173 research outputs found

    Cold-seep ostracods from the western Svalbard margin: direct palaeo-indicator for methane seepage?

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    Source at https://doi.org/10.5194/jm-37-139-2018 Despite their high abundance and diversity, microfossil taxa adapted to a particular chemosynthetic environment have rarely been studied and are therefore poorly known. Here we report on an ostracod species, Rosaliella svalbardensis gen. et sp. nov., from a cold methane seep site at the western Svalbard margin, Fram Strait. The new species shows a distinct morphology, different from other eucytherurine ostracod genera. It has a marked similarity to Xylocythere, an ostracod genus known from chemosynthetic environments of wood falls and hydrothermal vents. Rosaliella svalbardensis is probably an endemic species or genus linked to methane seeps. We speculate that the surface ornamentation of pore clusters, secondary reticulation, and pit clusters may be related to ectosymbiosis with chemoautotrophic bacteria. This new discovery of specialized microfossil taxa is important because they can be used as an indicator species for past and present seep environments (http: //zoobank.org/urn:lsid:zoobank.org:pub:6075FF30-29D5-4DAB-9141-AE722CD3A69B)

    Cold-seep ostracods from the western Svalbard margin: direct palaeo-indicator for methane seepage?

    Get PDF
    Despite their high abundance and diversity, microfossil taxa adapted to a particular chemosynthetic environment have rarely been studied and are therefore poorly known. Here we report on an ostracod species, Rosaliella svalbardensis gen. et sp. nov., from a cold methane seep site at the western Svalbard margin, Fram Strait. The new species shows a distinct morphology, different from other eucytherurine ostracod genera. It has a marked similarity to Xylocythere, an ostracod genus known from chemosynthetic environments of wood falls and hydrothermal vents. Rosaliella svalbardensis is probably an endemic species or genus linked to methane seeps. We speculate that the surface ornamentation of pore clusters, secondary reticulation, and pit clusters may be related to ectosymbiosis with chemoautotrophic bacteria. This new discovery of specialized microfossil taxa is important because they can be used as an indicator species for past and present seep environments (http: //zoobank.org/urn:lsid:zoobank.org:pub:6075FF30-29D5-4DAB-9141-AE722CD3A69B)

    Data from: Late Quaternary deep-sea ostracode taxonomy of the eastern North Atlantic Ocean

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    Taxonomic revision and re-evaluation of the eastern North Atlantic deep-sea ostracodes are conducted based on late Quaternary sediments from Ocean Drilling Program (ODP) Hole 982A, Rockall Plateau, eastern North Atlantic. Twenty one genera and 51 species were examined and (re-)illustrated with high-resolution scanning electron microscopy images. Six new species are described: Polycope lunaris, Argilloecia labri, Bythoceratina nuda, Cytheropteron colesoabyssorum, Cytheropteron colesopunctatum, and Cytheropteron paramediotumidum. Excellent fossil ostracode preservation in this sediment core enabled us to provide a robust taxonomic baseline of the eastern North Atlantic deep-sea ostracodes for application to palaeoceanographical, palaeoecological, and biogeographical studies

    Data from: Quarternary deep-sea Ostracode taxonomy of ocean drilling program site 980, Easterm North Atlantic Ocean

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    Ocean Drilling Program (ODP) Holes 980 B and C, Feni Drift at the eastern slope of the Rockall Plateau, eastern North Atlantic, were examined for late Quaternary deep-sea ostracode taxonomy. Nineteen genera and 32 species were examined and (re-)illustrated with high-resolution scanning electron microscopy images. One new species Cytheropteron paramassoni n. sp. is described and one new name Eucytherura zehali is proposed for Eucytherura hazeli Yasuhara et al., 2009. This study provides updated taxonomic information for deep-sea ostracode genera and species from the eastern North Atlantic, which is an important baseline for application of deep-sea ostracodes to paleoceanographical reconstructions and paleoecological studies in this region

    ЭтничСскиС ΠΊΠΎΠ½Ρ„Π»ΠΈΠΊΡ‚Ρ‹

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    Π£Ρ‡Π΅Π±.-ΠΌΠ΅Ρ‚ΠΎΠ΄. пособиС для ΠΏΡ€Π°ΠΊΡ‚ΠΈΡ‡. ΠΈ самостоят. Ρ€Π°Π±ΠΎΡ‚ [для студСнтов спСц. 030300.68 Β«ΠŸΡΠΈΡ…ΠΎΠ»ΠΎΠ³ΠΈΡΒ»].Доступ ΠΊ ΠΏΠΎΠ»Π½ΠΎΠΌΡƒ тСксту ΠΎΡ‚ΠΊΡ€Ρ‹Ρ‚ ΠΈΠ· сСти Π‘Π€Π£, Π²Π½Π΅ сСти доступ Π²ΠΎΠ·ΠΌΠΎΠΆΠ΅Π½ для Ρ‡ΠΈΡ‚Π°Ρ‚Π΅Π»Π΅ΠΉ Научной Π±ΠΈΠ±Π»ΠΈΠΎΡ‚Π΅ΠΊΠΈ Π‘Π€Π£ ΠΈΠ»ΠΈ Π·Π° ΠΏΠ»Π°Ρ‚Ρƒ.Π£Ρ‡Π΅Π±Π½ΠΎ-мСтодичСскоС пособиС ΠΏΡ€Π΅Π΄Π½Π°Π·Π½Π°Ρ‡Π΅Π½ΠΎ для ΠΎΡ€Π³Π°Π½ΠΈΠ·Π°Ρ†ΠΈΠΈ ΡΠ°ΠΌΠΎΡΡ‚ΠΎΡΡ‚Π΅Π»ΡŒΠ½ΠΎΠΉ Ρ€Π°Π±ΠΎΡ‚Ρ‹ студСнта Π² соотвСтствии с Π“ΠžΠ‘ Π’ΠŸΠž Π Π€ ΠΏΠΎ ΠΈΠ·ΡƒΡ‡Π΅Π½ΠΈΡŽ ΠΌΠ°Ρ‚Π΅Ρ€ΠΈΠ°Π»Π° ΠΏΠΎ курсу «ЭтничСскиС ΠΊΠΎΠ½Ρ„Π»ΠΈΠΊΡ‚Ρ‹Β» ΠΈ содСрТит мСтодичСскиС указания, ΠΎΠΏΡ€Π΅Π΄Π΅Π»ΡΡŽΡ‰ΠΈΠ΅ состав, объСм Π·Π°Π΄Π°Π½ΠΈΠΉ, Π° Ρ‚Π°ΠΊΠΆΠ΅ трСбования ΠΈ Ρ€Π΅ΠΊΠΎΠΌΠ΅Π½Π΄Π°Ρ†ΠΈΠΈ ΠΏΠΎ Π²Ρ‹ΠΏΠΎΠ»Π½Π΅Π½ΠΈΡŽ Ρ€Π°Π±ΠΎΡ‚, прСдусмотрСнных ΠΈΡ‚ΠΎΠ³ΠΎΠ²Ρ‹ΠΌ ΠΊΠΎΠ½Ρ‚Ρ€ΠΎΠ»Π΅ΠΌ. Π’ обСспСчСниС Π²ΠΊΠ»ΡŽΡ‡Π΅Π½ список основной ΠΈ Π΄ΠΎΠΏΠΎΠ»Π½ΠΈΡ‚Π΅Π»ΡŒΠ½ΠΎΠΉ Π»ΠΈΡ‚Π΅Ρ€Π°Ρ‚ΡƒΡ€Ρ‹, ΠΏΡ€Π΅Π΄Π»Π°Π³Π°Π΅ΠΌΠΎΠΉ студСнту для ΡΠ°ΠΌΠΎΡΡ‚ΠΎΡΡ‚Π΅Π»ΡŒΠ½ΠΎΠ³ΠΎ изучСния ΠΏΠΎ ΠΊΠ°ΠΆΠ΄ΠΎΠΉ Ρ‚Π΅ΠΌΠ΅ курса. ΠŸΡ€Π΅Π΄Π½Π°Π·Π½Π°Ρ‡Π΅Π½ΠΎ для магистров психологии ΠΏΠΎ ΠΏΡ€ΠΎΠ³Ρ€Π°ΠΌΠΌΠ°ΠΌ ΠΏΠΎΠ΄Π³ΠΎΡ‚ΠΎΠ²ΠΊΠΈ, Π½Π°ΠΏΡ€Π°Π²Π»Π΅Π½ΠΈΠ΅ 030300.68 Β«ΠŸΡΠΈΡ…ΠΎΠ»ΠΎΠ³ΠΈΡΒ»

    High resolution Fig. 5

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    High resolution Fig.
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