A new species of Pseudotsuga (Pinaceae) from the lower Miocene of Lesvos, Greece, and its palaeogeographical and palaeoclimatic implications

被引:1
作者
Zhu, Yan-Bin [1 ,2 ,3 ]
Li, Ya [1 ]
Zhang, Jian-Ping [4 ]
Wang, Yong-Dong [1 ]
Zouros, Nikolaos [3 ,5 ]
机构
[1] Chinese Acad Sci, State Key Lab Palaeobiol & Stratig, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Univ Aegean, Dept Geog, Mitilini 81103, Greece
[4] China Univ Geosci, Geoheritage Res Ctr, Beijing 100083, Peoples R China
[5] Nat Hist Museum Lesvos Petrified Forest, Sigri 81103, Lesvos, Greece
基金
中国国家自然科学基金;
关键词
Pseudotsuga; fossil wood; early Miocene; palaeogeography; Lesvos Petrified Forest; PETRIFIED FOREST; LESBOS; FLORAS; WOODS;
D O I
10.1016/j.palwor.2024.06.001
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
Pseudotsuga Carrie`re is commonly known as Douglas-fir, a minor genus attributed to Pinaceae of conifer. Four extant species are included in this genus, with dispersed distribution in East Asia and western North America. Pseudotsuga possesses a number of fossil records of needled leaves, seed cones, and seeds. Nevertheless, few reliable fossil wood of this genus has been specifically investigated. Here, we describe some anatomically well-preserved petrified fossil wood from the lower Miocene of Lesvos Island, Greece, as Pseudotsuga lesvosensis n. sp. The studied fossil wood remains are characterized by the presence of normal axial and radial resin canals, piceoid cross-field pitting, along with distinctive helical thickenings in cell walls consistent with Pseudotsuga. The present fossil conifer further enriches the species diversity of the Miocene Petrified Forest in Lesvos. The first report of Pseudotsuga lesvosensis from the southern Europe in this study extends the tempo-spatial distribution patterns of Pseudotsuga and contributes to further understanding of its origin and evolutionary history. The occurrence of P. lesvosensis fossil wood, as well as other palaeontological macrofloral composition evidence, indicates a humid warm temperate to subtropical climatic condition during the early Miocene within the Lesvos, which differs significantly from the current Mediterranean climate. (c) 2024 Elsevier B.V. and Nanjing Institute of Geology and Palaeontology, CAS. All rights are reserved, including those for text and data mining, AI training, and similar technologies.
引用
收藏
页数:14
相关论文
共 71 条
[1]  
Axelrod D.I., 1991, The Early Miocene Buffalo Canyon flora of western Nevada
[2]   IAWA list of microscopic features for softwood identification - Preface [J].
Baas, P ;
Blokhina, N ;
Fujii, T ;
Gasson, P ;
Grosser, D ;
Heinz, I ;
Ilic, J ;
Jiang, XM ;
Miller, R ;
Newsom, LA ;
Noshiro, S ;
Richter, HG ;
Suzuki, M ;
Terrazas, T ;
Wheeler, E ;
Wiedenhoeft, A .
IAWA JOURNAL, 2004, 25 (01) :1-+
[3]  
Blokhina NI, 2004, PALEONTOL J+, V38, P327
[4]  
Borsi S., 1972, B VOLCANOL, V36, P473, DOI DOI 10.1007/BF02597122
[5]  
Chelebaeva A.I., 1979, Stratigraphy and Flora of the Continental Neogene in the Far East, P30
[6]  
Czaja A., 2000, Feddes Repertorium, V111, P129
[7]   The Miocene floras of Iceland and their significance for late Cainozoic North Atlantic biogeography [J].
Denk, T ;
Grímsson, F ;
Kvacek, Z .
BOTANICAL JOURNAL OF THE LINNEAN SOCIETY, 2005, 149 (04) :369-417
[8]  
Dolezych M., 2001, Feddes Repertorium, V112, P1
[9]  
DORF ERLING, 1930, CARNEGIE INST WASHINGTON PUBL, V412, P1
[10]  
Farjon A., 1990, PINACEAE, P330