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Статті в журналах з теми "Coleoids"

Автор: Grafiati

Опубліковано: 5 березня 2024

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1

Mapes, Royal H., and Larisa A. Doguzhaeva. "New Pennsylvanian coleoids (Cephalopoda) from Nebraska and Iowa, USA." Journal of Paleontology 92, no. 2 (2017): 146–56. http://dx.doi.org/10.1017/jpa.2017.79.

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AbstractFour rare Pennsylvanian (Stark Shale: Pennsylvanian, Missourian [=Kasimovian]) coleoids from Nebraska and Iowa, which are preserved as flattened partial phragmocones and body chambers associated with three-dimensionally fossilized ink sacs, are herein described as Pabianiconus starkensis new genus new species, Nebraskaconus whitei new genus new species, and Starkites compressus new genus new species. One specimen that is missing most of the phragmocone, is provisionally assigned to Donovaniconus. The fossils are assigned to the Coleoidea because of the presence of ink-filled sacs in th

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2

Doguzhaeva, Larisa A., and Royal H. Mapes. "A new late Carboniferous coleoid from Oklahoma, USA: implications for the early evolutionary history of the subclass Coleoidea (Cephalopoda)." Journal of Paleontology 92, no. 2 (2017): 157–69. http://dx.doi.org/10.1017/jpa.2017.81.

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AbstractThe limited record of the bactritoid-like coleoid cephalopods is here expanded due to discovery of a late Carboniferous (Moscovian) orthocone comprising a phragmocone and a body chamber with a proostracum-like structure, a sheath-like rostrum, an ink sac, and a muscular mantle preserved on top of the conch. The specimen comes from the Wewoka Formation in the vicinity of the city of Okmulgee, Oklahoma, which previously yielded an orthocone indicative of an evolutionary branch of the Carboniferous cephalopods described as the order Donovaniconida Doguzhaeva, Mapes, and Mutvei, 2007a with

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3

Tanner, Alastair R., Dirk Fuchs, Inger E. Winkelmann, et al. "Molecular clocks indicate turnover and diversification of modern coleoid cephalopods during the Mesozoic Marine Revolution." Proceedings of the Royal Society B: Biological Sciences 284, no. 1850 (2017): 20162818. http://dx.doi.org/10.1098/rspb.2016.2818.

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Coleoid cephalopod molluscs comprise squid, cuttlefish and octopuses, and represent nearly the entire diversity of modern cephalopods. Sophisticated adaptations such as the use of colour for camouflage and communication, jet propulsion and the ink sac highlight the unique nature of the group. Despite these striking adaptations, there are clear parallels in ecology between coleoids and bony fishes. The coleoid fossil record is limited, however, hindering confident analysis of the tempo and pattern of their evolution. Here we use a molecular dataset (180 genes, approx. 36 000 amino acids) of 26

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4

Jattiot, Romain, Nathalie Coquel-Poussy, Isabelle Kruta, Isabelle Rouget, Alison J. Rowe, and Jean-David Moreau. "The first gladius-bearing coleoid cephalopods from the lower Toarcian “Schistes Cartons” Formation of the Causses Basin (southeastern France)." PeerJ 12 (February 26, 2024): e16894. http://dx.doi.org/10.7717/peerj.16894.

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The fossil record of gladius-bearing coleoids is scarce and based only on a few localities with geological horizons particularly favourable to their preservation (the so-called Konservat-Lagerstätten), which naturally leads to strongly limited data on geographical distributions. This emphasizes the importance of every new locality providing gladius-bearing coleoids. Here, we assess for the first time the gladius-bearing coleoid taxonomic diversity within the lower Toarcian “Schistes Cartons” of the Causses Basin (southeastern France). The material includes two fragmentary gladii, identified as

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5

Shoshan, Yoav, Noa Liscovitch-Brauer, Joshua J. C. Rosenthal, and Eli Eisenberg. "Adaptive Proteome Diversification by Nonsynonymous A-to-I RNA Editing in Coleoid Cephalopods." Molecular Biology and Evolution 38, no. 9 (2021): 3775–88. http://dx.doi.org/10.1093/molbev/msab154.

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Abstract RNA editing by the ADAR enzymes converts selected adenosines into inosines, biological mimics for guanosines. By doing so, it alters protein-coding sequences, resulting in novel protein products that diversify the proteome beyond its genomic blueprint. Recoding is exceptionally abundant in the neural tissues of coleoid cephalopods (octopuses, squids, and cuttlefishes), with an over-representation of nonsynonymous edits suggesting positive selection. However, the extent to which proteome diversification by recoding provides an adaptive advantage is not known. It was recently suggested

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6

Fuchs, Dirk, Vladimir Laptikhovsky, Svetlana Nikolaeva, Alexei Ippolitov, and Mikhail Rogov. "Evolution of reproductive strategies in coleoid mollusks." Paleobiology 46, no. 1 (2020): 82–103. http://dx.doi.org/10.1017/pab.2019.41.

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AbstractColeoid cephalopods exhibited two distinct reproductive strategies, resulting in small pelagic and large demersal hatchlings, both in the geologic past and recently. In ectocochleate cephalopods, the hatching event is recorded in shell structures (e.g., nepionic constrictions, ultrastructural shifts, or ornamentation differences). In contrast, well-defined hatching markers do not exist on coleoid shells. Changes in septal spacing may be evidence of hatching (e.g., some extant sepiids), but not in all fossil groups. In the present study, we subdivide the early ontogenetic shells of phra

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7

Klug, Christian, Gianpaolo Di Silvestro, Rene Hoffmann, et al. "Taphonomic patterns mimic biologic structures: diagenetic Liesegang rings in Mesozoic coleoids and coprolites." PeerJ 9 (January 14, 2021): e10703. http://dx.doi.org/10.7717/peerj.10703.

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Because of physiology of coleoids, their fossils preserve soft-tissue-remains more often than other cephalopods. Sometimes, the phosphatized soft-tissues, particularly parts of the muscular mantle, display dark circular patterns. Here, we showcase that these patterns, here documented for fossil coleoids from the Jurassic of Germany and the Cretaceous of Lebanon, superficially resemble chromatophores (which enable living coleoids to alter their coloration). We examined and chemically analyzed the circular structures in these specimens, describe them, and discuss their genesis. Based on their st

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8

Mutvei, Harry, and Royal H. Mapes. "Carboniferous coleoids with mixed coleoid-orthocerid characteristics: a new light on cephalopod evolution." GFF 140, no. 1 (2018): 11–24. http://dx.doi.org/10.1080/11035897.2018.1429490.

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9

Tanabe, Kazushige, Pat Trask, Rick Ross, and Yoshinori Hikida. "Late Cretaceous octobrachiate coleoid lower jaws from the north Pacific regions." Journal of Paleontology 82, no. 2 (2008): 398–408. http://dx.doi.org/10.1666/07-029.1.

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Eight well-preserved cephalopod jaw fossils were discovered from the Upper Cretaceous (Santonian and Campanian) deposits of Vancouver Island, Canada, and Hokkaido, Japan. They occur individually in calcareous concretions and retain their three-dimensional architecture. Seven of them consist of a widely open outer lamella and a posteriorly projected inner lamella with a pointed rostrum. Both lamellae are made of fluorapatite, which may represent diagenetically altered chitin, and lack a calcareous element. Based on these diagnostic features, the seven jaw fossils are identified as lower jaws of

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10

Jattiot, Romain, Arnaud Brayard, Emmanuel Fara, and Sylvain Charbonnier. "Gladius-bearing coleoids from the Upper Cretaceous Lebanese Lagerstätten: diversity, morphology, and phylogenetic implications." Journal of Paleontology 89, no. 1 (2015): 148–67. http://dx.doi.org/10.1017/jpa.2014.13.

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AbstractGladius-bearing coleoids are rare in the fossil record. For the Cretaceous period, these cephalopods are mainly recorded in a few Lagerstätten in Lebanon (Haqel, Hajoula, En Nammoura, and Sahel Aalma). Here, we study 16 specimens of gladius-bearing coleoids from these Upper Cretaceous Lebanese Lagerstätten to investigate their taxonomic diversity. Besides two species that were already reported (Dorateuthis syriacaandGlyphiteuthis libanotica), one new species is identified in the Cenomanian site of Hajoula:Rachiteuthis acutalin. sp., as well as another form ofGlyphiteuthisfrom En Nammou

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11

Mather, Jennifer A., and Michael J. Kuba. "The cephalopod specialties: complex nervous system, learning, and cognition." Canadian Journal of Zoology 91, no. 6 (2013): 431–49. http://dx.doi.org/10.1139/cjz-2013-0009.

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While clearly of molluscan ancestry, the coleoid cephalopods are emergent within the phylum for complexity of brain and behaviour. The brain does not just have centralization of the molluscan ganglia but also contains lobes with “higher order” functions such as storage of learned information, and centres have been compared with the vertebrate cerebellum and frontal lobe. The flexible muscular hydrostat movement system theoretically has unlimited degrees of freedom, and octopuses are models for “soft movement” robots. The decentralized nervous system, particularly in the arms of octopuses, resu

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12

MUTVEI, HARRY, and DESMOND T. DONOVAN. "SIPHUNCULAR STRUCTURE IN SOME FOSSIL COLEOIDS AND RECENT SPIRULA." Palaeontology 49, no. 3 (2006): 685–91. http://dx.doi.org/10.1111/j.1475-4983.2006.00533.x.

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13

Fuchs, Dirk, and Robert Weis. "Taxonomy, morphology and phylogeny of Lower Jurassic loligosepiid coleoids (Cephalopoda)." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 249, no. 1 (2008): 93–112. http://dx.doi.org/10.1127/0077-7749/2008/0249-0093.

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14

Fuchs, Dirk, and Robert Weis. "Taxonomy, morphology and phylogeny of Lower Jurassic teudopseid coleoids (Cephalopoda)." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 257, no. 3 (2010): 351–66. http://dx.doi.org/10.1127/0077-7749/2010/0083.

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15

Mutvei, Harry. "Siphuncular Structure in the Extant Spirula and in Other Coleoids (Cephalopoda)." GFF 139, no. 2 (2016): 129–39. http://dx.doi.org/10.1080/11035897.2016.1227364.

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16

Mutvei, Harry, Royal H. Mapes, and Larisa A. Doguzhaeva. "Shell structures in Carboniferous bactritid-like coleoids (Cephalopoda) from South Central USA." GFF 134, no. 3 (2012): 201–16. http://dx.doi.org/10.1080/11035897.2012.696134.

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17

Hoffmann, René, Manuel F. G. Weinkauf, and Dirk Fuchs. "Grasping the shape of belemnoid arm hooks—a quantitative approach." Paleobiology 43, no. 2 (2017): 304–20. http://dx.doi.org/10.1017/pab.2016.44.

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AbstractChitinous arm hooks (onychites) of belemnoid coleoid cephalopods are widely distributed in Mesozoic sediments. Due to their relative abundance and variable morphology compared with the single, bullet-shaped, belemnite rostrum, arm hooks came into the focus of micropaleontologists as a promising index fossil group for the Jurassic–Cretaceous rock record and have been the target of functional, ecological, and phylogenetic interpretations in the past. Based on three well-preserved arm crowns of the Toarcian diplobelid Chondroteuthis wunnenbergi, we analyzed the shape of a total of 87 micr

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18

Garassino, Alessandro, and Desmond T. Donovan. "A New Family Of Coleoids From The Lower Jurassic Of Osteno, Northern Italy." Palaeontology 43, no. 6 (2000): 1019–38. http://dx.doi.org/10.1111/1475-4983.00160.

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19

Stanley, George D., Carlos González-León, Michael R. Sandy, et al. "Upper Triassic Invertebrates from the Antimonio Formation, Sonora, Mexico." Journal of Paleontology 68, S36 (1994): 1–33. http://dx.doi.org/10.1017/s0022336000062284.

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A diverse Upper Triassic tropical marine fauna from northwestern Sonora, Mexico, includes 31 taxa of tropical invertebrates including scleractinian corals, spongiomorphs, disjectoporoids, “hydrozoans,” thalamid and nonthalamid sponges, spiriferid and terebratulid brachiopods, gastropods, bivalves, coleoids, and anomuran microcoprolites. They occur within the late Karnian to Norian part of the Antimonio Formation (Antimonio terrane), which is juxtaposed against a fragmented portion of the North American craton. Most of the fauna is also known from the Tethys region. Sixteen Sonoran taxa co-occu

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20

FUCHS, DIRK, HELMUT KEUPP, PAT TRASK, and KAZUSHIGE TANABE. "Taxonomy, morphology and phylogeny of Late Cretaceous spirulid coleoids (Cephalopoda) from Greenland and Canada." Palaeontology 55, no. 2 (2012): 285–303. http://dx.doi.org/10.1111/j.1475-4983.2011.01125.x.

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21

Tanabe, Kazushige, and Royal H. Mapes. "Jaws and radula of the Carboniferous ammonoid Cravenoceras." Journal of Paleontology 69, no. 4 (1995): 703–7. http://dx.doi.org/10.1017/s0022336000035228.

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A well-preserved mouth apparatus consisting of jaws and a radula was found in situ within the body chamber of the goniatite Cravenoceras fayettevillae Gordon, 1965 (Neoglyphiocerataceae: Cravenoceratidae), from the middle Chesterian (Upper Mississippian) of Arkansas. Both upper and lower jaws consist of a black material. The lower jaw is characterized by a widely opened larger outer lamella and a shorter inner lamella. The upper jaw is fragmental. The radula is preserved in the anterior portion of the buccal space and comprises a series of tooth elements. Each transverse tooth row consists of

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22

Lukeneder, Petra, and Alexander Lukeneder. "Mineralized belemnoid cephalic cartilage from the late Triassic Polzberg Konservat-Lagerstätte (Austria)." PLOS ONE 17, no. 4 (2022): e0264595. http://dx.doi.org/10.1371/journal.pone.0264595.

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Although hyaline cartilage is widely distributed in various invertebrate groups such as sabellid polychaetes, molluscs (cephalopods, gastropods) and a chelicerate arthropod group (horseshoe crabs), the enigmatic relationship and distribution of cartilage in taxonomic groups remains to be explained. It can be interpreted as a convergent trait in animal evolution and thus does not seem to be a vertebrate invention. Due to the poor fossil record of cartilaginous structures, occurrences of mineralized fossil cartilages are important for evolutionary biology and paleontology. Although the biochemic

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23

Košťák, Martin, John W. M. Jagt, Robert P. Speijer, Peter Stassen, and Etienne Steurbaut. "New Paleocene Sepiid Coleoids (Cephalopoda) from Egypt: Evolutionary Significance and Origin of the Sepiid ‘Rostrum’." PLoS ONE 8, no. 11 (2013): e81180. http://dx.doi.org/10.1371/journal.pone.0081180.

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24

Fuchs, D., S. von Boletzky, and H. Tischlinger. "New evidence of functional suckers in belemnoid coleoids (Cephalopoda) weakens support for the 'Neocoleoidea' concept." Journal of Molluscan Studies 76, no. 4 (2010): 404–6. http://dx.doi.org/10.1093/mollus/eyq032.

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25

Fuchs, Dirk, Andreas Klinghammer, and Helmut Keupp. "Taxonomy, morphology and phylogeny of plesioteuthidid coleoids from the Upper Jurassic (Tithonian) Plattenkalks of Solnhofen." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 245, no. 2 (2007): 239–52. http://dx.doi.org/10.1127/0077-7749/2007/0245-0239.

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26

Valente, David E., Amanda L. Edwards, and John E. Pollard. "Reappraisal of the gastric contents of a Lower Jurassic ichthyosaur." Geological Curator 9, no. 3 (2010): 133–42. http://dx.doi.org/10.55468/gc220.

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Re-examination of cephalopod hooklets preserved within the gastric mass of several Lower Jurassic ichthyosaurs reveals that these reptiles fed mainly on phragmoteuthids, rather than belemnites as previously proposed. This conclusion matches the findings of recent research on ichthyosaurs and well-preserved coleoids from the Lower Jurassic (Toarcian) Posidonia Shales of southern Germany. A greater variety of belemnoid species known in the Posidonia Shales includes complete belemnites with bite marks; these provide evidence of predation from large vertebrates such as ichthyosaurs. However, no be

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27

Basil, J. A., R. T. Hanlon, S. I. Sheikh, and J. Atema. "Three-dimensional odor tracking by Nautilus pompilius." Journal of Experimental Biology 203, no. 9 (2000): 1409–14. http://dx.doi.org/10.1242/jeb.203.9.1409.

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The ‘living fossil’ Nautilus pompilius is thought to use olfaction as its primary sensory system during foraging, yet neither the organs responsible for olfaction nor the mechanisms or behaviors associated with odor tracking have been subjected to experimentation. Flume testing under dark conditions revealed that Nautilus could consistently detect and follow turbulent odor plumes to the source over distances up to 10 m, exhibiting two types of orientation behavior while sampling in three dimensions. The paired rhinophores were necessary for orientation behavior: when they were temporarily bloc

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28

Shiino, Yuta, and Kota Kitazawa. "Stealth Effect of Red Shell in Laqueus rubellus (Brachiopoda, Terebratulida) on the Sea Bottom: An Evolutionary Insight into the Prey-Predator Interaction." ISRN Zoology 2012 (March 14, 2012): 1–7. http://dx.doi.org/10.5402/2012/692517.

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The selective advantage of empire red coloration in the shell of Laqueus rubellus (a terebratulid brachiopod) was examined in terms of prey-predator interactions. The study was based on a comparison of benthic suspension feeders living at a depth of about 130 m in Suruga Bay, Japan, with special reference to their visibility under visible and near-infrared light conditions. Almost all species exhibited red coloration under visible light, while only the shell of Laqueus was dark under infrared light, similar to rocks and bioclasts. Given the functional eyes of macropredators such as fishes and

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29

Yamaguchi, Ayaka, Yuichiro Kumada, Andrea C. Alfaro, and Ryoji Wani. "Abrupt changes in distance between succeeding septa at the hatching time in modern coleoids Sepiella japonica and Spirula spirula." Swiss Journal of Palaeontology 134, no. 2 (2015): 301–7. http://dx.doi.org/10.1007/s13358-015-0078-x.

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30

Konstantinov, A. G., E. S. Sobolev, A. V. Yadrenkin, et al. "High-Resolution Triassic Biostratigraphy of the Kotelny Island (New Siberian Islands, Arctic Siberia)." Russian Geology and Geophysics 63, no. 4 (2022): 398–416. http://dx.doi.org/10.2113/rgg20214424.

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Abstract The study of Triassic paleontology and stratigraphy of various regions of northeastern Russia and adjacent Arctic shelf is essential not only for improving and refining zonal biostratigraphic schemes, interregional and global correlation of Triassic deposits, and resolving problems of stratigraphic boundaries but also for developing and substantiating a new generation of Triassic stratigraphic schemes, which could serve as the stratigraphic basis for different regional and detailed geological investigations of the Arctic. The results of the study were used to improve existing zonal sc

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31

Donovan, S. K., J. W. M. Jagt, and D. N. Lewis. "Notes on some trace fossils and other parataxa from the Maastrichtian type area, southeast Netherlands and northeast Belgium." Netherlands Journal of Geosciences - Geologie en Mijnbouw 90, no. 2-3 (2011): 99–109. http://dx.doi.org/10.1017/s0016774600001050.

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AbstractNew specimens described herein add to our knowledge of uncommon parataxa (embedment structures, borings and a certain type of burrow) from the type area of the Maastrichtian Stage, the material originating from the ENCI-HeidelbergCement Group (Maastricht), Ankerpoort-'t Rooth (Bemelen) and former Blom (Berg en Terblijt) quarries in southern Limburg (the Netherlands), and from the CBR-Romontbos (Eben Emael) and CPL SA (Haccourt) chalk pits in the province of Liège (northeast Belgium). Although Centrichnus eccentricus Bromley & Martinell has previously been recorded from this area, i

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32

Mutvei, Harry, and Royal H. Mapes. "Carboniferous orthocerid-like coleoid Mitorthoceras with unique shell structure (new order Tuborthocerida, Coleoidea, Cephalopoda); comparison with bactritid-like coleoid Shimanskya." GFF 141, no. 2 (2019): 121–32. http://dx.doi.org/10.1080/11035897.2019.1572218.

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33

Moreau, Jean-David, Romain Vullo, Sylvain Charbonnier, et al. "Konservat-Lagerstätten from the Upper Jurassic lithographic limestone of the Causse Méjean (Lozère, southern France): palaeontological and palaeoenvironmental synthesis." Geological Magazine 159, no. 5 (2022): 761–81. http://dx.doi.org/10.1017/s0016756821001382.

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AbstractSince the 1980s, the Upper Jurassic lithographic limestone of the Causse Méjean (southern France) has been known by local naturalists to yield fossils. However, until the beginning of the 21st century, this plattenkalk remained largely undersampled and scientifically underestimated. Here, we present the results of two decades of prospection and sampling in the Drigas and the Nivoliers quarries. We provide the first palaeontological inventory of the fossil flora, the fauna and the ichnofauna for these localities. The fossil assemblages show the co-occurrence of marine and terrestrial or

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34

WELLS, M. J., and J. WELLS. "Ventilation and Oxygen Uptake by Nautilus." Journal of Experimental Biology 118, no. 1 (1985): 297–312. http://dx.doi.org/10.1242/jeb.118.1.297.

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The shell of Nautilus prevents the mantle from playing any part in creating the ventilatory stream. This is generated instead by movements of the collar and funnel folds which fuse to form flaps (the ‘wings’), overlapping below and joined to the head above. The gills lie horizontally, dividing the space enclosed by the wings into three cavities, two lateral and prebranchial, on either side of the head, and a common ventral postbranchial space. Water is drawn in above, behind the eyes, and expelled forward through the siphon of the funnel, which is used both for ventilation and jet propulsion.

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35

Jeffery, Charlotte H. "Paleobase: macrofossils part 2. Ammonoids, bivalves coleoids, gastropods and other mollusca edited by Norman MacLeod, Blackwell Publishing, Oxford, 2003. ISBN 0632 05891 9(CD-ROM)." Geological Journal 39, no. 2 (2004): 228–29. http://dx.doi.org/10.1002/gj.972.

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36

Linzmeier, Benjamin J., Neil H. Landman, Shanan E. Peters, Reinhard Kozdon, Kouki Kitajima, and John W. Valley. "Ion microprobe–measured stable isotope evidence for ammonite habitat and life mode during early ontogeny." Paleobiology 44, no. 4 (2018): 684–708. http://dx.doi.org/10.1017/pab.2018.21.

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AbstractAmmonites have disparate adult morphologies indicative of diverse ecological niches, but ammonite hatchlings are small (~1 mm diameter), which raises questions about the similarity of egg incubation and hatchling life mode in ammonites. ModernNautilusis sometimes used as a model organism for understanding ammonites, but despite their outward similarities, the groups are only distantly related. Trends in ammonite diversity and extinction vulnerability in the fossil record contrast starkly with those of nautilids, and embryonic shells from Late Cretaceous ammonites are two orders of magn

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Rolfe, W. D. Ian. "Form and function in Thylacocephala, Conchyliocarida and Concavicarida (?Crustacea): a problem of interpretation." Earth and Environmental Science Transactions of the Royal Society of Edinburgh 76, no. 2-3 (1985): 391–99. http://dx.doi.org/10.1017/s0263593300010609.

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ABSTRACTDifferences in the preservation of Jurassic thylacocephalans and conchyliocarids have given rise to different interpretations of the form of these fossils, and thus their mode of life. When evidence from these two groups is combined with that derived from Palaeozoic concavicarids, it becomes possible to unify the several interpretations of this one group of organisms, the Thylacocephala. The group ranges from at least the Silurian to the Cretaceous.A review is given of how these differences of interpretation have arisen, and some resolution is attempted. If the thylacocephalan “anterio

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Schlögl, Ján, Martin Košt’ák, and Matúš Hyžný. "First record of a gladius-bearing coleoid Teudopsis bollensis Voltz (Cephalopoda, Coleoidea) in the Toarcian of the Western Carpathians (Slovakia)." Paläontologische Zeitschrift 86, no. 4 (2012): 367–75. http://dx.doi.org/10.1007/s12542-012-0139-z.

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Rogov, Mikhail, Aleksandr Mironenko, Alexey Ippolitov, and Oleg Lutikov. "A First Record of Lower Jurassic (Toarcian) Coleoid Jaws in Siberia." Diversity 15, no. 6 (2023): 742. http://dx.doi.org/10.3390/d15060742.

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In the present paper, we describe several coleoid jaws discovered in the lower Toarcian black shales, cropping out along the Vilyui River (Yakutia, Russia). This is the first record of a Lower Jurassic coleoid jaw outside Europe and the first report of such a finding from the Mesozoic of Siberia. The described coleoid jaws demonstrate the same mode of preservation and morphology as the coeval jaws previously reported from Europe. Their preservation in Siberia became possible due to the widespread occurrence of black shale facies associated with the early Toarcian oceanic anoxic event (TOAE).

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Kruta, Isabelle, Isabelle Rouget, Sylvain Charbonnier, et al. "Proteroctopus ribetiin coleoid evolution." Palaeontology 59, no. 6 (2016): 767–73. http://dx.doi.org/10.1111/pala.12265.

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Lozouet, Pierre. "Paleobase Macrofossils Part 2.0. Ammonoids, Bivalves, Coleoids, Gastropods and other Mollusca, N. Macleod (ed.). Blackwell Publishing and the Natural History Museum, 2003, £27.50 (single user) £130 (site licence). ISBN 0-63205891-9 (CD-ROM)." Journal of Quaternary Science 19, no. 8 (2004): 836–37. http://dx.doi.org/10.1002/jqs.867.

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Dernov, Vitaly. "Coleolus carbonarius Demanet, 1938 (incertae sedis) from the late Bashkirian (Carboniferous) of the Donets Basin." GEO&BIO 2022, no. 22 (2022): 79–93. http://dx.doi.org/10.15407/gb2207.

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Problematic fossils Coleolus carbonarius Demanet, 1938 were described from seven localities of the Mospyne Formation (late Bashkirian, Carboniferous) of the central Donets Basin. Many authors attributed these conoidal fossils to various groups of animals, including worms, conulariids, pteropods, hyoliths, tentaculitids, gastropods, scaphopods, and other molluscs without specifying the class, as well as phyllocarids. Representatives of the genus Coleolus cannot belong to the scaphopods because the apex of their tube is closed. The aperture of the tube in living Coleolus is directed upwards, whi

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Talbot, Christopher, Thomas M. Jordan, Nicholas W. Roberts, Shaun P. Collin, N. Justin Marshall, and Shelby E. Temple. "Corneal microprojections in coleoid cephalopods." Journal of Comparative Physiology A 198, no. 12 (2012): 849–56. http://dx.doi.org/10.1007/s00359-012-0755-9.

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VECCHIONE, MICHAEL, RICHARD E. YOUNG, DESMOND T. DONOVAN, and PAUL G. RODHOUSE. "Reevaluation of coleoid cephalopod relationships based on modified arms in the Jurassic coleoid Mastigophora." Lethaia 32, no. 2 (2007): 113–18. http://dx.doi.org/10.1111/j.1502-3931.1999.tb00529.x.

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Sweeney, A. M., S. H. D. Haddock, and S. Johnsen. "Comparative visual acuity of coleoid cephalopods." Integrative and Comparative Biology 47, no. 6 (2007): 808–14. http://dx.doi.org/10.1093/icb/icm092.

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Vecchione, Michael, Richard E. Young, and Desmond T. Donovan. "Questions of Coleoid Cephalopod Relationships Based On the Possibility of Tentacles in the Jurassic Coleoid Mastigophora." Paleontological Society Special Publications 8 (1996): 406. http://dx.doi.org/10.1017/s2475262200004081.

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Skelton, Peter. "MACLEOD, N. 2003. PaleoBase. Macrofossils Part 2.0. Ammonoids, Bivalves, Coleoids, Gastropods, and other Mollusca. vi+19 pp. +CD-ROM, in boxed set. PC and Mac compatible. Oxford, Malden, Carlton: Blackwell Publishing. Price £29.99 (boxed set). ISBN 0 632 05891 9." Geological Magazine 142, no. 3 (2005): 303–4. http://dx.doi.org/10.1017/s0016756805220770.

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Riccardi, A. C., and N. Sabattini. "Supposed coleoid remains reinterpreted as fish scales." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 1985, no. 11 (1985): 700–706. http://dx.doi.org/10.1127/njgpm/1985/1985/700.

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Challinor, A. B., and J. A. Grant-Mackie. "Jurassic Coleoidea of New Caledonia." Alcheringa: An Australasian Journal of Palaeontology 13, no. 4 (1989): 269–304. http://dx.doi.org/10.1080/03115518908619051.

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Bhandari, Renuka, C. S. Mathela, Philip S. Beauchamp, A. T. Bottini, and V. Dev. "Coleons from Nepeta elliptica." Phytochemistry 34, no. 5 (1993): 1438–39. http://dx.doi.org/10.1016/0031-9422(91)80047-5.

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