Calcium orthophosphates (CaPO4): occurrence and properties
SV Dorozhkin - Progress in biomaterials, 2016 - Springer
The present overview is intended to point the readers' attention to the important subject of
calcium orthophosphates (CaPO 4). This type of materials is of the special significance for …
calcium orthophosphates (CaPO 4). This type of materials is of the special significance for …
Bacteria-induced mineral precipitation: a mechanistic review
TD Hoffmann, BJ Reeksting, S Gebhard - Microbiology, 2021 - microbiologyresearch.org
Micro-organisms contribute to Earth's mineral deposits through a process known as bacteria-
induced mineral precipitation (BIMP). It is a complex phenomenon that can occur as a result …
induced mineral precipitation (BIMP). It is a complex phenomenon that can occur as a result …
Defining “serious harm” to the marine environment in the context of deep-seabed mining
Increasing interest in deep-seabed mining has raised many questions surrounding its
potential environmental impacts and how to assess the impacts' significance. Under the …
potential environmental impacts and how to assess the impacts' significance. Under the …
Subseafloor life and its biogeochemical impacts
Subseafloor microbial activities are central to Earth's biogeochemical cycles. They control
Earth's surface oxidation and major aspects of ocean chemistry. They affect climate on long …
Earth's surface oxidation and major aspects of ocean chemistry. They affect climate on long …
Comprehensive REE+ Y and sensitive redox trace elements of Algerian phosphorites (Tébessa, eastern Algeria): A geochemical study and depositional environments …
R Kechiched, R Laouar, O Bruguier, L Kocsis… - Journal of Geochemical …, 2020 - Elsevier
The Algerian sedimentary phosphorites of marine origin are located mainly in the Tébessa
region, which is part of the Eastern Saharan Atlas. These phosphorites are hosted by …
region, which is part of the Eastern Saharan Atlas. These phosphorites are hosted by …
Palaeoproterozoic oxygenated oceans following the Lomagundi–Jatuli Event
K Mänd, SV Lalonde, LJ Robbins, M Thoby… - Nature …, 2020 - nature.com
Abstract The approximately 2,220–2,060 million years old Lomagundi–Jatuli Event was the
longest positive carbon isotope excursion in Earth history and is traditionally interpreted to …
longest positive carbon isotope excursion in Earth history and is traditionally interpreted to …
[HTML][HTML] The impact of transport processes on rare earth element patterns in marine authigenic and biogenic phosphates
G Auer, M Reuter, CA Hauzenberger… - … et Cosmochimica Acta, 2017 - Elsevier
Rare earth elements (REEs) are commonly used proxies to reconstruct water chemistry and
oxygen saturation during the formation of authigenic and biogenic phosphates in marine …
oxygen saturation during the formation of authigenic and biogenic phosphates in marine …
Characterization of Ca-phosphate biological materials by scanning transmission X-ray microscopy (STXM) at the Ca L2, 3-, P L2, 3-and C K-edges
Several naturally occurring biological materials, including bones and teeth, pathological
calcifications, microbial mineral deposits formed in marine phosphogenesis areas, as well …
calcifications, microbial mineral deposits formed in marine phosphogenesis areas, as well …
A review of phosphate mineral nucleation in biology and geobiology
Relationships between geological phosphorite deposition and biological apatite nucleation
have often been overlooked. However, similarities in biological apatite and phosphorite …
have often been overlooked. However, similarities in biological apatite and phosphorite …
Glauconite-bearing sedimentary phosphorites from the Tébessa region (eastern Algeria): Evidence of REE enrichment and geochemical constraints on their origin
R Kechiched, R Laouar, O Bruguier… - Journal of African Earth …, 2018 - Elsevier
Rare earth element (REE) analyses are reported on glauconite-bearing phosphorites from
northeastern Algeria. These rocks of Paleocene-Eocene age are located in the Eastern part …
northeastern Algeria. These rocks of Paleocene-Eocene age are located in the Eastern part …