Guido Adriano, Gerovasileiou Vasilis, Russo Franco, Rosso Antonietta, Sanfilippo Rossana, Voultsiadou Eleni, Mastandrea Adelaide
Department of Biology, Ecology and Earth Sciences, University of Calabria, Via Bucci, Cubo 15b, 87036, Rende, Cosenza, Italy.
Institute of Marine Biology, Biotechnology and Aquaculture, Hellenic Centre for Marine Research, 71500, Heraklion, Crete, Greece.
Data Brief. 2019 Nov 4;27:104745. doi: 10.1016/j.dib.2019.104745. eCollection 2019 Dec.
This dataset aims at illustrating the relationships between Metazoa and Bacteria in confined environments. For this purpose, the biotic crusts inside two submarine caves of the Aegean Sea were examined in order to characterize organisms involved in their formation. The present manuscript provides additional data and information to our research article "Composition and biostratinomy of sponge-rich biogenic crusts in submarine caves (Aegean Sea, Eastern Mediterranean)" [1] (Guido et al.). The data were collected with an integrated approach utilizing microfacies observations in optical microscopy and micromorphological and geochemical characterization in electron microscopy (SEM and EPMA). We present here microfacies showing the boundstone framework, which is rich in microcavities partly filled by sponge spicules and scant autochthonous micrite. SEM and EPMA data put in evidence the abundance of sponge spicules inside the crusts and allow discriminating between two types of micrite: detrital micrite and autochthonous micrite. The data presented in this article and those described in Guido et al. [1] allow the evaluation of the relationship between sponges and carbonatogenetic bacteria in the cryptic conditions of submarine caves, and provide new knowledge to interpret the fossil record.
该数据集旨在阐明在受限环境中后生动物与细菌之间的关系。为此,对爱琴海两个海底洞穴内的生物结皮进行了研究,以确定参与其形成的生物特征。本手稿为我们的研究文章《海底洞穴(东地中海爱琴海)富含海绵的生物源结皮的组成和生物地层学》[1](圭多等人)提供了额外的数据和信息。这些数据是通过综合方法收集的,利用光学显微镜下的微相观察以及电子显微镜(扫描电子显微镜和电子探针微分析仪)下的微观形态和地球化学特征分析。我们在此展示了显示粘结岩框架的微相,该框架富含部分由海绵骨针填充的微腔以及少量原地微晶灰岩。扫描电子显微镜和电子探针微分析仪的数据证明了结皮内海绵骨针的丰富性,并能够区分两种类型的微晶灰岩:碎屑微晶灰岩和原地微晶灰岩。本文所呈现的数据以及圭多等人[1]中描述的数据,有助于评估在海底洞穴隐秘环境中海绵与碳酸盐生成细菌之间的关系,并为解释化石记录提供新知识。