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In the light of the paleoenvironmental significance reflected by the radiolaria, graptolite, brachiopod,sponge spicule and the rock character, its suggested that the greyish green mudstone at the basal WufengFormation of the Goujiaya section would be probably deposited in 60 to 100 meters deep water, theGuanyinqiao bed in 50 to 80 meters deep, and the radiolaria-bearing silicalite from Wufeng Formation inwater with 200 to 400 meters deep. Combining the above-mentioned water depth with the sea-level changecycles, the change range of every one of the 5 cycles could be further conjectured. They were in ascendingorder: 20~120 m, 80~130 m, about 150 m, 50~250 m, and in excess of 200 m.
根据放射虫、笔石、腕足类、海绵骨针以及岩性等对古环境的指示意义,认为五峰组底部灰绿色泥岩段产出时水深约60-100m,观音桥层水深约50-80m,在晚奥陶世最大海侵期(对应于T.typicus亚带下部),水深约400m,五峰组含放射虫硅质岩沉积时最小水深约200m,结合以上海平面变化的5次旋回,从而推算出各旋回海平面的变化幅度:在第①旋回,海平面变化范围大致为20~120m;在第②、第③和第④旋回中,海平面变化分别为80~130 m、大约150 m和50~250m;第⑤旋回的海平面升降幅度大于200 m。
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Analysis of the morphological feature, diversity and abundance of graptolite, brachiopod and radiolaria indicated that the sea-level in the Yangtze basin underwent the change from rising to falling, then to rising again during the latest Ordovician to the earliest Silurian interval, and the maxium rising episode eppeared in the lower Tangyagraptus typicus Subzone and the maxium falling at the top of the Guanyinqiao bed.
笔石、腕足类、放射虫的形态、分异度和丰度的研究表明:扬子海盆晚奥陶世晚期至志留纪初期,总体上,海平面经历了上升→下降→上升的变化,海平面上升的最大阶段发生在Tangyagraptus typicus亚带下部,到观音桥层顶部,海平面下降到最低点。
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In the light of the palenenvironmental significance reflected by the radiolaria, graptolite, brachiopod, sponge spicule and the rock character, it's suggested that the grayish green mudstone at the basal Wufeng Formation of the Goujiaya section would be probably deposited in 60 to 100meters deep water, the Guanyinqiao bed in 50 to 80meters deep, and the radiolaria-bearing silicalite from Wufeng Formation in water with 200 to 400 meters deep. Combining the above-mentioned water depth with the sea-level change cycles, the change range of every one of the 5 cycles could be further conjectured. They were in ascending order: 20~120m, 80~130m, about 150m, 50~250m, and in excess of 200m.
根据放射虫、笔石、腕足类、海绵骨针以及岩性等对古环境的指示意义,认为五峰组底部灰绿色泥岩段产出时水深约60-100m,观音桥层水深约50-80m,在晚奥陶世最大海侵期(对应于T.typicus亚带下部),水深约400m,五峰组含放射虫硅质岩沉积时最小水深约200m,结合以上海平面变化的5次旋回,从而推算出各旋回海平面的变化幅度:在第①旋回,海平面变化范围大致为20~120m;在第②、第③和第④旋回中,海平面变化分别为80~130m、大约150m和50~250m;第⑤旋回的海平面升降幅度大于200m。
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Radiolaria is an important fauna among the marine micropaleontology, whose ecology knowledge is the base of paleoceanographical and paleoenvironmental reconstruction.
中国加入综合大洋钻探计划,势必会加快[JP2]我国古海洋学的研究步伐,放射虫作为海洋微体古生物中的一个重要类群,其生态学知识是重建古海洋、古环境的基础。
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Distribution of biogenic silica content in surface sediments from deep water areas showed that it could not only reflect the paleoproductivity of siliceous micropaleontology in surface waters, but also indicate the strong or feeble upwelling. Thus, it was further confirmed that using biogenic silica content in sediments to trace upwelling and its change was effective and reliable. The analyzed result showed that radiolaria and poriferous specula have more contribution for biogenic opal, comparing with diatom in surface sediments from the northern studied area, probably owing to the diatom dissolved easily away and eaten by other organisms with little effort.
深水区表层沉积物中生物硅的含量分布表明,其不仅能反映出表层水体中硅质生物的古生产力水平,而且还能指示上升流的强弱,从而进一步证实了利用沉积物中生物硅含量来追踪上升流发育和变化的有效性与可信度研究结果还显示,在研究区域中北部表层沉积生物硅中放射虫和海绵骨针较硅藻占有更大的比重,这可能是由于硅藻易被溶解并易被其他生物体摄食的缘故。
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radiolaria:放射虫类
海洋原虫包括有孔虫类(Foraminifera)与放射虫类(Radiolaria)以及许多鞭毛虫与纤毛虫,此等原虫大量出现于浮游植物栖息之区域. 同时,浮游动物性动物以浮游植物性生物、各种细菌或碎屑等为食物. 白画期间浮游动物垂直向下移动生活于光合作用区之下,
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radiolaria:放射虫
砂壳虫(Difflugia) 太阳虫(Heliozoa) 放射虫(Radiolaria)孢子虫纲(Sarcodina)的原虫全部营寄生生活,以寄主体液或组织为养料,可引起疾病. 成体无伪足、纤毛或鞭毛,故不能活动. 一般是有性生殖(配子)和无性生殖(裂体)交替进行.
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radiolaria:放射虫目
辐足纲放射虫目(Radiolaria)原生动物之通称.全在海洋中营漂浮生活.身体通常球状,觶kf5969277lvyouぶ实闹醒肽医珃kf5477877lvyou分为明确的外质与内质,中央囊的形状与奶头、手指或其他物体碰到嘴唇,新生儿立即作出吃奶的动作.这是一种食物性无条件反射,
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radiolaria:射形原虫类
radioisotope 放射性同位素 | radiolaria 射形原虫类 | radiolarian 射形原虫类
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radiolaria ooze:放射虫软泥
raceway 流水路 | radiolaria ooze 放射虫软泥 | raindow trout 虹鳟
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