Gephyrocapsa kennettii sp. nov., a new calcareous nannofossil species from the Middle Pleistocene, Solomon Sea, western equatorial Pacific

被引:0
|
作者
Chuang, Chih-Kai [1 ,2 ]
Wei, Kuo-Yen [1 ,2 ]
Mii, Horng-Sheng [3 ]
Suk, Hui-Ping [1 ]
Lo, Li [1 ,2 ]
机构
[1] Natl Taiwan Univ, Dept Geosci, Taipei 10617, Taiwan
[2] Natl Taiwan Univ, Res Ctr Future Earth, Taipei 10617, Taiwan
[3] Natl Taiwan Normal Univ, Dept Earth Sci, Taipei 10677, Taiwan
关键词
Calcareous nannofossil; Gephyrocapsa; ODP Hole 1115B; Solomon Sea; FLUCTUATIONS; FOSSIL; OCEAN; AGE;
D O I
10.47894/mpal.67.1.01
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
Detailed examinations of middle Pleistocene sediments of ODP Hole 1115B and CoreMD05-2925 in the Solomon Sea, southwest equatorial Pacific, reveal a distinctive new form of the calcareous nannofossil group of gephyrocapsid which has peculiar elongate kite-shaped slits on the distal shields of the coccolith. Anew species, Gephyrocapsa kennettii sp. nov., is proposed and described in this study with SEM (scanning electron microscope) images. The coccolith of this new species is elliptical in shape, bearing 2 to 19 kite-shaped slits on the distal shield and a low-angle, raised arch-like bridge. The distal shield has fewer slits than G. protohuxleyi which has slits in between all elements. The bridge is orientated clockwise with a similar to 10 degrees angle to the long axiswhen viewed distally. The average length of the distal shield is 3.26 +/- 0.22 (1 sigma) mu m(n = 36), and, by definition, this new species belongs to the small Gephyrocapsa group. The chronologic range of this species is short, spanning only from 0.520-0.465 Ma. Its last occurrence datum is almost coeval with that of Pseudoemiliania lacunosa at the bottom of Marine Isotope Stage 12. Morphologically, G. kennettii sp. nov. is intermediate between G. ericsonii and G. protohuxleyi and considered to be a transitional species originated by hybridization between them.
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页码:1 / 10
页数:10
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