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

IF 1.3 4区 地球科学 Q3 PALEONTOLOGY Micropaleontology Pub Date : 2021-01-01 DOI:10.47894/mpal.67.1.01
C. Chuang, K. Wei, H. Mii, Hui-Ying Suk, L. Lo
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引用次数: 1

Abstract

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. A new 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 am approximate 10 degree angle to the long axis when viewed distally. The average length of the distal shield is 3.26 plus or minus 0.22 (1 theta) 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 coevalwith 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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赤道西太平洋所罗门海中更新世钙质纳米化石一新种Gephyrocapsa kennettii sp. nov.
通过对赤道太平洋西南所罗门海ODP 1115B孔和CoreMD05-2925孔中更新世沉积物的详细研究,发现了一种独特的钙质球壳纳米化石群,在球岩远端盾状结构上具有独特的细长风筝状裂缝。本文提出了一新种Gephyrocapsa kennettii sp. nov.,并利用扫描电镜对其进行了描述。这个新种的球骨是椭圆形的,在远端的盾上有2到19个风筝形状的裂缝和一个低角度的,凸起的拱形桥。远端护盾的缝隙比原赫胥黎的少,后者在所有元素之间都有缝隙。桥沿顺时针方向,与长轴有大约10度角,远观时。远端盾的平均长度为3.26±0.22 (1 θ) μ m (n = 36),根据定义,该新种属于小型Gephyrocapsa类群。该物种的年代学范围较短,仅跨越0.520 ~ 0.465 Ma。它的最后一次产状基准面与海洋同位素第12期底部的lacunosa Pseudoemiliania的产状基准面几乎一致。在形态上,kennettii sp. 11 .介于G. ericsonii和G. protohuxleyi之间,被认为是由两者杂交产生的过渡物种。
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来源期刊
Micropaleontology
Micropaleontology 地学-古生物学
CiteScore
3.20
自引率
6.70%
发文量
18
审稿时长
>12 weeks
期刊介绍: The Journal of Micropalaeontology (JM) is an established international journal covering all aspects of microfossils and their application to both applied studies and basic research. In particular we welcome submissions relating to microfossils and their application to palaeoceanography, palaeoclimatology, palaeobiology, evolution, taxonomy, environmental change and molecular phylogeny. Owned by The Micropalaeontological Society, the scope of the journal is broad, demonstrating the application of microfossils to solving broad geoscience issues.
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