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Fernández J, Escayo J, Camacho AG, Palano M, Prieto JF, Hu Z, Samsonov SV, Tiampo KF, Ancochea E. Shallow magmatic intrusion evolution below La Palma before and during the 2021 eruption. Sci Rep 2022; 12:20257. [PMID: 36509802 PMCID: PMC9744821 DOI: 10.1038/s41598-022-23998-w] [Citation(s) in RCA: 4] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/19/2022] [Accepted: 11/08/2022] [Indexed: 12/14/2022] Open
Abstract
La Palma, Canary Islands, underwent volcanic unrest which culminated in its largest historical eruption. We study this unrest along 2021 using Interferometric Synthetic Aperture Radar (InSAR) and a new improved interpretation methodology, comparing achieved results with the crustal structure. We reproduce the final phase of La Palma volcanic unrest, highligthing a shallow magma accumulation which begins about 3.5 months before the eruption in a crustal volume charactherized by low density and fractured rocks. Our modeling, together with our improved pictures of the crustal structure, allows us to explain the location and characteristics of the eruption and to detect failed eruption paths. These can be used to explain post-eruptive phenomena and hazards to the local population, such as detected gases anomalies in La Bombilla and Puerto Naos. Our results have implications for understanding volcanic activity in the Canaries and volcano monitoring elsewhere, helping to support decision-making and providing significant insights into urban and infrastructure planning in volcanic areas.
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Affiliation(s)
- José Fernández
- grid.473617.0Instituto de Geociencias (CSIC, UCM). Calle del Doctor Severo Ochoa, nº 7, Ciudad Universitaria, 28040 Madrid, Spain
| | - Joaquin Escayo
- grid.473617.0Instituto de Geociencias (CSIC, UCM). Calle del Doctor Severo Ochoa, nº 7, Ciudad Universitaria, 28040 Madrid, Spain
| | - Antonio G. Camacho
- grid.473617.0Instituto de Geociencias (CSIC, UCM). Calle del Doctor Severo Ochoa, nº 7, Ciudad Universitaria, 28040 Madrid, Spain
| | - Mimmo Palano
- grid.470198.30000 0004 1755 400XIstituto Nazionale di Geofisica e Vulcanologia, Osservatorio Etneo - Sezione di Catania, Piazza Roma 2, 95125 Catania, Italy
| | - Juan F. Prieto
- grid.5690.a0000 0001 2151 2978ETS de Ingenieros en Topografía, Geodesia y Cartografía, Universidad Politécnica de Madrid, 28031 Madrid, Spain
| | - Zhongbo Hu
- Dares Technology, C/ Esteve Terrades, 1, Building RDIT Office 117, Parc UPC – PMT 08860, Castelldefels, Barcelona, Spain ,grid.6835.80000 0004 1937 028XAlso at CommSensLab, Dep. Signal Theory and Communications, Universitat Politècnica de Catalunya (UPC), D3-Campus Nord-UPC, C. Jordi Girona 1-3, 08034 Barcelona, Spain ,grid.473617.0Present Address: Instituto de Geociencias (CSIC, UCM). Calle del Doctor Severo Ochoa, nº 7, Ciudad Universitaria, 28040 Madrid, Spain
| | - Sergey V. Samsonov
- grid.202033.00000 0001 2295 5236Canada Centre for Mapping and Earth Observation, Natural Resources Canada, 560 Rochester Street, Ottawa, ON K1A 0E4 Canada
| | - Kristy F. Tiampo
- grid.266190.a0000000096214564Cooperative Institute for Research in Environmental Sciences (CIRES), 216UCB, University of Colorado at Boulder, Boulder, CO 80309 USA
| | - Eumenio Ancochea
- grid.4795.f0000 0001 2157 7667Departamento de Mineralogía y Petrología, Fac. CC. Geológicas, Universidad Complutense de Madrid, 28040 Madrid, Spain
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Fernandez J, Prieto JF, Escayo J, Camacho AG, Luzón F, Tiampo KF, Palano M, Abajo T, Pérez E, Velasco J, Herrero T, Bru G, Molina I, López J, Rodríguez-Velasco G, Gómez I, Mallorquí JJ. Modeling the two- and three-dimensional displacement field in Lorca, Spain, subsidence and the global implications. Sci Rep 2018; 8:14782. [PMID: 30283152 PMCID: PMC6170491 DOI: 10.1038/s41598-018-33128-0] [Citation(s) in RCA: 27] [Impact Index Per Article: 4.5] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/29/2018] [Accepted: 09/24/2018] [Indexed: 11/29/2022] Open
Abstract
Land subsidence associated with overexploitation of aquifers is a hazard that commonly affects large areas worldwide. The Lorca area, located in southeast Spain, has undergone one of the highest subsidence rates in Europe as a direct consequence of long-term aquifer exploitation. Previous studies carried out on the region assumed that the ground deformation retrieved from satellite radar interferometry corresponds only to vertical displacement. Here we report, for the first time, the two- and three-dimensional displacement field over the study area using synthetic aperture radar (SAR) data from Sentinel-1A images and Global Navigation Satellite System (GNSS) observations. By modeling this displacement, we provide new insights on the spatial and temporal evolution of the subsidence processes and on the main governing mechanisms. Additionally, we also demonstrate the importance of knowing both the vertical and horizontal components of the displacement to properly characterize similar hazards. Based on these results, we propose some general guidelines for the sustainable management and monitoring of land subsidence related to anthropogenic activities.
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Affiliation(s)
- Jose Fernandez
- Instituto de Geociencias (CSIC, UCM), Calle del Doctor Severo Ochoa, no 7, Facultad de Medicina (Edificio Entrepabellones 7 y 8, 4a planta), Ciudad Universitaria, 28040, Madrid, Spain.
| | - Juan F Prieto
- ETSI Topografía, Geodesia y Cartografía, Universidad Politécnica de Madrid, Ctra. Valencia km 7, 28031, Madrid, Spain
| | - Joaquin Escayo
- Instituto de Geociencias (CSIC, UCM), Calle del Doctor Severo Ochoa, no 7, Facultad de Medicina (Edificio Entrepabellones 7 y 8, 4a planta), Ciudad Universitaria, 28040, Madrid, Spain
| | - Antonio G Camacho
- Instituto de Geociencias (CSIC, UCM), Calle del Doctor Severo Ochoa, no 7, Facultad de Medicina (Edificio Entrepabellones 7 y 8, 4a planta), Ciudad Universitaria, 28040, Madrid, Spain
| | - Francisco Luzón
- Dpto de Química y Física, Universidad de Almería, Edificio CITE-IIA, Cañada de San Urbano s/n, 04120, Almería, Spain
| | - Kristy F Tiampo
- Cooperative Institute for Research in Environmental Sciences (CIRES), 216UCB, University of Colorado at Boulder, Boulder, CO, 80309, USA
| | - Mimmo Palano
- Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Etneo, 95125, Catania, Italy
| | - Tamara Abajo
- Instituto de Geociencias (CSIC, UCM), Calle del Doctor Severo Ochoa, no 7, Facultad de Medicina (Edificio Entrepabellones 7 y 8, 4a planta), Ciudad Universitaria, 28040, Madrid, Spain
| | - Enrique Pérez
- Dpto. Ingeniería Agroforestal, ETSI Agronómica, Alimentaria y de Biosistemas, Universidad Politécnica de Madrid, Avda. Puerta de Hierro, no 2 - 4, 28040, Madrid, Spain
| | - Jesus Velasco
- ETSI Topografía, Geodesia y Cartografía, Universidad Politécnica de Madrid, Ctra. Valencia km 7, 28031, Madrid, Spain
| | - Tomas Herrero
- Dpto. Ingeniería Agroforestal, ETSI Agronómica, Alimentaria y de Biosistemas, Universidad Politécnica de Madrid, Avda. Puerta de Hierro, no 2 - 4, 28040, Madrid, Spain
| | - Guadalupe Bru
- Instituto de Geociencias (CSIC, UCM), Calle del Doctor Severo Ochoa, no 7, Facultad de Medicina (Edificio Entrepabellones 7 y 8, 4a planta), Ciudad Universitaria, 28040, Madrid, Spain
| | - Iñigo Molina
- ETSI Topografía, Geodesia y Cartografía, Universidad Politécnica de Madrid, Ctra. Valencia km 7, 28031, Madrid, Spain
| | - Juan López
- Dpto. Ingeniería Agroforestal, ETSI Agronómica, Alimentaria y de Biosistemas, Universidad Politécnica de Madrid, Avda. Puerta de Hierro, no 2 - 4, 28040, Madrid, Spain
| | - Gema Rodríguez-Velasco
- Dpto. Física de la Tierra y Astrofísica, Unidad Departamental Astronomía y Geodesia, Universidad Complutense de Madrid, Fac. C. Matemáticas, Plaza de Ciencias, 3, 28040, Madrid, Spain
| | - Israel Gómez
- Instituto de Geociencias (CSIC, UCM), Calle del Doctor Severo Ochoa, no 7, Facultad de Medicina (Edificio Entrepabellones 7 y 8, 4a planta), Ciudad Universitaria, 28040, Madrid, Spain
| | - Jordi J Mallorquí
- CommSensLab, Dep. Signal Theory and Communications, Universitat Politècnica de Catalunya (UPC), D3-Campus Nord-UPC, C. Jordi Girona 1-3, 08034, Barcelona, Spain
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Hidalgo-Zarco F, Camacho AG, Bernier-Villamor V, Nord J, Ruiz-Pérez LM, González-Pacanowska D. Kinetic properties and inhibition of the dimeric dUTPase-dUDPase from Leishmania major. Protein Sci 2001; 10:1426-33. [PMID: 11420444 PMCID: PMC2374113 DOI: 10.1110/ps.48801] [Citation(s) in RCA: 32] [Impact Index Per Article: 1.4] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 10/14/2022]
Abstract
Kinetic properties of the dimeric enzyme dUTPase from Leishmania major were studied using a continuous spectrophotometric method. dUTP was the natural substrate and dUMP and PPi the products of the hydrolysis. The trypanosomatid enzyme exhibited a low K(m) value for dUTP (2.11 microM), a k(cat) of 49 s(-1), strict Michaelis-Menten kinetics and is a potent catalyst of dUDP hydrolysis, whereas in other dUTPases described, this compound acts as a competitive inhibitor. Discrimination is achieved for the base and sugar moiety showing specificity constants for different dNTPs similar to those of bacterial, viral, and human enzymes. In the alkaline range, the K(m) for dUTP increases with the dissociation of ionizable groups showing pK(a) values of 8.8, identified as the uracil moiety of dUTP and 10, whereas in the acidic range, K(m) is regulated by an enzyme residue exhibiting a pK(a) of 7.1. Activity is strongly inhibited by the nucleoside triphosphate analog alpha-beta-imido-dUTP, indicating that the enzyme can bind triphosphate analogs. The existence of specific inhibition and the apparent structural and kinetic differences (reflected in different binding strength of dNTPs) with other eukaryotic dUTPases suggest that the present enzyme might be exploited as a target for new drugs against leishmaniasis.
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Affiliation(s)
- F Hidalgo-Zarco
- Instituto de Parasitología y Biomedicina López-Neyra, 18001-Granada, Spain
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Meinhart A, Alings C, Sträter N, Camacho AG, Alonso JC, Saenger W. Crystallization and preliminary X-ray diffraction studies of the epsilonzeta addiction system encoded by Streptococcus pyogenes plasmid pSM19035. Acta Crystallogr D Biol Crystallogr 2001; 57:745-7. [PMID: 11320325 DOI: 10.1107/s0907444901004176] [Citation(s) in RCA: 19] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/01/2001] [Accepted: 03/07/2001] [Indexed: 11/10/2022]
Abstract
The proteins encoded by the Streptococcus pyogenes broad-host range and low copy-number plasmid pSM19035 form a toxin-antitoxin module that secures stable maintenance by causing the death of plasmid-free segregants. The epsilonzeta protein complex was crystallized in four different forms at pH 5.0 and pH 7.0 using the vapour-diffusion method with PEG 3350 and ethylene glycol as precipitants. Three of the crystal forms were obtained in the same droplet under identical conditions at pH 5.0. One form belongs to the enantiomorphic space groups P4(3)2(1)2 or P4(1)2(1)2. For the other two, the X-ray reflection conditions match those of space group P2(1)2(1)2(1), one representing a superlattice of the other. A crystal form growing at pH 7.0 also belongs to space group P2(1)2(1)2(1), but there is no indication of a structural relationship to the other orthorhombic forms. Initially, the crystals diffracted to 2.9 A resolution and diffracted to 1.95 A after soaking at pH 7.0. A preparation of selenomethionyl epsilonzeta protein complex yielded single crystals suitable for X-ray diffraction experiments using synchrotron sources.
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Affiliation(s)
- A Meinhart
- Institut für Kristallographie, Freie Universität Berlin, Takustrasse 6, D-14195 Berlin, Germany
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Abstract
The terminase of bacteriophage SPP1, constituted by a large (G2P) and a small (G1P) subunit, is essential for the initiation of DNA packaging. A hexa-histidine G2P (H6-G2P), which is functional in vivo, possesses endonuclease, ATPase, and double-stranded DNA binding activities. H6-G2P introduces a cut with preference at the 5'-RCGG downward arrowCW-3' sequence. Distamycin A, which is a minor groove binder that mimics the architectural structure generated by G1P at pac, enhances the specific cut at both bona fide 5'-CTATTGCGG downward arrowC-3' sequences within pacC of SPP1 and SF6 phages. H6-G2P hydrolyzes rATP or dATP to the corresponding rADP or dADP and P(i). H6-G2P interacts with two discrete G1P domains (I and II). Full-length G1P and G1PDeltaN62 (lacking domain I) stimulate 3.5- and 1.9-fold, respectively, the ATPase activity of H6-G2P. The results presented suggest that a DNA structure, artificially promoted by distamycin A or facilitated by the assembly of G1P at pacL and/or pacR, stimulates H6-G2P cleavage at both target sites within pacC. In the presence of two G1P decamers per H6-G2P monomer, the H6-G2P endonuclease is repressed, and the ATPase activity stimulated. Based on these results, we propose a model that can account for the role of terminase in headful packaging.
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Affiliation(s)
- A Gual
- Departamento de Biotecnologia Microbiana, Centro Nacional de Biotecnologia, Consejo Superior de Investigaciones Cientificas, Campus Universidad Autónoma de Madrid, Cantoblanco, Madrid 28049, Spain
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