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首页> 外文期刊>Neues Jahrbuch fur Geologie und Palaontologie. Abhandlungen >Morphogroups, test shape variability and test asymmetry in Pellatispira crassicolumnata UMBGROVE from the Eocene of Surat-Bharuch (India)
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Morphogroups, test shape variability and test asymmetry in Pellatispira crassicolumnata UMBGROVE from the Eocene of Surat-Bharuch (India)

机译:来自苏拉特-巴鲁奇始新世的印度软体动物Pellatispira crassicolumnata UMBGROVE中的形态群,测试形状变异性和测试不对称性

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摘要

Bilaterally symmetrical and planispirally evolute Pellatispira crassicolumnata UMBGROVE from the middle and upper Eocene shelf successions of Vagalkhod-Tarkesvar area (Gujarat) record variations in test shape, symmetry and coiling, and contain rare joined tests. These aspects are investigated to explore their development. Based on semi-quantitative measurements of test shape parameters from different stratigraphic levels, four categories of test shape were recognized, whereby the flattened lenticular and subglobular tests predominate in the marl and arenaceous marlite while lenticular and inflated lenticular tests show wide distribution. Based on test shape and host lithology, four morphogroups (A-D) are recognized. Morphogroup-A comprising flattened lenticular tests with thin lateral walls, closely spaced short vertical pillars and low apertural face thrived on the soft substrate towards the lower part of the photic zone. Morphogroup-D, characterized by subglobular tests with thick lateral wall, long thick vertical pillars and high apertural face, dwelled on the hard substrate towards at the upper part of the photic zone where high energy and sufficient light prevailed. Morphogroup-B and morphogroup-C comprising respectively of lenticular and inflated lenticular forms generally thrived between the upper (shallow) to lower (deep) levels of the photic zone, though the former dominated on the soft substrate and the latter on the hard substrate. Both apertural face and pillars appear to reflect the light requirements at different depths. Asymmetric tests occur in all morphogroups and sediment types. Asymmetrical tests are shown to originate by modifying growth during ontogeny, or by merging tests in the adult stage.
机译:来自Vagalkhod-Tarkesvar地区(古吉拉特邦)中新世和上新世陆架的双侧对称和平面螺旋渐生的Pellatispira crassicolumnata UMBGROVE记录了测试形状,对称性和卷曲的变化,并且包含罕见的联合测试。对这些方面进行了研究,以探讨它们的发展。基于来自不同地层水平的测试形状参数的半定量测量,可以识别出四类测试形状,其中扁平的柱状镜和球状测试在泥灰岩和砂质大理石中占主导地位,而柱状镜和膨胀的柱状镜显示出广泛的分布。根据测试形状和宿主岩性,可识别四个形态群(A-D)。 Morphogroup-A包括扁平的双凸透镜测试,带有薄的侧壁,紧密间隔的短垂直支柱和低孔眼面,在柔软的基底上朝着光区的下部蓬勃发展。 Morphogroup-D的特征是球状亚测试,侧壁厚,垂直的柱子长且开孔高,在硬质基质上朝着高能量和充足光的光区上部居住。通常分别由双凸透镜和膨胀双凸透镜形式组成的Morphogroup-B和morphogroup-C通常在光区的较高(浅)到较低(较深)水平之间繁荣发展,尽管前者在软质基底上占主导地位,而后者在硬质基底上占主导地位。孔面和柱子似乎都反映了不同深度的光线需求。所有形态组和沉积物类型均进行不对称测试。结果表明,不对称测试是通过改变个体发育过程中的生长或在成年阶段合并测试而产生的。

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