Marine bacterial biomineralisation by CaCO precipitation provides natural limestone structures, like beachrocks and stromatolites. Calcareous deposits can also be abiotically formed in seawater at the surface of steel grids under cathodic polarisation. In this work, we showed that this mineral-rich alkaline environment harbours bacteria belonging to different genera able to induce CaCO precipitation. We previously isolated 14 biocalcifying marine bacteria from electrochemically formed calcareous deposits and their immediate environment. By microscopy and µ-Raman spectroscopy, these bacterial strains were shown to produce calcite-type CaCO. Identification by 16S rDNA sequencing provided between 98.5 and 100% identity with genera and . All 14 strains produced carbonic anhydrase, and six were urease positive. Both proteins are major enzymes involved in the biocalcification process. However, this does not preclude that one or more other metabolisms could also be involved in the process. In the presence of urea, CD6 exhibited the most efficient precipitation of CaCO. However, the urease pathway has the disadvantage of producing ammonia, a toxic molecule. We showed herein that different marine bacteria could induce CaCO precipitation without urea. These bacteria could then be used for eco-friendly applications, e.g., the formation of bio-cements to strengthen dikes and delay coastal erosion.
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http://dx.doi.org/10.3390/microorganisms10010076 | DOI Listing |
Zootaxa
August 2024
Laboratório de Micropaleontologia Aplicada (LMA/LAGESE); Instituto de Pesquisa em Petróleo e Energia (LITPEG); Universidade Federal de Pernambuco; Av. da Arquitetura; s/n; 50740-540; Recife; PE; Brazil; Programa de Pós-Graduação em Geociências; Departamento de Geologia; Centro de Tecnologia e Geociências; Universidade Federal de Pernambuco; Av. da Arquitetura; s/n; 50740-540; Recife; PE; Brazil.
The Ostracoda Subclass comprises the most expressive group of calcareous microfossils in the deposits of the Araripe Basin, especially in its post-rift sequence, which is represented by the Santana Group, of Late Aptian age (= Alagoas Local Stage). Due to the abundance, ostracod species are of great importance for understanding the evolution of the Araripe Basin, with direct application in biostratigraphic and paleoecological analyses. Improving these important applications involves refining the taxonomy of these ostracods, which also contributes to understanding the diversity of this fauna.
View Article and Find Full Text PDFHeliyon
November 2024
Agricultural Innovation and Technology Transfer Center (AITTC), Mohammed VI Polytechnic University (UM6P), Ben Guerir, Morocco.
Phosphorus (P) deficiency is one of the major constraints for sustainable crop production in calcareous soils. This study aimed to elucidate the key soil characteristics modulating the variability of soil Olsen P in these typical soils. A comprehensive soil sampling initiative (1.
View Article and Find Full Text PDFMetallomics
December 2024
The SR Center, Ritsumeikan University, Kusatsu, Shiga 525-8577, Japan.
The shell color of Corbicula clams, which are globally distributed, is roughly divided into yellowish and blackish depending on the environmental conditions of the sediment. The formation of an iron-L-3,4-dihydroxyphenylalanine (DOPA) complex in a thin organic layer, called the periostracum, on a calcareous layer causes the blackening of the clamshell. However, the iron-DOPA complex formation mechanism is unclear.
View Article and Find Full Text PDFMar Pollut Bull
November 2024
Programa de Física, Facultad de Ciencias Básicas, Universidad del Atlántico, Barranquilla, Atlántico, Colombia.
This study documents the natural accumulation of mollusk shells on an elevated rocky shore carved into the calcareous rocks of the La Popa formation at Punta Roca (Atlántico), covering an estimated area of 0.35 km. Hydrodynamic transport and differential exposure to environmental conditions are the primary factors contributing to shell deposition.
View Article and Find Full Text PDFLife (Basel)
August 2024
State Key Laboratory of Continental Dynamics, Shaanxi Key Laboratory of Early Life and Environments, Department of Geology, Northwest University, Xi'an 710069, China.
Cnidarians are among the most important diploblastic organisms, elucidating many of the early stages of Metazoan evolution. However, Cnidarian fossils from Cambrian deposits have been rarely documented, mainly due to difficulties in identifying early Cnidarian representatives. , a tabulate coral from Silurian reef systems, serves as a crucial taxon for interpreting Cambrian cnidarians.
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