The emergence of the tropical rainforest biome in the Cretaceous

被引:0
|
作者
Coiffard, Clement [1 ]
El Atfy, Haytham [2 ,3 ,4 ]
Renaudie, Johan [5 ]
Bussert, Robert [6 ]
Uhl, Dieter [7 ,8 ]
机构
[1] Free Univ Berlin, Inst Biol, Struct & Funct Plant Divers Grp, Altensteinstr 6, D-14195 Berlin, Germany
[2] Univ Tubingen, Dept Geosci, D-72076 Tubingen, Germany
[3] Mansoura Univ, Fac Sci, Geol Dept, Mansoura 35516, Egypt
[4] Univ Munster, Inst Geol & Palaeontol, Palaeobotany Grp, D-48149 Munster, Germany
[5] Leibniz Inst Evolut & Biodiversitatsforsch, Museum Naturkunde, Invalidenstr 43, D-10115 Berlin, Germany
[6] Tech Univ Berlin, Inst Appl Geosci, D-10587 Berlin, Germany
[7] Senckenberg Res Inst, D-60325 Frankfurt, Germany
[8] Nat Hist Museum Frankfurt, D-60325 Frankfurt, Germany
关键词
ARACEAE; DIVERSITY; CLIMATE; STRATA; ORIGIN; MEMBER; EGYPT; GEN; NOV;
D O I
10.5194/bg-20-1145-2023
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Modern tropical rainforests (TRFs) are one of the mostecologically important and species-rich biomes on the planet. However, theorigin of modern TRFs is still debated, especially due to the incongruencebetween the fossil record and molecular data. Here, we test whetherCampanian assemblages from northeastern Africa could represent fossil TRFvegetation. In so doing, we compare the investigated assemblages with otherassemblages known to represent temperate forests, subtropical forests, andTRF in terms of leaf physiognomy, species richness, and taxonomiccomposition. We conclude based on fossil leaves that modern-looking TRFsalready existed since 80 Ma during the Campanian in northeastern Africain an area corresponding to 10 % of the modern Amazonian or 25 % of theCongolese TRF. The apparent conflict between the fossil record andphylogenetic evidence is due to the nearly complete absence of publishedtropical floras for the Cretaceous.
引用
收藏
页码:1145 / 1154
页数:10
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