Bioerosion in fossil cephalopods: a case study from the Upper Carboniferous Buckhorn Asphalt Quarry Lagerstätte, Oklahoma, USA
Bioerosion in fossil cephalopods: a case study from the Upper Carboniferous Buckhorn Asphalt Quarry Lagerstätte, Oklahoma, USA
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头足类化石的生物侵蚀：美国俄克拉荷马州上石炭统 Buckhorn 沥青采石场的案例研究
DOI：
10.1007/s10347-018-0547-y
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发表时间：
2019
期刊：
影响因子：
1.8
通讯作者：
Nützel A
中科院分区：
文献类型：
--
作者：
Seuss B;Nützel A
俄克拉荷马州萨尔弗附近的 Buckhorn 沥青采石场 Lagerstätte 的宾夕法尼亚中期（德斯莫因 - 维吉尔）沉积物以硅质碎屑 - 碳酸盐岩为特征。这些沉积物之一是“头足类贝壳灰岩”，其中含有大量的正甲壳动物、卷曲的鹦鹉螺和菊石壳遗骸。这些用于对头足类动物贝壳生物侵蚀的详细研究，以帮助重建古环境并增加对化石头足类动物生物侵蚀的一般知识。铸造并研究了 50 多枚炮弹碎片。本研究中铸造和研究的贝壳包含多种不同的鱼类类型。除了叶绿素和蓝藻痕迹外，还存在红绿藻、真菌和海绵痕迹以及来源不明的痕迹。此外，还有六种类型可能以有孔虫为生产者。在正角兽科中，有 Ichnoreticulina elegans 和 Scoleciaisp 的卷曲形态类型。最常见，而卷曲头足类动物的丰度主要是“超薄型”、“极薄型”和Flagrichnus profundus。总共识别出22种鱼类和-型，其中12种在石炭纪有最古老的记录。直锥体铸件中的鱼类群的连续性表明沉积在鹿角海的深透光到不透光的区域，而卷曲标本的贝壳已经漂流了一段时间；因此，它们更容易受到自养生物的生物侵蚀，直到沉入海底。
The mid-Pennsylvanian (Desmoinesian–Virgilian) deposits from the Buckhorn Asphalt Quarry Lagerstätte near Sulphur, Oklahoma, are characterized by siliciclastic–carbonate rocks. One of these deposits is the ‘cephalopod coquina’ that contains a large amount of orthocerid and coiled nautiloid, and ammonoid shell remains. These were used for a detailed study on bioerosion in cephalopod shells in order to help in the reconstruction of the paleoenvironment and to increase the general knowledge on bioerosion in fossil cephalopods. More than 50 shell fragments were cast and investigated. The shells cast and investigated in this study comprise a diverse set of ichnotaxa-/forms. Besides chlorophyte and cyanobacterial traces, also rhodophyte, fungal, and spongal traces are present as well as those of unknown origin. In addition, there are six ichnoforms that might have foraminiferans as producers. In orthoceratids,Ichnoreticulina elegansand a curly morphotype ofScoleciaisp. are most common while the abundance in coiled cephalopods is dominated by the ‘superthin form’, the ‘extremely thin form’, andFlagrichnus profundus.In total, 22 ichnotaxa and -forms were recognized and 12 of these have their oldest record in the Carboniferous. The succession of ichnotaxa/-forms in the casts of orthocones suggests deposition in the deep euphotic to dysphotic zone of the Buckhorn sea while shells of coiled specimens had drifted for a while; they were therefore more prone to bioerosion by autotrophs until they sank to the seafloor.
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影响因子：
1.1
作者：
A. Radwański
通讯作者：
A. Radwański
影响因子：
3.7
作者：
Seuss B;Wisshak M;Mapes RH;Landman NH
通讯作者：
Landman NH
宾夕法尼亚州鹿角沥青采石场矿床的相和动物群：对具有文石保存的重要古生代化石矿床的回顾和新数据
影响因子：
1.8
作者：
Nützel;Yancey
通讯作者：
Yancey
Ostreobium quekettii（Codiales，绿藻门）
DOI：
10.1007/bf01984034
发表时间：
1980
期刊：
Helgoländer Meeresuntersuchungen
影响因子：
--
作者：
P. Kornmann;P.
通讯作者：
P.
埃及萨法加湾软体动物贝壳中的微钻孔：形态测量和地貌学
影响因子：
1.8
作者：
Gudrun Radtke;S. Golubić
通讯作者：
S. Golubić