New larger benthic foraminifera from Brac Island, Croatia: Further evidence for early-middle Campanian foraminiferan high diversity in the inner platform facies of the Adriatic Carbonate Platform

被引:2
作者
Schlagintweit, Felix [1 ]
Tesovic, Blanka Cvetko [2 ]
Martinus, Maja [2 ]
Vlahovic, Igor [3 ]
机构
[1] Lerchenauerstr 167, D-80935 Munich, Germany
[2] Univ Zagreb, Fac Sci, Dept Geol, Horvatovac 102a, HR-10000 Zagreb, Croatia
[3] Univ Zagreb, Fac Min Geol & Petr Engn, Pierottijeva 6, HR-10000 Zagreb, Croatia
关键词
Larger benthic foraminifera; Taxonomy; Biostratigraphy; Palaeogeography; Lithofacies; Platform carbonates; Upper Cretaceous; STRONTIUM-ISOTOPE STRATIGRAPHY; CENOMANIAN-TURONIAN BOUNDARY; SEA-LEVEL RISE; ZAGROS ZONE; N; GEN; EVOLUTION; ISLAND; BRAC; BIOSTRATIGRAPHY; CLASSIFICATION;
D O I
10.1016/j.cretres.2023.105667
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Four new species of larger benthic foraminifera are described from lower-middle Campanian inner-platform carbonates of the island of Brac ⠁, Croatia: Bakhtiarella minima sp. nov. (family Bakhtiarellidae), Biconcava brattiana sp. nov. (family Mayncinidae), Paravanneauina campaniana gen. et sp. nov. and Calveziconus pygmaeus sp. nov. (family Orbitolinidae). The latter two taxa are also reported from time-equivalent strata of the Gavrovo-Tripolitza Platform, southwestern Greece. The new taxa provide further evidence for the pronounced Campanian diversification within the Late Cretaceous Global Maturation Cycle of larger benthic foraminifera in the inner platform facies of the Mediterranean Adriatic Carbonate Platform.& COPY; 2023 Elsevier Ltd. All rights reserved.
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页数:17
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