Xinyi Liu, Yu Li, Jianrui Zha, Xiangna Han, Hao Wang
{"title":"中国盛北峪沉船出水的龙泉青瓷(公元 14 世纪)上附着的管状 凝固物的生物污损和生物矿化:一项多分析案例研究","authors":"Xinyi Liu, Yu Li, Jianrui Zha, Xiangna Han, Hao Wang","doi":"10.1186/s40494-024-01352-9","DOIUrl":null,"url":null,"abstract":"<p>A comprehensive multi-analytical investigation was conducted on a piece of Longquan celadon excavated from the Shengbeiyu shipwreck site in the East China Sea. This study focused on a representative type of tubular bio-concretions attached to the submerged celadon, believed to have been formed through the construction activities of a marine tubeworm belonging to the benthic phylum of <i>Polychaeta Annelids.</i> The research examined the microstructure, composition and adhesion form of these tubular bio-concretions, aiming to elucidate their developmental and attachment patterns from a biomineralization and biofouling perspective. The tubular bio-concretions were found to have a bimineralic composition, with notably higher content of aragonite than calcite, and display diverse yet highly ordered microstructures. The presence of organic matter within the bio-concretions indicates an organic matrix-controlled crystallization model, commonly observed in the construction of benthic calcareous tubes. Microscopic analyses revealed the primary degradation microstructures and corresponding phases of the glaze to which calcareous tubes attached. These findings closely resembled the corrosion characteristics observed in submerged ceramic glaze without bio-concretion attachments, as documented in earlier studies. OM and SEM observations also indicated that the calcareous tubes intricately intermeshed with the cracked glaze layer of the celadon. Additionally, Raman spectroscopic analysis detected the presence of proteins at the interface, likely residual adhesives secreted by fouling organisms to cement themselves to the settlement substrata, suggesting the occurrence of organic-mediated bio-adhesion mechanisms. These results shed new light on the formation process of bio-concretions and their interaction with attached underwater ceramics. A simplified formation mechanism of this biologically-induced degradation has been discussed.</p>","PeriodicalId":13109,"journal":{"name":"Heritage Science","volume":"40 1","pages":""},"PeriodicalIF":2.6000,"publicationDate":"2024-07-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Biofouling and biomineralization of tubular concretions attached to Longquan celadon from Shengbeiyu shipwreck, China (14th Century CE): a multi-analytical case study\",\"authors\":\"Xinyi Liu, Yu Li, Jianrui Zha, Xiangna Han, Hao Wang\",\"doi\":\"10.1186/s40494-024-01352-9\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>A comprehensive multi-analytical investigation was conducted on a piece of Longquan celadon excavated from the Shengbeiyu shipwreck site in the East China Sea. This study focused on a representative type of tubular bio-concretions attached to the submerged celadon, believed to have been formed through the construction activities of a marine tubeworm belonging to the benthic phylum of <i>Polychaeta Annelids.</i> The research examined the microstructure, composition and adhesion form of these tubular bio-concretions, aiming to elucidate their developmental and attachment patterns from a biomineralization and biofouling perspective. The tubular bio-concretions were found to have a bimineralic composition, with notably higher content of aragonite than calcite, and display diverse yet highly ordered microstructures. The presence of organic matter within the bio-concretions indicates an organic matrix-controlled crystallization model, commonly observed in the construction of benthic calcareous tubes. Microscopic analyses revealed the primary degradation microstructures and corresponding phases of the glaze to which calcareous tubes attached. These findings closely resembled the corrosion characteristics observed in submerged ceramic glaze without bio-concretion attachments, as documented in earlier studies. OM and SEM observations also indicated that the calcareous tubes intricately intermeshed with the cracked glaze layer of the celadon. Additionally, Raman spectroscopic analysis detected the presence of proteins at the interface, likely residual adhesives secreted by fouling organisms to cement themselves to the settlement substrata, suggesting the occurrence of organic-mediated bio-adhesion mechanisms. These results shed new light on the formation process of bio-concretions and their interaction with attached underwater ceramics. 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Biofouling and biomineralization of tubular concretions attached to Longquan celadon from Shengbeiyu shipwreck, China (14th Century CE): a multi-analytical case study
A comprehensive multi-analytical investigation was conducted on a piece of Longquan celadon excavated from the Shengbeiyu shipwreck site in the East China Sea. This study focused on a representative type of tubular bio-concretions attached to the submerged celadon, believed to have been formed through the construction activities of a marine tubeworm belonging to the benthic phylum of Polychaeta Annelids. The research examined the microstructure, composition and adhesion form of these tubular bio-concretions, aiming to elucidate their developmental and attachment patterns from a biomineralization and biofouling perspective. The tubular bio-concretions were found to have a bimineralic composition, with notably higher content of aragonite than calcite, and display diverse yet highly ordered microstructures. The presence of organic matter within the bio-concretions indicates an organic matrix-controlled crystallization model, commonly observed in the construction of benthic calcareous tubes. Microscopic analyses revealed the primary degradation microstructures and corresponding phases of the glaze to which calcareous tubes attached. These findings closely resembled the corrosion characteristics observed in submerged ceramic glaze without bio-concretion attachments, as documented in earlier studies. OM and SEM observations also indicated that the calcareous tubes intricately intermeshed with the cracked glaze layer of the celadon. Additionally, Raman spectroscopic analysis detected the presence of proteins at the interface, likely residual adhesives secreted by fouling organisms to cement themselves to the settlement substrata, suggesting the occurrence of organic-mediated bio-adhesion mechanisms. These results shed new light on the formation process of bio-concretions and their interaction with attached underwater ceramics. A simplified formation mechanism of this biologically-induced degradation has been discussed.
期刊介绍:
Heritage Science is an open access journal publishing original peer-reviewed research covering:
Understanding of the manufacturing processes, provenances, and environmental contexts of material types, objects, and buildings, of cultural significance including their historical significance.
Understanding and prediction of physico-chemical and biological degradation processes of cultural artefacts, including climate change, and predictive heritage studies.
Development and application of analytical and imaging methods or equipments for non-invasive, non-destructive or portable analysis of artwork and objects of cultural significance to identify component materials, degradation products and deterioration markers.
Development and application of invasive and destructive methods for understanding the provenance of objects of cultural significance.
Development and critical assessment of treatment materials and methods for artwork and objects of cultural significance.
Development and application of statistical methods and algorithms for data analysis to further understanding of culturally significant objects.
Publication of reference and corpus datasets as supplementary information to the statistical and analytical studies above.
Description of novel technologies that can assist in the understanding of cultural heritage.