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Tytuł:
New insights into the origin and relationships of blastoid echinoderms
Autorzy:
Paul, C.R.C.
Powiązania:
https://bibliotekanauki.pl/articles/2082286.pdf
Data publikacji:
2021
Wydawca:
Polska Akademia Nauk. Instytut Paleobiologii PAN
Tematy:
Blastozoa
Glyptocystitoida
Hemicosmitoida
Coronata
Blastoidea
homology
phylogeny
ontogeny
Opis:
“Pan-dichoporites” (new informal term) is proposed to unite Cambrian blastozoans, such as Cambrocrinus, Ridersia, and Sanducystis, glyptocystitoid and hemicosmitoid rhombiferans, coronates, blastoids, and Lysocystites. Pan-dichoporite ambulacra have double biserial main axes with brachiole facets shared by pairs of floor (glyptocystitoids), side (blastoid) or trunk (hemicosmitoids, coronates) plates. These axial plates are the first two brachiolar plates modified to form the ambulacral axes. In glyptocystitoids the first brachiole facet in each ambulacrum is shared by an oral and another plate. Hence, these are also two modified brachiolar plates and part of the axial skeleton under the Extraxial Axial Theory (EAT). Pan-dichoporites are also characterized by thecae composed of homologous plate circlets. The unique glyptocystitoid genus Rhombifera bears ambulacral facets on five radial plates, which alternate with five orals. The oral area of Lysocystites (blastoid sensu lato) is very similar, which suggests that rhombiferan radials are homologous with “ambulacrals” of Lysocystites and hence with blastoid lancet plates. This implies derivation of blastoids from glyptocystitoids and suggests that blastoid and coronate radials and deltoids are homologous with rhombiferan infralaterals and laterals. Thus, homologous plate circlets occur in all pan-dichoporites, which strengthens the validity of a pan-dichoporite clade. Under Universal Elemental Homology (UEH), deltoids were homologized with rhombiferan orals, but this is inconsistent with the EAT. Deltoids bear respiratory pore structures and so are perforate extraxial skeletal plates, whereas rhombiferan orals are axial skeleton. The new plate homologies also explain why only five plates form the oral frames of coronates, blastoids and Lysocystites, whereas glyptocystitoids (except Rhombifera) have six oral frame plates; all glyptocystitoids have only five laterals. Hemicosmitoids arose by paedomorphic ambulacral reduction, but the paedomorphosis also affected the thecal plates and stem. Paedomorphosis poses special problems for cladistic character analysis, since the new characters often appear to be plesiomorphic.
Źródło:
Acta Palaeontologica Polonica; 2021, 66, 1; 41-62
0567-7920
Pojawia się w:
Acta Palaeontologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Anatomical distinctions of the Mesozoic lingulide brachiopods
Autorzy:
Biernat, G
Emig, C.C.
Powiązania:
https://bibliotekanauki.pl/articles/23486.pdf
Data publikacji:
1993
Wydawca:
Polska Akademia Nauk. Instytut Paleobiologii PAN
Tematy:
Lingularia smirnovae
mezozoik
trias
skamienialosci
jura
Brachiopoda
muszle
Lingularia sibirica
lingule
ewolucja
kreda
morfologia
Lingula
Lingularia
Lingularia similis
paleontologia
Glottidia
Opis:
The long held view that Lingula represents an extremely bradytelic lineage is questioned. Examination of Mesozoic lingulides has shown that they significantly differ from their Recent relatives Lingula and Glottidia in having longer lophophoral cavities, shorter ventral canals, better developed posterior adductor muscles, and less acute umbones. Morphological characters of the shell interior are needed to identify members of the Lingulidae, not solely external shell characteristics. The apparent evolutionary tendency towards a reduction of the volume of the lophophoral cavity contradics the traditional view that the ‘living fossil’ Lingula has survived without significant morphological change since the Paleozoic. Actually the today living lingulide genera probably arose in the early Cenozoic. A new inarticulate brachiopod genus, Lingularia is introduced, with three new species. Middle Triassic L. siberica, Middle Jurassic L. similis, and Cretaceous L. smirnovae.
Badania dobrze zachowanych okazów mezozoicznych lingul wskazały, że te różnią się zasadniczo od współczesnych rodzajów Ligula i Glottidia objętością jamy lofoforalnej, długością kanałów wentralnego płaszcza, wykształceniem nieparzystego mięśnia tylnego adduktora oraz, dodatkowo, morfologią części dziobowych muszli. Zaznaczająca się tendencja ewolucyjna w kierunku redukcji objętości jamy lofoforalnej przeczy ogólnie przyjętemu poglądowi, że Lingula to „żyjąca skamieniałość”, która przeżyła, od wczesnego paleozoiku do dzisiaj, prawie bez zmian morfologicznych. W pracy wyodrębniono nowy rodzaj Lingularia z 3-ma nowymi gatunkami: L. sibirica (trias), L. similis (jura), L. smirnovae (kreda).
La traditionnelle opinion que Lingula représente une lingée très ancienne est remise en question. L’étude de lingules mésozoïques démontre que celles-ci diffèrent significativement des genres actuels Lingula et Glottidia par une cavité lophophorale plus volumineuse, des canaux ventraux du manteau plus courts, un développement plus important du muscle adducteur postérieur, les régions umbonales. Les caractères morphologiques internes s’avèrent indispensables pour pouvoir identifier les genres et espèces des Lingulidae, les caractères externes de la coquille étant insuffisants. La tendance évolutive d’une réduction de la cavité lophophorale s’oppose à l’opinion traditionnellement véhiculée que le genre fossile-vivant Lingula a survécu sans modification morphologique significative depuis le début du Paléozoïque: en fait, l’origine des lingules actuelles date probablement du début du Cénozoïque. Un nouveau genre de brachiopode inarticulé, Lingularia, est décrit avec trois nouvelle espèces, L. siberica (Trias Moyen), L. similis (Jurassique Moyen) et L. smirnovae (Crétacé).
Źródło:
Acta Palaeontologica Polonica; 1993, 38, 1-2; 1-20
0567-7920
Pojawia się w:
Acta Palaeontologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The Upper Triassic flora of Svalbard
Autorzy:
Pott, C.
Powiązania:
https://bibliotekanauki.pl/articles/945880.pdf
Data publikacji:
2014
Wydawca:
Polska Akademia Nauk. Instytut Paleobiologii PAN
Tematy:
paleobotany
Triassic
Upper Triassic
flora
Bennettitales
Asterotheca
Neocalamites
Pterophyllum
Paratatarina
Carnian
Svalbard
Spitsbergen
Opis:
The Triassic plant fossils from the Svalbard archipelago are comprehensively reviewed. The poorly known flora is widespread and has been recovered from all Triassic exposures in the archipelago; 24 species are identified and one new species, viz. Arberophyllum substrictum, is described. The flora consists of sphenophytes, ferns, cycadophytes, and putative ginkgophytes and seed ferns. Ferns and Bennettitales are the dominant elements. The composition of the flora is strikingly similar to the Carnian flora of Lunz in Lower Austria, sharing an unexpectedly large number of taxa, and thus, it is proposed that most of the fossils derive from the De Geerdalen Formation, which is dated as Carnian. Key taxa in the Svalbard flora are Asterotheca, Neocalamites, Pterophyllum, and Arberophyllum. The floristic composition and sedimentology of the host strata suggests that the flora thrived in a coastal lagoonal/deltaic environment. The similarity of the Svalbard and Lunz floras argues that the North Atlantic floral sub-province hypothesised for the Rhaetian in this region was already established by the Carnian.
Źródło:
Acta Palaeontologica Polonica; 2014, 59, 3; 709-740
0567-7920
Pojawia się w:
Acta Palaeontologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Reassessment of the generic attribution of Numidotherium savagei and the homologies of lower incisors in proboscideans
Autorzy:
Delmer, C.
Powiązania:
https://bibliotekanauki.pl/articles/21470.pdf
Data publikacji:
2009
Wydawca:
Polska Akademia Nauk. Instytut Paleobiologii PAN
Tematy:
generic attribute
Numidotherium savagei
lower incisor
proboscidean
Proboscidea
Barytherium
Elephantiformes
phylogenesis
Paleogene
Libya
Eocene
Oligocene
Opis:
Near the end of the twentieth century, a medium−sized early proboscidean found in Dor El Talha (late Eocene to early Oligocene), Libya, originally identified as a small species of Barytherium, was described as a new species of Numidotherium and designated Numidotherium savagei. Poorly known, this taxon has been excluded from most of the recent debate about the origin and diversification of the order Proboscidea. New specimens described herein show strong structural similarities of the upper teeth with those of bunolophodont early proboscideans (e.g., Moeritherium and Phiomia) and document the shared presence of derived traits in the postcranial skeleton. The newly referred material also demonstrates some unique characteristics of this taxon, notably in its mandibular morphology and the microstructure of its dental enamel. Included for the first time in a cladistic analysis (207 anatomical characters applied to all early tethytheres), N. savagei is distinct from both Numidotherium and Barytherium, and lies in an “intermediate” position between the strictly lophodont Eocene proboscideans and the bunolophodont moeritheres and elephantiforms. Accordingly, the species is herein referred to a new genus, Arcanotherium. New data on its mandibular symphysis and, especially, on its lower incisors loci and morphology, bring new support to a hypothesis of homology between the lower incisors of early proboscideans and the ever−growing lower tusks of the elephantiforms, which are identified here as di1 and i1.
Źródło:
Acta Palaeontologica Polonica; 2009, 54, 4
0567-7920
Pojawia się w:
Acta Palaeontologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Halina Pugaczewska [1921-1997]
Autorzy:
Kulicki, C.
Powiązania:
https://bibliotekanauki.pl/articles/21589.pdf
Data publikacji:
1997
Wydawca:
Polska Akademia Nauk. Instytut Paleobiologii PAN
Tematy:
Belemnitida
fauna
biography
paleobiology
geology
Jurassic belemnite
Pugaczewska Halina biography
paleontology
Źródło:
Acta Palaeontologica Polonica; 1997, 42, 4
0567-7920
Pojawia się w:
Acta Palaeontologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Morphological disparity in Plio-Pleistocene large carnivore guilds from Italian Peninsula
Autorzy:
Meloro, C.
Powiązania:
https://bibliotekanauki.pl/articles/22061.pdf
Data publikacji:
2011
Wydawca:
Polska Akademia Nauk. Instytut Paleobiologii PAN
Tematy:
Carnivora
Italian Peninsula
Italy
morphological diversity
Pleistocene
Plio-Pleistocene
Quaternary
geometrical morphometry
large mammal
mandible shape
paleontology
morphological variability
taxonomy
Opis:
Communities of large mammals exhibit changes in morphological diversity through space and time; changes that are possibly correlated to distinct aspects of the physical environment. Here, I explore shape changes in the trophic apparatus of large carnivore guilds, comparing extant communities with Quaternary ones, from peninsular Italy. Mandibular shape is quantified through geometric morphometrics and its disparity is computed for each carnivore guild. Patterns of morphospace occupation through space and time reveal that extant carnivore guilds are negatively influenced by number of artiodactyls. Very productive ecosystems show low values of morphological disparity because species tend to occupy central regions of the morphospace rather than extreme areas. Disparity of mandibular corpus shape remains relatively stable throughout the Quaternary in the large carnivore communities of the Italian peninsula. They exhibit similar values to extant guilds because the trophic apparatus did not evolved important morphological novelties. Interestingly, carnivore guilds of the late Pliocene (3.5 Ma) and early Pleistocene (0.8 Ma) show over−dispersed or random morphospace occupation because of a depleted fauna, precluding successive structural changes. The same applies for the extant European carnivore guild as a result of recent extinctions without replacement.
Źródło:
Acta Palaeontologica Polonica; 2011, 56, 1
0567-7920
Pojawia się w:
Acta Palaeontologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
New observations on Rhabdopleura kozlowskii (Pterobranchia) from the Bathonian of Poland
Nowe obserwacje nad Rhabdopleura kozlowskii (Pterobranchia) z batonu Polski
Novye dannye o Rhabdopleura kozlowskii (Pterobranchia) iz batskoga jarusa Polkhi
Autorzy:
Kulicki, C.
Powiązania:
https://bibliotekanauki.pl/articles/22539.pdf
Data publikacji:
1971
Wydawca:
Polska Akademia Nauk. Instytut Paleobiologii PAN
Źródło:
Acta Palaeontologica Polonica; 1971, 16, 4
0567-7920
Pojawia się w:
Acta Palaeontologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The brachiopod Lingula in the Middle Miocene of the Central Paratethys
Autorzy:
Emig, C C
Bitner, M.A.
Powiązania:
https://bibliotekanauki.pl/articles/20475.pdf
Data publikacji:
2005
Wydawca:
Polska Akademia Nauk. Instytut Paleobiologii PAN
Tematy:
Lingula dregeri
Miocene
brachiopod
Middle Miocene
deposit
Lingula dumortieri
paleontology
Lingula
Opis:
In the Middle Miocene deposits of the Central Paratethys, lingulides, because of their low taphonomic potential, are very rare and difficult to identify. Two species of Lingula, L. dumortieri Nyst, 1843 and L. dregeri Andreae, 1893, have been recorded from the Badenian (Middle Miocene) of Poland. Re−examination of the specimens has shown that none of them can be referred to Lingula dumortieri (now Glottidia dumortieri). The rounded outline of the scar of the posterior adductor muscle and the lack of the septa indicate that all the specimens must be referred to the genus Lingula. Their valves appear to be slightly more convex than in other species of Lingula and closely resemble the Recent L. tumidula Reeve, 1841. We assign all the specimens of Lingula found in the Miocene of Poland to L. dregeri. Because our specimens are juveniles and some are broken we cannot adequately redescribe this species. Lingula dregeri was distributed in the Middle Miocene of the Central Paratethys (Austria, Poland, Ukraine, Romania), while Glottidia dumortieri occurs in the Pliocene of Northern Europe (Atlantic Province).
Źródło:
Acta Palaeontologica Polonica; 2005, 50, 1
0567-7920
Pojawia się w:
Acta Palaeontologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Modes of ventilation in early tetrapods: costal aspiration as a key feature of amniotes
Autorzy:
Janis, C M
Keller, J C
Powiązania:
https://bibliotekanauki.pl/articles/21209.pdf
Data publikacji:
2001
Wydawca:
Polska Akademia Nauk. Instytut Paleobiologii PAN
Tematy:
reptile
bird
skin
carbon dioxide
mammal
ventilation
anamniote
amphibian
rib
tetrapod
skull
egg
Opis:
The key difference between amniotes (reptiles, birds and mammals) and anamniotes (amphibians in the broadest sense of the word) is usually considered to be the amniotic egg, or a skin impermeable to water. We propose that the change in the mode of lung ventilation from buccal pumping to costal (rib-based) ventilation was equally, if not more important, in the evolution of tetrapod independence from the water. Costal ventilation would enable superior loss of carbon dioxide via the lungs: only then could cutaneous respiration be abandoned and the skin made impermeable to water. Additionally efficient carbon dioxide loss might be essential for the greater level of activity of amniotes. We examine aspects of the morphology of the heads, necks and ribs that correlate with the mode of ventilation. Anamniotes, living and fossil, have relatively broad heads and short necks, correlating with buccal pumping, and have immobile ribs. In contrast, amniotes have narrower, deeper heads, may have longer necks, and have mobile ribs, in correlation with costal ventilation. The stem amniote Diadectes is more like true amniotes in most respects, and we propose that the changes in the mode of ventilation occurred in a stepwise fashion among the stem amniotes. We also argue that the change in ventilatory mode in amniotes related to changes in the postural role of the epaxial muscles, and can be correlated with the evolution of herbivory.
Źródło:
Acta Palaeontologica Polonica; 2001, 46, 2
0567-7920
Pojawia się w:
Acta Palaeontologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The discovery of Rhabdopleura (Pterobranchia) in the Jurassic of Poland
Odkrycie Rhabdopleura (Pterobranchia) iw Jurze Polski
Otkrytie Rhabdopleura (Krylozhabernye) v Jure Polshi
Autorzy:
Kulicki, C.
Powiązania:
https://bibliotekanauki.pl/articles/21074.pdf
Data publikacji:
1969
Wydawca:
Polska Akademia Nauk. Instytut Paleobiologii PAN
Źródło:
Acta Palaeontologica Polonica; 1969, 14, 4
0567-7920
Pojawia się w:
Acta Palaeontologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Remarks on the embryogeny and postembryonal development of ammonites
Uwagi o embriogenezie i rozwoju postembrionalnym amonitów
Primechanija na temu ehmbriogeneza i postehmbrionalnojj ehvoljucii ammonitov
Autorzy:
Kulicki, C.
Powiązania:
https://bibliotekanauki.pl/articles/21929.pdf
Data publikacji:
1974
Wydawca:
Polska Akademia Nauk. Instytut Paleobiologii PAN
Źródło:
Acta Palaeontologica Polonica; 1974, 19, 2
0567-7920
Pojawia się w:
Acta Palaeontologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Systematic relationships of the blind phacopine trilobite Trimerocephalus, with a new species from Causses-et-Veyran, Montagne Noire
Autorzy:
Cronier, C
Powiązania:
https://bibliotekanauki.pl/articles/22111.pdf
Data publikacji:
2003
Wydawca:
Polska Akademia Nauk. Instytut Paleobiologii PAN
Tematy:
Montagne Noire
Famennian
trilobite
Upper Devonian
Trilobita
Phacopinae
Trimerocephalus
new species
France
paleontology
Opis:
The paper describes a new species of blind trilobite from the lower Fammenian of Concours−le−Haut at Causses−et−Veyran, Montagne Noire (France). Trimerocephalus (Trifoliops) nigritus subgen. et sp. nov. is assigned to a new subgenus together with Tr. (Trif.) trifolius (Osmólska, 1958). This grouping is supported by the results of phylogenetic analysis of thirteen species attributed to the Fammenian genus Trimerocephalus McCoy, 1849; of 16 previously known species attributed to this genus, only 12 were represented by data of quality sufficient to be included in the analysis, using 23 morphological characters. The Frasnian phacopine Acuticryphops acuticeps (Kayser, 1889) is used as the outgroup. The three most parsimonious trees have a length of 51 steps and a consistency index of 0.82. The new subgenus Trifoliops forms a clade together with Trimerocephalus? steinachensis (Richter and Richter, 1926), supported by an exclusive synapomorphy: widening of the cephalic antero−lateral border. Tr.? steinachensis seems to be more closely related to Tr. (Trif.) trifolius (sharing two synapomorphies) and may represent a more derived taxon (possibly deserving a separate subgeneric status). The remanig Trimerocephalus species are not formally assigned to subgeneric taxa, pending further studies (their relationships are shown in cladograms). The results do not confirm the classification suggested by Chlupač (1966) for Trimerocephalus.
Źródło:
Acta Palaeontologica Polonica; 2003, 48, 1
0567-7920
Pojawia się w:
Acta Palaeontologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Sublethal injuries in Early Devonian cephalopod shells from Morocco
Autorzy:
Klug, C.
Powiązania:
https://bibliotekanauki.pl/articles/22322.pdf
Data publikacji:
2007
Wydawca:
Polska Akademia Nauk. Instytut Paleobiologii PAN
Tematy:
Ammonoidea
Bactritoidea
Devonian
Early Devonian
Gnathostomata
Morocco
cephalopod
paleontology
shell
predation
life mode
ectocochleate cephalopod
Opis:
Internal moulds of the relatively small− to moderate−size shells of Early Devonian ectocochleate cephalopods (typically <150 mm diameter) occasionally display traces of repaired shell damage. Presumably, these animals with their highly specialized buoyancy device, the phragmocone, lived in the water column. It is uncertain as to how the shells of these animals were damaged; one likely cause would be predatory attacks but the identity of the perpetrator remains uncertain. So far, no remains of arthropods capable of breaking or cutting shells have been found in the fossiliferous outcrops of this age in the Anti−Atlas (Morocco). The only macrovertebrate remains of this age are of acanthodian and placoderm fish which probably lived a more or less benthonic life style. Additionally, a fish attack on these cephalopods would probably have destroyed most of the thin−shelled conch and killed the animal. Most of the repaired shell breaks are triangular in shape which is characteristic for cephalopod bite marks. Additionally, the paired arrangement of the fractures in over 70 bactritoids supports the hypothesis that it was a cephalopod attacking another cephalopod. It cannot be excluded with certainty that occasional vertebrate attacks left traces on their shells. Fossil evidence indicates that the development of tightly coiled conchs was a rapid evolutionary event in the Ammonoidea in the Early Devonian; however, the evolution of coiling is probably not directly related to predation pressures because the ratio of injured to healthy specimens is roughly the same in Zlíchovian bactritoids with orthoconic and ammonoids with coiled shells.
Źródło:
Acta Palaeontologica Polonica; 2007, 52, 4
0567-7920
Pojawia się w:
Acta Palaeontologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Functional morphology and taphonomy of nautiloid beaks from the Middle Triassic of Southern Germany
Autorzy:
Klug, C
Powiązania:
https://bibliotekanauki.pl/articles/22638.pdf
Data publikacji:
2001
Wydawca:
Polska Akademia Nauk. Instytut Paleobiologii PAN
Tematy:
Muschelkalk
taphonomy
beak
Germany
Upper Muschelkalk
Middle Triassic
Germanonautilus
Conchorhynchus avirostris
Triassic
Rhyncholithes hirundo
fossil
rhyncholith
living chamber
nautiloid beak
deposit
paleontology
Nautilus
functional morphology
paleozoology
Opis:
New records of nautiloid beak elements conventionally classified as 'Rhyncholithes hirundo (Biguet, 1819)' and 'Conchorhynchus avirostris (von Schlotheim, 1820)' with carbonised (originally chitinous) three-dimensionally preserved appendages from the Upper Muschelkalk (Middle Triassic) of northern Württemberg (Southwest Germany) enable restoration of the complete beak of Germanonautilus. In three specimens, the lower mandible is embedded within the living chamber of Germanonautilus conchs, Beak elements of Germanonautilus differ from those of Recent Nautilus in the more elongate appendages of the fossil lower mandibles and the weaker sculpture on the originally chitinous parts. Furthermore, the dorsal sculpture of the fossil conchorhynchs consists of ridges rather than denticles and the ventral sculpture of the fossil rhyncholiths displays ridges in places where the Recent rhyncholiths have a smooth surface. Additionally, the fossil beak elements attained a larger size than their Recent counterparts, During transport of 'Rhyncholithes hirundo', the light chitinous parts served as a sail and the heavier conchorhynch anchored in the sediment causing alignment. In contrast to the irregularly embedded isolated rhyncholiths, the conchorhynchs usually settled with their ventral side up. From the study of 407 fossil nautiloid beak-elements, a significant variability of the hard parts is evident. Consequently, the assignment of specific morphologies to the species of Germanonautilus is impossible.
Zrekonstruowano aparat szczękowy łodzika z rodzaju Germanonautilus wykorzystując nowe materiały z górnego wapienia muszlowego (środkowy trias) północnej Wirtembergii (południowo-zachodnie Niemcy). Opisane elementy aparatu szczękowego Germanonautilus, tradycyjnie klasyfikowane jako „Rhyncholites hirundo (Biguet, 1819)” oraz „Conchorhynchus avirostris (von Schlotheim, 1820)”, są dobrze zachowane, niekiedy ze zwęglonymi, pierwotnie chitynowymi wyrostkami. Trzy okazy dolnej szczęki znaleziono w komorze mieszkalnej Germanonautilus, co potwierdza powiązanie opisanych elementów aparatu szczękowego z tym rodzajem łodzika. W porównaniu ze współcześnie żyjącym łodzikiem z rodzaju Nautilus, elementy dolnej szczęki Germanonautilus mają bardziej wydłużone wyrostki i mniej wydatne urzeźbienie części pierwotnie organicznych, oraz urzeźbienie grzbietowej części elementów zmieneralizowanych (konchorynchów) w postaci grzbiecików, a nie ząbków jak u Nautilus. Pierwotnie organiczne elementy górnej szczęki u Germanonautilus oraz współczesnego łodzika są bardzo podobne, natomiast części zmineralizowane górnych szczęk (ryncholity) Germanonautilus różnią się bardziej rozciągniętą pokrywą oraz wydatną rzeźbą części brzusznej w postaci grzbiecików (u Nautilus element ten jest gładki). W czasie pośmiertnego transportu pierwotnie organiczne i lżejsze elementy górnej szczęki Germanonautilus działały zapewne jak żagiel, natomiast cięższe elementy szczęki dolnej kotwiczyły się w osadzie, powodując doprądową orientacje skamieniałości. Po rozkładzie części organicznych, elementy aparatu ulegały rozproszeniu, jednak o ile ryncholity znajdowane są w osadzie w rozmaitym położeniu, to konchorynchy położone są najczęściej stroną brzuszną do góry.
Źródło:
Acta Palaeontologica Polonica; 2001, 46, 1
0567-7920
Pojawia się w:
Acta Palaeontologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Structure and mode of origin of the ammonite proseptum
Budowa i sposób powstawania proseptum amonitów
Stroenie i sposob obrazovanija prosepta ammonitov
Autorzy:
Kulicki, C.
Powiązania:
https://bibliotekanauki.pl/articles/22859.pdf
Data publikacji:
1975
Wydawca:
Polska Akademia Nauk. Instytut Paleobiologii PAN
Źródło:
Acta Palaeontologica Polonica; 1975, 20, 4
0567-7920
Pojawia się w:
Acta Palaeontologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł

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