Erratum to: New insights into Lithocodium aggregatum Elliott 1956 and Bacinella irregularis Radoičić 1959 (Late Jurassic–Lower Cretaceous): two ulvophycean green algae (?Order Ulotrichales) with a heteromorphic life cycle (epilithic/euendolithic)

Schlagintweit, Félix; Bover‐Arnal, Telm; Salas, R.

doi:10.1007/s10347-010-0223-3

Cited by 16 publications

(2 citation statements)

References 94 publications

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“…The relative abundance of Protopeneroplis striata in the olistolith studied, as well as the presence of planktonic foraminifera, is suggestive of original deposition on the upper slope. This view is supported by the occurrence of Lithocodium/Pseudolithocodium, also known from shallow-to deeper-water settings (see Schlagintweit et al, 2010). We conclude that the Upper Jurassic olistolith that has yielded the decapod crustaceans described here developed in the central parastromatoporoid zone of a Jurassic coral reef complex.…”

Section: Palaeoecology and Palaeoenvironmentsupporting

confidence: 76%

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Mesogalathea ardua sp. nov., a new species of squat lobster (Decapoda, Galatheidae) from the Upper Jurassic olistolith at Velika Strmica (Dolenjska, Slovenia)

Gašparič¹,

Robins²,

Gale³

2020

Geologija

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Mesogalathea ardua sp. nov., a new species of squat lobster (Decapoda, Galatheidae) from the Upper Jurassic olistolith at Velika Strmica (Dolenjska, Slovenia) Nova vrsta raka Mesogalathea ardua sp. nov. (Decapoda, Galatheidae) iz zgornjejurskega olistolita pri Veliki Strmici (Dolenjska, Slovenija) Abstract A new species of squat lobster, Mesogalathea ardua sp. nov., is described on the basis of newly collected dorsal carapaces from an Upper Jurassic reefal limestone olistolith at Velika Strmica. The fossiliferous olistolith is situated within Upper Cretaceous flysch-type deposits, but originally formed within the central parastromatoporoid zone of a Jurassic reef complex. Mesogalathea ardua sp. nov. represents the first formal description of a Jurassic squat lobster from Slovenia and extends the known palaeobiogeographical distribution of galatheoid anomurans. IzvlečekPredstavljena je nova zgornjejurska vrsta raka skakača Mesogalathea ardua sp. nov., opisana na podlagi na novo zbranih primerkov iz grebenskega olistolita pri Veliki Strmici. S fosili bogat olistolit se nahaja znotraj zgornjekrednih flišnih plasti, njegov izvor pa je v parastromatoporoidni coni centralnega dela jurskega koralnega grebena. Novo opisana vrsta Mesogalathea ardua sp. nov. je prvi opis jurskega raka skakača iz Slovenije in širi do sedaj znano paleobiogeografsko razširjenost galatheoidnih rakov.

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Section: Palaeoecology and Palaeoenvironmentsupporting

confidence: 76%

“…Most of these are tabular sponges; corals and brachiopods are subordinate. Sponges and corals are commonly encrusted by Lithocodium/ Pseudolithocodium-like crusts (see comments in Schlagintweit et al, 2010), sessile foraminifera, serpulids, red algae and sponges. Serpulids are also found within internal canals of sponges.…”

Section: Description Of Olistolithmentioning

confidence: 99%

Mesogalathea ardua sp. nov., a new species of squat lobster (Decapoda, Galatheidae) from the Upper Jurassic olistolith at Velika Strmica (Dolenjska, Slovenia)

Gašparič¹,

Robins²,

Gale³

2020

Geologija

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Microfossil assemblages and relative sea-level fluctuations in a lagoon at the Oxfordian/Kimmeridgian boundary (Upper Jurassic) in the eastern part of the Paris Basin

Lefort

Lathuilière

Carpentier

et al. 2011

Facies

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The Late Oxfordian-Early Kimmeridgian interval of the eastern part of the Paris Basin is characterized by a carbonate succession deposited in shallowmarine platform environments. The Gudmont-Villiers section is represented by deposits ranging from barrier to typical lagoonal environments often poor in macrofossils. Previously unpublished calcareous microfossils are more abundant and provide alternative paleoenvironmental indicators. They also provide a biostratigraphical framework across the Oxfordian-Kimmeridgian boundary. The evolution of microfossil associations (algae and benthic foraminifera) in the lower part of the section, based on statistical analyses, is correlated to the sea-level variations. The first highly diversified association composed of small agglutinated and calcitic foraminifera (miliolids, textulariids, Spirillina, Trocholina, Molherina basiliensis etc.) characterizes high sea-level deposits; a second association richer in large agglutinated foraminifera (Alveosepta jaccardi, Everticyclammina, Nautiloculina oolithica) is significantly abundant in low sea-level deposits. A third association characterizes beds with a significant occurrence of encrusting microorganisms and algae (Lithocodium aggregatum, Troglotella incrustans, Cayeuxia piae, dasycladaceans). The upper part of the section is marked by more argillaceous beds and by the occurrence of one opportunist taxon (Lenticulina). This study shows that the microfaunaflora evolution in an internal carbonate platform environment constitute an efficient tool to determine variations in the relative sea level.

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Erratum to: Microfossil assemblages and relative sea-level fluctuations in a lagoon at the Oxfordian/Kimmeridgian boundary (Upper Jurassic) in the eastern part of the Paris Basin

Lefort

Lathuilière

Carpentier

et al. 2011

Facies

View full text Add to dashboard Cite

Erratum to: New insights into Lithocodium aggregatum Elliott 1956 and Bacinella irregularis Radoičić 1959 (Late Jurassic–Lower Cretaceous): two ulvophycean green algae (?Order Ulotrichales) with a heteromorphic life cycle (epilithic/euendolithic)

Abstract: The Late Jurassic-Lower Cretaceous microorganisms incertae sedis Lithocodium aggregatum Elliott and

Cited by 16 publications

References 94 publications

Mesogalathea ardua sp. nov., a new species of squat lobster (Decapoda, Galatheidae) from the Upper Jurassic olistolith at Velika Strmica (Dolenjska, Slovenia)

Mesogalathea ardua sp. nov., a new species of squat lobster (Decapoda, Galatheidae) from the Upper Jurassic olistolith at Velika Strmica (Dolenjska, Slovenia)

Microfossil assemblages and relative sea-level fluctuations in a lagoon at the Oxfordian/Kimmeridgian boundary (Upper Jurassic) in the eastern part of the Paris Basin

Erratum to: Microfossil assemblages and relative sea-level fluctuations in a lagoon at the Oxfordian/Kimmeridgian boundary (Upper Jurassic) in the eastern part of the Paris Basin

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