Metadata changes

Title

SpecConditolepis Tempfalcatea

Parent

Species.Conditolepis distorta

Document author

XWiki.Ajdmzink

Object changes

Object number 0 of type Species.SpeciesClass modified

Diagnoza

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	1	+P,,1 ,,elements very elongate and narrow, with triangular, aborally pointing anterior lobe; P,,2 ,,elements sinuous, with rudimentary platform, S,,0 ,,elements with prominent processes.

Literatura

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	1	+Dzik, J. 2006. The Famennian "Golden Age" of conodonts and ammonoids in the Polish part of the Variscan sea. //Palaeontologia Polonica// 63, 1-359.

Materiały muzealne

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	1	+ZPAL: 41,366 specimens.

Locus typicus

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	1	+Bohlen near Saalfeld, Thuringia.

Stratum typicum

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	1	+Upper part of bed 5.

Porównanie

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	1	+//C. falcata// is the most abundant palmatolepidid species in the Holy Cross Mountains and its apparatus reconstruction leaves little doubt. Sample Ost-12 offers the largest material of this species being devoid of any other //Conditolepis// species.
	2	+
	3	+The origin of this species remains in doubt. The species emerged from an unknown source in the late //K. crepida// Zone at Kadzielnia together with equally cryptic //C. klapperi//. Although relatively little change is necessary in the morphology of the P,,1,, element to derive it from that of //C. glabra//, the whole apparatus is quite different. It cannot be excluded that the lack of a platform in P,,2,, elements is an ancestral feature inherited from //C. lobicornis// and early //C. tenuipunctata// and that the lineage of //C. falcata// is independent of that of //C. glabra//.

Występowanie geograficzne

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	1	+All localities in Holy Cross Mountains.

Zasięg czasowy

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	1	+Common from the C. quadrantinodosa Zone, most abundant in the P. trachytera and L. styriacus Zones.