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Changes for document Klapperilepis triangularis
From version 785.1
edited by Administrator
on 2025/09/12 06:14
on 2025/09/12 06:14
To version 786.1
edited by Administrator
on 2025/09/12 06:14
on 2025/09/12 06:14
Change comment: There is no comment for this version
Object changes
Object number 2 of type Species.ImageInfoClass modified
- subtitle
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... ... @@ -1,1 +1,1 @@ 1 -Elementy aparatu z próbkiPł-42 z Płucek koło Łagowa, wczesny famen;okazy ZPAL cXVI/1233, 1235, 1237, 1238 i 1239(Dzik 2006).1 +Elementy aparatu z Płucek koło Łagowa, wczesny famen (Dzik 2006).
Object number 0 of type Species.SpeciesClass modified
- Diagnoza
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... ... @@ -1,1 +1,1 @@ 1 - P,,1,, elementsrelativelyelongated and M elements usually with relatively wide angle between processes.1 +From its abcestor, K. ultima, differs in more elongated P,,1,, elements and M elements usually with relatively wide angle between processes, from successors of various lineages in underived, lambda-shaped M elements. - Literatura
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... ... @@ -1,1 +1,8 @@ 1 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. 2 + 3 + 4 +Nehring, M. 1967. Konodonty dolnego famenu z profilu Winowno w okolicach Siewierza (Wyżyna Śląsko−Krakowska). //Biuletyn Instytutu Geologicznego// 209, 113–169. 5 + 6 +Szulczewski, M. 1971. Upper Devonian conodonts, stratigraphy and facies development in the Holy Cross Mts. //Acta Geologica Polonica// 21, 1-129. 7 + 8 +Wolska, Z. 1967. Górno-dewońskie konodonty z południowo-zachodniego regionu Gór Świętokrzyskich. //Acta Palaeontologica Polonica// 12, 363-435. - Holotyp
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... ... @@ -1,1 +1,1 @@ 1 -Sannemann (1955)1 +Sannemann 1955, p. 327, pl. 24:3 SMF XVI 52 - Stratum typicum
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... ... @@ -1,1 +1,1 @@ 1 -Early Famenian odular limestone. 1 +Early Famennian nodular limestone. - Porównanie
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... ... @@ -1,1 +1,1 @@ 1 -A variable species, both in respect to the outline of platform in P,,1,, elements, which ranges from that typical to //K. ultima// to that of early species of //Palmatolepis//, but also in the prominence of the cusp and curvature of P,,2,, elements. The mean value of elongation index of the P,,1,, elements is ,however,distinctly higher than in //K. ultima//(Dzik 2002,2004),remaining elements of the apparatus being hardly distinguishable. In fact, to distinguish these chronospecies a large sample is needed and singlerelements are of little taxonomic value. Some late populations(e.g., Pł-1; Fig. 80H-R)show robust denticulation of ramiform elements and widely angular processes of the M element1 +A variable species, both in respect to the outline of platform in P,,1,, elements, which ranges from that typical to //K. ultima// to that of early species of //Palmatolepis//, but also in the prominence of the cusp and curvature of P,,2,, elements. The mean value of elongation index of the P,,1,, elements is distinctly higher than in //K. ultima//, remaining elements of the apparatus being hardly distinguishable. In fact, to distinguish these chronospecies a large sample is needed and single elements are of little taxonomic value. Some late populations show robust denticulation of ramiform elements and widely angular processes of the M element - Występowanie geograficzne
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... ... @@ -1,1 +1,1 @@ 1 -Płucki, Karczówka, Kowala, and Wietrznia. 1 +Płucki, Kadzielnia, Kostomłoty, Śluchowice, Psie Górki, Dalnia, Górno, Karczówka, Kowala, and Wietrznia in the Holy Cross Mts.; borehole near Siewierz in Upper Silesia