Red tides or chemical purges associated with tectonic children
Descripción del Articulo
Red tides, considered by the international scientific community as harmful algae blooms (FAN), are colonies of phytoplankton and microalgae capable of developing massively. There are algae that probably associate their toxicity with the invasion of host bacteria and microorganisms from the acidic an...
Autores: | , |
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Formato: | artículo |
Fecha de Publicación: | 2000 |
Institución: | Universidad Nacional Mayor de San Marcos |
Repositorio: | Revistas - Universidad Nacional Mayor de San Marcos |
Lenguaje: | español |
OAI Identifier: | oai:ojs.csi.unmsm:article/2553 |
Enlace del recurso: | https://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/2553 |
Nivel de acceso: | acceso abierto |
Materia: | Red Tides Chemical Purges phytoplankton Child Tectonic phytoplankton microalgae chemosynthetic microorganisms Mareas Rojas Purgas Químicas Fitoplancton Niño Tectónico fitoplancton microalgas microorganismos quimiosintéticos |
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Revistas - Universidad Nacional Mayor de San Marcos |
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dc.title.none.fl_str_mv |
Red tides or chemical purges associated with tectonic children Mareas rojas o purgas químicas asociadas a niños tectónicos |
title |
Red tides or chemical purges associated with tectonic children |
spellingShingle |
Red tides or chemical purges associated with tectonic children Campoblanco Díaz, Honorio Red Tides Chemical Purges phytoplankton Child Tectonic phytoplankton microalgae chemosynthetic microorganisms Mareas Rojas Purgas Químicas Fitoplancton Niño Tectónico fitoplancton microalgas microorganismos quimiosintéticos |
title_short |
Red tides or chemical purges associated with tectonic children |
title_full |
Red tides or chemical purges associated with tectonic children |
title_fullStr |
Red tides or chemical purges associated with tectonic children |
title_full_unstemmed |
Red tides or chemical purges associated with tectonic children |
title_sort |
Red tides or chemical purges associated with tectonic children |
dc.creator.none.fl_str_mv |
Campoblanco Díaz, Honorio Gomero Torres, Julia |
author |
Campoblanco Díaz, Honorio |
author_facet |
Campoblanco Díaz, Honorio Gomero Torres, Julia |
author_role |
author |
author2 |
Gomero Torres, Julia |
author2_role |
author |
dc.subject.none.fl_str_mv |
Red Tides Chemical Purges phytoplankton Child Tectonic phytoplankton microalgae chemosynthetic microorganisms Mareas Rojas Purgas Químicas Fitoplancton Niño Tectónico fitoplancton microalgas microorganismos quimiosintéticos |
topic |
Red Tides Chemical Purges phytoplankton Child Tectonic phytoplankton microalgae chemosynthetic microorganisms Mareas Rojas Purgas Químicas Fitoplancton Niño Tectónico fitoplancton microalgas microorganismos quimiosintéticos |
description |
Red tides, considered by the international scientific community as harmful algae blooms (FAN), are colonies of phytoplankton and microalgae capable of developing massively. There are algae that probably associate their toxicity with the invasion of host bacteria and microorganisms from the acidic and hot waters of the oxygen-poor ocean floor, as a product of intense underwater sulphurous volcanic activities. According to the El Niño Tectonic hypothesis, there is indirect evidence that the bacteria and chemosynthetic microorganisms that inhabit the acidic and hot waters, devoid of oxygen close to the active volcanoes of the ocean floor, synthesize the chemical compounds resulting from chemical, thermochemical reactions of fifty hundred isotopes and chemical elements released by sulphurous volcanoes; what conditions the multiplication of these toxic microorganisms, which when migrating later to the upper levels of the sea invade phytoplankton, algae and microalgae colonies, imparting various colorations as a result of the oxidation reactions of the volcanic broth saturated with bacteria, developing toxic properties to constitute the algal blooms of red tides or chemical purges. Red tides are frequently associated with two types of poisons: paralyzing venom (VPM), produced by dinoflagellate alexandrum catenella, and diarrheal shellfish venom (VDM), generated by dinophysis acuta. There are bacteria that normally live in symbiosis with mollusks, crustaceans, mussels in the gills of clams, in some special organs of tubular worms from the deep ocean and the by-product of their metabolism is filtered to the host animal as food that, in turn, imparts toxic properties. Red tides, considered by the international scientific community as harmful algae blooms (FAN), are colonies of phytoplankton and microalgae capable of developing massively. There are algae that probably associate their toxicity with the invasion of host bacteria and microorganisms from the acidic and hot waters of the oxygen-poor ocean floor, as a product of intense underwater sulphurous volcanic activities. According to the El Niño Tectonic hypothesis, there is indirect evidence that the bacteria and chemosynthetic microorganisms that inhabit the acidic and hot waters, devoid of oxygen close to the active volcanoes of the ocean floor, synthesize the chemical compounds resulting from chemical, thermochemical reactions of fifty hundred isotopes and chemical elements released by sulphurous volcanoes; what conditions the multiplication of these toxic microorganisms, which when migrating later to the upper levels of the sea invade phytoplankton, algae and microalgae colonies, imparting various colorations as a result of the oxidation reactions of the volcanic broth saturated with bacteria, developing toxic properties to constitute the algal blooms of red tides, or chemical purges. Frequently, red tides are associated with two types of poisons: paralyzing venom (VPM), produced by dinoflagellate alexandrum catenella, and diarrheal shellfish venom (VDM), generated by dinophysis acuta. There are bacteria that normally live in symbiosis with mollusks, crustaceans, mussels in the gills of clams, in some special organs of tubular worms from the deep ocean and the by-product of their metabolism is filtered to the host animal as food that, in turn, imparts toxic properties. |
publishDate |
2000 |
dc.date.none.fl_str_mv |
2000-12-15 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
format |
article |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
https://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/2553 10.15381/iigeo.v3i6.2553 |
url |
https://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/2553 |
identifier_str_mv |
10.15381/iigeo.v3i6.2553 |
dc.language.none.fl_str_mv |
spa |
language |
spa |
dc.relation.none.fl_str_mv |
https://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/2553/2241 |
dc.rights.none.fl_str_mv |
Derechos de autor 2000 Honorio Campoblanco Díaz, Julia Gomero Torres https://creativecommons.org/licenses/by-nc-sa/4.0 info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Derechos de autor 2000 Honorio Campoblanco Díaz, Julia Gomero Torres https://creativecommons.org/licenses/by-nc-sa/4.0 |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
Universidad Nacional Mayor de San Marcos, Facultad de Ingeniería Geológica, Minera, Metalúrgica y Geográfica |
publisher.none.fl_str_mv |
Universidad Nacional Mayor de San Marcos, Facultad de Ingeniería Geológica, Minera, Metalúrgica y Geográfica |
dc.source.none.fl_str_mv |
Revista del Instituto de investigación de la Facultad de minas, metalurgia y ciencias geográficas; Vol. 3 No. 6 (2000); 51-54 Revista del Instituto de investigación de la Facultad de minas, metalurgia y ciencias geográficas; Vol. 3 Núm. 6 (2000); 51-54 1682-3087 1561-0888 reponame:Revistas - Universidad Nacional Mayor de San Marcos instname:Universidad Nacional Mayor de San Marcos instacron:UNMSM |
instname_str |
Universidad Nacional Mayor de San Marcos |
instacron_str |
UNMSM |
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UNMSM |
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Revistas - Universidad Nacional Mayor de San Marcos |
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Revistas - Universidad Nacional Mayor de San Marcos |
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1795238285611630592 |
spelling |
Red tides or chemical purges associated with tectonic childrenMareas rojas o purgas químicas asociadas a niños tectónicosCampoblanco Díaz, HonorioGomero Torres, JuliaRed TidesChemical Purgesphytoplankton Child Tectonicphytoplanktonmicroalgaechemosynthetic microorganismsMareas RojasPurgas QuímicasFitoplancton Niño Tectónicofitoplanctonmicroalgasmicroorganismos quimiosintéticosRed tides, considered by the international scientific community as harmful algae blooms (FAN), are colonies of phytoplankton and microalgae capable of developing massively. There are algae that probably associate their toxicity with the invasion of host bacteria and microorganisms from the acidic and hot waters of the oxygen-poor ocean floor, as a product of intense underwater sulphurous volcanic activities. According to the El Niño Tectonic hypothesis, there is indirect evidence that the bacteria and chemosynthetic microorganisms that inhabit the acidic and hot waters, devoid of oxygen close to the active volcanoes of the ocean floor, synthesize the chemical compounds resulting from chemical, thermochemical reactions of fifty hundred isotopes and chemical elements released by sulphurous volcanoes; what conditions the multiplication of these toxic microorganisms, which when migrating later to the upper levels of the sea invade phytoplankton, algae and microalgae colonies, imparting various colorations as a result of the oxidation reactions of the volcanic broth saturated with bacteria, developing toxic properties to constitute the algal blooms of red tides or chemical purges. Red tides are frequently associated with two types of poisons: paralyzing venom (VPM), produced by dinoflagellate alexandrum catenella, and diarrheal shellfish venom (VDM), generated by dinophysis acuta. There are bacteria that normally live in symbiosis with mollusks, crustaceans, mussels in the gills of clams, in some special organs of tubular worms from the deep ocean and the by-product of their metabolism is filtered to the host animal as food that, in turn, imparts toxic properties. Red tides, considered by the international scientific community as harmful algae blooms (FAN), are colonies of phytoplankton and microalgae capable of developing massively. There are algae that probably associate their toxicity with the invasion of host bacteria and microorganisms from the acidic and hot waters of the oxygen-poor ocean floor, as a product of intense underwater sulphurous volcanic activities. According to the El Niño Tectonic hypothesis, there is indirect evidence that the bacteria and chemosynthetic microorganisms that inhabit the acidic and hot waters, devoid of oxygen close to the active volcanoes of the ocean floor, synthesize the chemical compounds resulting from chemical, thermochemical reactions of fifty hundred isotopes and chemical elements released by sulphurous volcanoes; what conditions the multiplication of these toxic microorganisms, which when migrating later to the upper levels of the sea invade phytoplankton, algae and microalgae colonies, imparting various colorations as a result of the oxidation reactions of the volcanic broth saturated with bacteria, developing toxic properties to constitute the algal blooms of red tides, or chemical purges. Frequently, red tides are associated with two types of poisons: paralyzing venom (VPM), produced by dinoflagellate alexandrum catenella, and diarrheal shellfish venom (VDM), generated by dinophysis acuta. There are bacteria that normally live in symbiosis with mollusks, crustaceans, mussels in the gills of clams, in some special organs of tubular worms from the deep ocean and the by-product of their metabolism is filtered to the host animal as food that, in turn, imparts toxic properties.Las mareas rojas considerados por la comunidad científica internacional como floraciones de algas nocivas (FAN), son colonias de fitoplancton y microalgas capaces de desarrollarse masivamente. Existen algas que probablemente asocian su toxicidad a la invasión de bacterias y microorganismos huéspedes procedentes de las aguas aciduladas y calientes de los fondos oceánicos carentes de oxígeno, como producto de intensas actividades volcánicas sulfurosas submarinas. De acuerdo a la hipótesis de El Niño Tectónico, existen evidencias indirectas que las bacterias y microorganismos quimiosintéticos que habitan las ácidas y calientes aguas, carentes de oxígeno cercano a los volcanes activos del fondo oceánico, sintetizan los compuestos químicos producto de las reacciones químicas, termoquímicas de medio centenar de isótopos y elementos químicos lanzados por los volcanes sulfurosos; lo que condiciona la multiplicación de estos microorganismos tóxicos, que al migrar posteriormente a los niveles superiores del mar, invaden colonias de fitoplancton, algas y microalgas impartiéndoles variadas coloraciones producto de las reacciones de oxidación del caldo volcánico saturado de bacterias desarrollando propiedades tóxicas para constituir las floraciones algales de mareas rojas o purgas químicas. Frecuentemente las mareas rojas están asociados a dos tipos de venenos: el veneno paralizante (VPM), producido por un dinoflagelado alexandrum catenella, y el veneno diarreico de los mariscos (VDM), generado por el dinophysis acuta. Existen bacterias que de manera normal viven en simbiosis con moluscos, crustáceos, mejillones en las branquias de almejas, en algunos órganos especiales de gusanos tubulares del océano profundo y el subproducto de su metabolismo se filtra al animal huésped como alimento que a su vez, le imparte propiedades tóxicas. Las mareas rojas considerados por la comunidad científica internacional como floraciones de algas nocivas (FAN), son colonias de fitoplancton y microalgas capaces de desarrollarse masivamente. Existen algas que probablemente asocian su toxicidad a la invasión de bacterias y microorganismos huéspedes procedentes de las aguas aciduladas y calientes de los fondos oceánicos carentes de oxígeno, como producto de intensas actividades volcánicas sulfurosas submarinas. De acuerdo a la hipótesis de El Niño Tectónico, existen evidencias indirectas que las bacterias y microorganismos quimiosintéticos que habitan las ácidas y calientes aguas, carentes de oxígeno cercano a los volcanes activos del fondo oceánico, sintetizan los compuestos químicos producto de las reacciones químicas, termoquímicas de medio centenar de isótopos y elementos químicos lanzados por los volcanes sulfurosos; lo que condiciona la multiplicación de estos microorganismos tóxicos, que al migrar posteriormente a los niveles superiores del mar, invaden colonias de fitoplancton, algas y microalgas impartiéndoles variadas coloraciones producto de las reacciones de oxidación del caldo volcánico saturado de bacterias desarrollando propiedades tóxicas para constituir las floraciones algales de mareas rojas, o purgas químicas. Frecuentemente, las mareas rojas están asociados a dos tipos de venenos: el veneno paralizante (VPM), producido por un dinoflagelado alexandrum catenella, y el veneno diarreico de los mariscos (VDM), generado por el dinophysis acuta. Existen bacterias que de manera normal viven en simbiosis con moluscos, crustáceos, mejillones en las branquias de almejas, en algunos órganos especiales de gusanos tubulares del océano profundo y el subproducto de su metabolismo se filtra al animal huésped como alimento que a su vez, le imparte propiedades tóxicas.Universidad Nacional Mayor de San Marcos, Facultad de Ingeniería Geológica, Minera, Metalúrgica y Geográfica2000-12-15info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/255310.15381/iigeo.v3i6.2553Revista del Instituto de investigación de la Facultad de minas, metalurgia y ciencias geográficas; Vol. 3 No. 6 (2000); 51-54Revista del Instituto de investigación de la Facultad de minas, metalurgia y ciencias geográficas; Vol. 3 Núm. 6 (2000); 51-541682-30871561-0888reponame:Revistas - Universidad Nacional Mayor de San Marcosinstname:Universidad Nacional Mayor de San Marcosinstacron:UNMSMspahttps://revistasinvestigacion.unmsm.edu.pe/index.php/iigeo/article/view/2553/2241Derechos de autor 2000 Honorio Campoblanco Díaz, Julia Gomero Torreshttps://creativecommons.org/licenses/by-nc-sa/4.0info:eu-repo/semantics/openAccessoai:ojs.csi.unmsm:article/25532020-07-06T21:52:40Z |
score |
13.772458 |
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La información contenida en este registro es de entera responsabilidad de la institución que gestiona el repositorio institucional donde esta contenido este documento o set de datos. El CONCYTEC no se hace responsable por los contenidos (publicaciones y/o datos) accesibles a través del Repositorio Nacional Digital de Ciencia, Tecnología e Innovación de Acceso Abierto (ALICIA).