analysis reaffirms recent studies of relationship for the sauropterygians and demonstrates the affinity ofSilvestrosaurus with the Nothosauriformes. The explicit hierarchical classification scheme presented incorporates the hypothesized phylogenetic relationships of these long-misunderstood taxa. The traditional Suborder Nothosauria, now seen to be paraphyletic, must be abandoned.  相似文献   

8.
钙质红藻是指可以发生生物钙化作用在其细胞壁上沉淀碳酸钙的红藻。钙质红藻可以保存为化石,是红藻古生物研究中的重要类群,具有重要的生态意义,但以往的研究对钙质红藻类群的系统分类及地史分布缺乏清晰认识。本文详细综述了钙质红藻化石的系统分类,归属于红藻门(Rhodophyta)红藻纲(Rhodophyceae)的4个目7个科,分别为珊瑚藻亚纲(Corallinophycidae)珊瑚藻目(Corallinales)的珊瑚藻科(Corallinaceae)、石叶藻科(Lithophyllaceae)、宽珊藻科(Mastophoraceae)和管孔藻科(Solenoporaceae),混石藻目(Hapalidiales)的混石藻科(Hapalidiaceae),孢石藻目(Sporolithales)的孢石藻科(Sporolithaceae)以及真红藻亚纲(Florideophycidae)耳壳藻目(Peyssonneliales)的耳壳藻科(Peyssonneliaceae)。最早的钙质红藻为管孔藻科,出现于中奥陶世,于中新世灭绝。珊瑚藻科最早出现于晚志留世并于白垩纪辐射演化至今,其他科均于白垩纪...  相似文献   

9.
The netted dog whelk Nassarius reticulatus (Linnaeus, 1758), considered as an extinct benthic species in German Baltic waters, was found again alive in the Mecklenburg Bight during several macrozoobenthic surveys since 1997. All data indicate that the establishment of this marine prosobranch species is connected with the more frequent intrusions of highly saline water from the North Sea into the Baltic that have been observed over the past few years. It is proposed that N. reticulatus is a good bioindicator for the hydrographic status in the western Baltic rather than for other existing potential conditions. Since 1998 a second extinct marine species, the polychaete Scalibregma inflatum Rathke, 1843 was found alive here, too.Original English Text Copyright © 2005 by Biologiya Morya, Nehring.This article was submitted by the author in English.  相似文献   

10.
To investigate the affinities of snakes, amphisbaenians and dibamids, the phylogenetic relationships among the major lineages (families) of extinct and extant squamates are assessed through a combined analysis of 248 osteological, 133 soft anatomical, and 18 ecological traits. The osteological data set represents a revision of previous data, taking into account recent criticism; the ecological data set is new. In addition, potentially critical fossil taxa (polyglyphanodontids and macrocephalosaurs) are included for the first time. The osteological and soft anatomical data sets each place snakes within anguimorphs, with dibamids and amphisbaenians near gekkotans. The putative primitive fossil amphisbaenian Sineoamphisbaena groups with macrocephalosaurs and polyglyphanodontids, together the sister group to scleroglossans. All three data sets are congruent, and these results are reinforced by combined analyses. In these, as in the osteological analyses, snakes are nested within marine lizards. However, exclusion of fossil taxa from the osteological data set results in a ‘limbless clade’ consisting of snakes, amphisbaenians and dibamids, and introduces significant conflict between osteology and soft anatomy. Also, deletion tests and character weighting reveal that the signal in the reduced osteological data set is internally contradictory. These results increase confidence in the arrangement supported by the all-taxon osteological, the soft anatomical, and the combined data, and suggest that exclusion of fossils confounds the signal in the osteological data set. Finally, the morphological data support the nesting of snakes within marine lizards, and thus a marine origin of snakes. This result still holds when relationships between living forms are constrained to the topology suggested by molecular sequences: if marine lizards are allowed to ‘float’ within this molecular framework, they form the stem group to snakes, and do not group with varanids as previously suggested.See also Electronic Supplement at: http://www.senckenberg.de/odes/05-04.htm.  相似文献   

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