La cerveza, ideal para reponer energías

La cerveza, ideal para reponer energías

Un estudio científico revela que la cerveza puede suponer una «eficaz» bebida rehidratante tras la práctica deportiva, gracias a su «alta presencia de elementos antioxidantes» que ayudan a reducir los efectos producidos por el ejercicio físico.

Así lo aseguró el profesor de Fisiología del Ejercicio de la Universidad de Barcelona (UB) Joan Ramón Barbany durante la presentación del estudio Idoneidad de la cerveza en la dieta equilibrada de los deportistas, en el marco de los Juegos Mundiales de Medicina y Salud (Medigames), que se celebran en Alicante.

«La cerveza tiene una alta presencia de elementos antioxidantes, derivados de su origen vegetal, que combaten la aparición de radicales libres», según Barbany, para quien esto contribuye a reducir los efectos producidos por el ejercicio físico, como son «los dolores musculares, la fatiga y el fenómeno conocido como sobreentrenamiento».

Además, esta bebida contiene componentes vitamínicos, minerales y carbohidratos, por lo que «su ingesta en dosis moderadas» por personas adultas puede desempeñar un papel en «la recuperación del metabolismo hormonal e inmunológico de los deportistas tras el ejercicio físico», según la investigación.

Por su parte, el profesor de Fisiología Médica de la Universidad de Granada Manuel Castillo-Garzón indicó que, «comparada con el agua», la ingesta de cerveza como rehidratante «no tiene ningún aspecto que la haga desaconsejable».

El estudio, realizado por científicos de la Universidad de Granada y del Consejo Superior de Investigaciones Científicas (CSIC), contó con la participación de dieciséis personas que se sometieron en dos ocasiones, separadas por un intervalo de tres semanas, a un ejercicio «extenuado» de sesenta minutos en condiciones de «elevada temperatura ambiental».

«Los participantes perdieron de dos a tres kilogramos de peso corporal», sobre todo de agua, detalló Castillo-Garzón, quien reseñó que, en una ocasión, se les dio sólo agua para rehidratarse y en la otra, «dos tercios de cerveza, junto con toda el agua que quisieran».

Por su parte, el médico especialista en Fisiología del Deporte y ex jugador profesional de básquet, Juan Antonio Corbalán, afirmó que, «a pesar del alcohol» y con «un uso inteligente», la cerveza es una «magnífica bebida compatible con el rendimiento deportivo de cualquier disciplina».

Corbalán señaló que hay multitud de leyendas alrededor de esta bebida que «no se basan en criterios científicos», como la falsa capacidad de engorde de la cerveza, cuyo contenido calórico es de unas 145 calorías, poco más del contenido en un yogur entero azucarado (125).

«Lo que engorda es el mal uso que podemos hacer de la cerveza», precisó Corbalán, para quien factores como el sexo, la capacidad para metabolizar el alcohol o un mal hábito en las personas influyen más en el aumento del peso corporal.

En este sentido, durante la rueda de prensa se avanzó un estudio sobre la «barriga cervecera» que se ultima en estos momentos y cuya primera conclusión es que las personas que beben cerveza de manera habitual no desarrollan más «tripa» que las que no lo hacen.

«El estrés crónico» y una mala alimentación, basada en una alta densidad calórica, son los causantes de este fenómeno, hecho contrario a lo que se creía en la actualidad.
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Las algas del Mediterráneo tuvieron en el pasado elementos tropicales

Las algas del Mediterráneo tuvieron en el pasado elementos tropicales

Las algas del Mediterráneo tuvieron una pasado tropical. Tomaron su forma actual cuando se produjo la separación de ese mar y el océano Índico hace 15 millones de años, al tiempo que se enfriaba la Tierra, según un estudio recogido por el Servicio de Información y Noticias Científicas (SINC).

La investigación, desarrollada por científicos de la Universidad de Granada (UGR) y de la Universidad de Modena y Reggio Emilia (Italia), analiza los patrones de distribución de las algas coralinas en el oeste y centro del Mediterráneo (en Salento, Italia, y Almería) a través del registro fósil de 21 especies recogidas en las dos áreas. De este modo, describe e interpreta la desaparición de los últimos arrecifes de coral del Messiniense (hace entre 7,24 y 5,3 millones de años).

«Las algas coralinas son algas calcáreas muy comunes en la actualidad, aunque desconocidas para el gran público, incluidos los naturalistas, y muy frecuentes como fósiles, especialmente en rocas relativamente modernas», explicó Juan C. Braga, autor principal e investigador del departamento de Estratigrafía y Paleontología de la UGR. «En épocas posteriores, más recientes, este mar ya no ha tenido las condiciones oceanográficas (sobre todo la temperatura suficiente) como para albergar arrecifes de coral», indicó el investigador.
Pérdida de biodiversidad

Los últimos arrecifes del Mediterráneo ya presentaban poca diversidad de corales durante el periodo estudiado. «Es el resultado de la larga historia de enfriamiento sufrida por toda la Tierra en los últimos 20 millones de años y el aislamiento (desconexión) del Mediterráneo al Índico, hace unos 15 millones de años», comentó Braga.

«Como los corales, la flora de algas refleja el enfriamiento del Mediterráneo y su separación del Índico, y sólo unos pocos elementos tropicales sobreviven en la época del Messiniense. Además, la mayoría ya tienen afinidades atlánticas y son similares a las algas que viven en nuestras costas en la actualidad», aseguró Braga.

Las características «mediterráneo-atlánticas» de la flora de los arrecifes de coral del Messiniense reflejan así la disminución en sus componentes tropicales que se generó durante el Mioceno (hace cerca de 20 millones de años). El declive generalizado de este tipo de algas se debe al enfriamiento global y al aislamiento del Mediterráneo en el Mioceno medio, según el equipo investigador.
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La cerveza es el mejor rehidradante después del ejercicio

La cerveza es el mejor rehidradante después del ejercicio

Un estudio científico revela que la cerveza puede suponer una «eficaz» bebida rehidratante tras la práctica deportiva, gracias a su «alta presencia de elementos antioxidantes» que ayudan a reducir los efectos producidos por el ejercicio físico, como las agujetas y la fatiga.

Así lo ha asegurado hoy el profesor de Fisiología del Ejercicio de la Universidad de Barcelona (UB) Joan Ramón Barbany durante la presentación del estudio «Idoneidad de la cerveza en la dieta equilibrada de los deportistas» en el marco de los Juegos Mundiales de Medicina y Salud (Medigames), que se celebran en Alicante.

«La cerveza tiene una alta presencia de elementos antioxidantes, derivados de su origen vegetal, que combaten la aparición de radicales libres», según Barbany, para quien esto contribuye a reducir los efectos producidos por el ejercicio físico, como son «los dolores musculares, la fatiga y el fenómeno conocido como sobreentrenamiento».

Además, esta bebida contiene componentes vitamínicos, minerales y carbohidratos, por lo que «su ingesta en dosis moderadas» por personas adultas puede desempeñar un papel en «la recuperación del metabolismo hormonal e inmunológico de los deportistas tras el ejercicio físico», según la investigación.

Por su parte, el profesor de Fisiología Médica de la Universidad de Granada Manuel Castillo-Garzón ha indicado que, «comparada con el agua», la ingesta de cerveza como rehidratante «no tiene ningún aspecto que la haga desaconsejable».

El estudio, realizado por científicos de la Universidad de Granada y del Consejo Superior de Investigaciones Científicas (CSIC), ha contado con la participación de dieciséis personas que se han sometido en dos ocasiones, separadas por un intervalo de tres semanas, a un ejercicio «extenuado» de sesenta minutos en condiciones de «elevada temperatura ambiental».

«Los participantes perdieron de dos a tres kilogramos de peso corporal», sobre todo de agua, ha detallado Castillo-Garzón, quien ha reseñado que, en una ocasión, se les dio sólo agua para rehidratarse y en la otra, «dos tercios de cerveza, junto con toda el agua que quisieran».

Por su parte, el médico especialista en Fisiología del Deporte y ex jugador profesional de baloncesto, Juan Antonio Corbalán, ha afirmado que, «a pesar del alcohol» y con «un uso inteligente», la cerveza es una «magnífica bebida compatible con el rendimiento deportivo de cualquier disciplina».

Corbalán ha señalado que hay multitud de leyendas alrededor de esta bebida que «no se basan en criterios científicos», como la falsa capacidad de engorde de la cerveza, cuyo contenido calórico es de unas 145 calorías, poco más de su contenido en un yogur entero azucarado (125).

«Lo que engorda es el mal uso que podemos hacer de la cerveza», ha precisado Corbalán, para quien factores como el sexo, la capacidad para metabolizar el alcohol o un mal hábito en las personas influyen más en el aumento del peso corporal.

En este sentido, durante la rueda de prensa se ha avanzado un estudio sobre la «barriga cervecera» que se ultima en estos momentos y cuya primera conclusión es que las personas que beben cerveza de manera habitual no desarrollan más «tripa» que las que no lo hacen.

«El estrés crónico» y una mala alimentación, basada en una alta densidad calórica, son los causantes de este fenómeno, hecho contrario a lo que se creía en la actualidad.
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Cerveza, eficaz para rehidratar a deportistas

Cerveza, eficaz para rehidratar a deportistas

Alicante, España Martes 07 de julio de 2009.- Un estudio científico revela que la cerveza puede ser una “eficaz” bebida rehidratante tras la práctica deportiva, gracias a su “alta presencia de elementos antioxidantes” que ayudan a reducir los efectos producidos por el ejercicio físico, como la fatiga.

Así lo aseguró el profesor de Fisiología del Ejercicio de la Universidad de Barcelona (UB) Joan Ramón Barbany durante la presentación del estudio “Idoneidad de la cerveza en la dieta equilibrada de los deportistas”, en el marco de los Juegos Mundiales de Medicina y Salud, que se celebran en Alicante.

“La cerveza tiene alta presencia de elementos antioxidantes, derivados de su origen vegetal, que combaten la aparición de radicales libres”, según Barbany, quien cree que esto contribuye a reducir los efectos producidos por el ejercicio físico, como son “los dolores musculares, la fatiga y el fenómeno conocido como sobre entrenamiento”.

Además, esta bebida contiene componentes vitamínicos, minerales y carbohidratos, por lo que “su ingesta en dosis moderadas” por personas adultas puede desempeñar un papel en “la recuperación del metabolismo hormonal e inmunológico de los deportistas tras el ejercicio físico”, según la investigación.

Por su parte, el profesor de Fisiología Médica de la Universidad de Granada, Manuel Castillo-Garzón indicó que, “comparada con el agua”, la ingesta de cerveza como rehidratante es aconsejable.

El estudio, realizado por científicos de la Universidad de Granada y del Consejo Superior de Investigaciones Científicas (CSIC) , contó con la participación de dieciséis personas sometidas en dos ocasiones, separadas por un intervalo de tres semanas, a un ejercicio “extenuado” de sesenta minutos en condiciones de “elevada temperatura ambiental”.

“Los participantes perdieron de dos a tres kilogramos de peso corporal” , sobre todo de agua, detalló Castillo-Garzón, quien ha reseñado que, en una ocasión, se les dio sólo agua para rehidratarse y en la otra, “dos tercios de cerveza, junto con toda el agua que quisieran”.

Por su parte, el médico especialista en Fisiología del Deporte y ex jugador profesional de baloncesto Juan Antonio Corbalán afirmó que, “a pesar del alcohol” y con “un uso inteligente”, la cerveza es una “magnífica bebida compatible con el rendimiento deportivo de cualquier disciplina”.

Los especialistas desmienten un de los grandes mitos del consumo de cerveza, pues no ocasiona un aumento de peso.

Lo que sí influye es: “El estrés crónico” y una mala alimentación, basada en una alta densidad calórica, causantes de la “barriga cervecera”.
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Researchers patent a process of ornamental stone consolidation to make it more resistant

Researchers patent a process of ornamental stone consolidation to make it more resistant

The University if Granada has patented a product and an implementation method to obtain the activation of the microorganisms that produce the carbonates found in construction and ornamental materials. Thanks to this, the formation of a calcium carbonate cement is induced, which can be used to protect and consolidate in situ surfaces made of construction and ornamentation lime materials in general, as well as natural stone too.

The people responsible of this patent are the members of a research group of the Microbiology Department and the Mineralogy and Petrology Department of the Faculty of Sciences of the University of Granada.

French company Bordeaux Architectural Antique, located in Bordeaux, works in the antique architecture and sculpture restoration sector and is interested in this patent. As a result of this, an ‘agreement of material and know-how transfer’ has been signed between this company and the University of Granada. These researchers have provided them with the product, as well as assessment to carry out trials to check the efficiency of the product and the method in their own samples.

In fact, company Bordeaux Architectural Antique has already asked for an authorization to apply this product in historical buildings. So far they have obtained the suitable permission from Le directeur régional des affaires culturelles (regional manager of cultural matters) to carry out trials in the Cathedral of San Andres in Burdeos, although so far the date of the work commencement is unknown.

In addition to obtaining the patent for the consolidation of ornamental stone, this Granada-based research group has started a study that aims to lower the implementation price of this patented mean of cultivation. They intend to analyse other useful products which produce the same results but at a lower cost. Moreover, they want to study how much the time of treatment can be reduced but getting these same results, as this would reduce the costs related to the implementation of the cultivation mean. They have been recently awarded with a Project of Excellence by the Innovation, Science and Enterprise Ministry of the Andalusian government Junta de Andalucía in order to continue with their current research.
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Weight determines the future cognitive development of children born very premature

Weight determines the future cognitive development of children born very premature

Researchers of the Department of Neuroscience and Health Sciences of the University of Almería and Hospital Torrecárdenas are carrying out an assessment of the physical neuropsychological characteristics of children born before 32 weeks’ gestation or whose weight is lower than 1500 grams –very premature-. The main aim of this project, coordinated by Mª Dolores Roldán Tapia, from the UAL, is to accurately define the origin of brain damage, so as to stimulate the affected area early thus causing the adequate cognitive and motric development of the individual.

The commonest differences between premature babies and those born after a nine-month pregnancy are mainly related to visoperceptive skills, memory and movement which eventually translate into learning and spatial orientation difficulties. That is why these difficulties that these children have in their cognitive performance and the development of perceptual and executive functions are being studied.

A population sample of 35 very premature children is being taken for this project, together with the same number of healthy children, all of them born between 2000 and 2001, with their parents’ authorisation. Special attention has been paid to the fact that both the children and their parents have similar educational and social levels, as the stimulation they get in the early stages of their lives has a decisive influence in their later development.

The results obtained so far reveal that the decisive variable for the existence of a reversible or irreversible brain damage is the baby’s weight at birth, rather than the time of gestation. According to experts, an early stimulation of the individual’s central nerve system, from birth until his complete cognitive development at 16 years of age, in foetuses whose weight at birth is over 1,500 gr. or who are very premature, will eventually get ideal cognitive levels. However, this stimulation must be continued throughout the whole development of babies whose weight is lower than 1,500 gr. so that they can get a proper brain maturity.

As a complement to this project, Alemeria-based researchers are developing an epidemiological study so as to set the percentage of very premature children who have brain damage against the total number of children born under the same characteristics between 2000 and 2001. This study is funded by Fundación para la Investigación Biosanitaria de Andalucía Oriental-Alejandro Otero (FIBAO, Alejandro Otero foundation for bio-health research in eastern Andalusia). Moreover, in collaboration with the University of Granada, experts are developing another line of research whose aim is to determine the existing relationship between visoperceptive skill deficit and the level of reasoning in very premature children.

In the near future, the team of researchers of the University of Almeria will be expanding their research and including new variables that may make a determining brain difference in very premature babies, like for example, the brain difference between babies born in natural multiple births and those with artificial techniques, or the interaction between pre-maturity and bad nutrition.
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Coralline algae in the Mediterranean lost their tropical element between 5 and 7 million years ago

Coralline algae in the Mediterranean lost their tropical element between 5 and 7 million years ago

An international team of researchers has studied the coralline algae fossils that lived on the last coral reefs of the Mediterranean Sea between 7.24 and 5.3 million years ago. Mediterranean algae and coral reefs began to resemble present day reefs following the isolation of the Mediterranean from the Indian Ocean and global cooling 15 and 20 million years ago respectively.

The research team from the University of Granada (UGR) and the University of Modena and Reggio Emilia (Italia) show coralline algae distribution patterns in the west and centre of the Mediterranean Sea (in Salento, Italy and Almería, Spain) by way of a fossil register of 21 species collected in the two areas.

«Coralline algae are calcareous algae that are very common nowadays, although unknown to the general public, including naturalists, and quite often in fossil form, particularly in relatively modern rocks», Juan C. Braga, the chief author and a researcher at the Stratigraphy and Paleontology Department of the UGR explained to SINC.

The study, which was published recently in Palaeogeography Palaeoclimatology Palaeoecology, describes and interprets the disappearance of the last Messinian coral reefs (between 7.24 and 5.3 million years ago) in the Mediterranean Sea. «In subsequent, more recent eras, this sea has not had the right oceanographic conditions (above all a high enough temperature) to house coral reefs,» Braga added.

When Tropical Coral Reefs Became Atlantic

During the period studied by the scientists through the coralline algae fossils found in the Mediterranean, the last few reefs boasted very little coralline diversity. «This is the result of the long history of global cooling over the last 20 million years and the isolation (separation) of the Mediterranean from the Indian Ocean, some 15 million years ago,» the research says.

According to the results of the research, the relative abundance of coralline algae in reefs and slope deposits is 1-5% and 18% lower respectively in the Sorbas basin (Almería) than in Salento (Italy). Furthermore, the main components of the coralline algae assemblages found in shallow water are extant species that are very common in the Mediterranean.

Other species, such as Spongites fruticulosus and Phymatolithon calcareum, have lived in the western Mediterranean for more than 25 million years. However, the typical components of present-day coral reefs, such as Hydrolithon species with thick thalli, which were no longer present in the western region of the Mediterranean 7 million years ago.

«Just like reef corallines, algae flora reflects the cooling of the Mediterranean and its isolation from the Indian Ocean, and only a few tropical biotas existed in the Messinian era. Moreover, most of them already had Atlantic affinities and resembled the algae that still inhabits our coasts today», Braga states.

The Mediterranean-Atlantic characteristics of Messinian reef corallines therefore reflect the decrease in tropical biotas that occurred during the Miocene (around 20 million years ago). According to the research team, the widespread decline of this type of algae was due to global cooling and the isolation of the Mediterranean during the middle Miocene.
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Coralline algae in the Mediterranean lost their tropical element between 5 and 7 million years ago

Coralline algae in the Mediterranean lost their tropical element between 5 and 7 million years ago

«Coralline algae are calcareous algae that are very common nowadays, although unknown to the general public, including naturalists, and quite often in fossil form, particularly in relatively modern rocks», Juan C. Braga, the chief author and a researcher at the Stratigraphy and Paleontology Department of the UGR explained to SINC.

The study, which was published recently in Palaeogeography Palaeoclimatology Palaeoecology, describes and interprets the disappearance of the last Messinian coral reefs (between 7.24 and 5.3 million years ago) in the Mediterranean Sea. «In subsequent, more recent eras, this sea has not had the right oceanographic conditions (above all a high enough temperature) to house coral reefs,» Braga added.

When Tropical Coral Reefs Became Atlantic

During the period studied by the scientists through the coralline algae fossils found in the Mediterranean, the last few reefs boasted very little coralline diversity. «This is the result of the long history of global cooling over the last 20 million years and the isolation (separation) of the Mediterranean from the Indian Ocean, some 15 million years ago,» the research says.

According to the results of the research, the relative abundance of coralline algae in reefs and slope deposits is 1-5% and 18% lower respectively in the Sorbas basin (Almería) than in Salento (Italy). Furthermore, the main components of the coralline algae assemblages found in shallow water are extant species that are very common in the Mediterranean.

Other species, such as Spongites fruticulosus and Phymatolithon calcareum, have lived in the western Mediterranean for more than 25 million years. However, the typical components of present-day coral reefs, such as Hydrolithon species with thick thalli, which were no longer present in the western region of the Mediterranean 7 million years ago.

«Just like reef corallines, algae flora reflects the cooling of the Mediterranean and its isolation from the Indian Ocean, and only a few tropical biotas existed in the Messinian era. Moreover, most of them already had Atlantic affinities and resembled the algae that still inhabits our coasts today», Braga states.

The Mediterranean-Atlantic characteristics of Messinian reef corallines therefore reflect the decrease in tropical biotas that occurred during the Miocene (around 20 million years ago). According to the research team, the widespread decline of this type of algae was due to global cooling and the isolation of the Mediterranean during the middle Miocene.
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Coralline Algae In The Mediterranean Lost Their Tropical Element Between 5 And 7 Million Years Ago

Coralline Algae In The Mediterranean Lost Their Tropical Element Between 5 And 7 Million Years Ago

An international team of researchers has studied the coralline algae fossils that lived on the last coral reefs of the Mediterranean Sea between 7.24 and 5.3 million years ago. Mediterranean algae and coral reefs began to resemble present day reefs following the isolation of the Mediterranean from the Indian Ocean and global cooling 15 and 20 million years ago respectively.

The research team from the University of Granada (UGR) and the University of Modena and Reggio Emilia (Italia) show coralline algae distribution patterns in the west and centre of the Mediterranean Sea (in Salento, Italy and Almería, Spain) by way of a fossil register of 21 species collected in the two areas.

«Coralline algae are calcareous algae that are very common nowadays, although unknown to the general public, including naturalists, and quite often in fossil form, particularly in relatively modern rocks», Juan C. Braga, the chief author and a researcher at the Stratigraphy and Paleontology Department of the UGR explained to SINC.

The study, which was published recently in Palaeogeography Palaeoclimatology Palaeoecology, describes and interprets the disappearance of the last Messinian coral reefs (between 7.24 and 5.3 million years ago) in the Mediterranean Sea. «In subsequent, more recent eras, this sea has not had the right oceanographic conditions (above all a high enough temperature) to house coral reefs,» Braga added.

When Tropical Coral Reefs Became Atlantic

During the period studied by the scientists through the coralline algae fossils found in the Mediterranean, the last few reefs boasted very little coralline diversity. «This is the result of the long history of global cooling over the last 20 million years and the isolation (separation) of the Mediterranean from the Indian Ocean, some 15 million years ago,» the research says.

According to the results of the research, the relative abundance of coralline algae in reefs and slope deposits is 1-5% and 18% lower respectively in the Sorbas basin (Almería) than in Salento (Italy). Furthermore, the main components of the coralline algae assemblages found in shallow water are extant species that are very common in the Mediterranean.

Other species, such as Spongites fruticulosus and Phymatolithon calcareum, have lived in the western Mediterranean for more than 25 million years. However, the typical components of present-day coral reefs, such as Hydrolithon species with thick thalli, which were no longer present in the western region of the Mediterranean 7 million years ago.

«Just like reef corallines, algae flora reflects the cooling of the Mediterranean and its isolation from the Indian Ocean, and only a few tropical biotas existed in the Messinian era. Moreover, most of them already had Atlantic affinities and resembled the algae that still inhabits our coasts today», Braga states.

The Mediterranean-Atlantic characteristics of Messinian reef corallines therefore reflect the decrease in tropical biotas that occurred during the Miocene (around 20 million years ago). According to the research team, the widespread decline of this type of algae was due to global cooling and the isolation of the Mediterranean during the middle Miocene.
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Coralline algae in the Mediterranean lost their tropical element between 5 and 7 million years ago

Coralline algae in the Mediterranean lost their tropical element between 5 and 7 million years ago

An international team of researchers has studied the coralline algae fossils that lived on the last coral reefs of the Mediterranean Sea between 7.24 and 5.3 million years ago. Mediterranean algae and coral reefs began to resemble present day reefs following the isolation of the Mediterranean from the Indian Ocean and global cooling 15 and 20 million years ago respectively.

«Coralline algae are calcareous algae that are very common nowadays, although unknown to the general public, including naturalists, and quite often in fossil form, particularly in relatively modern rocks», Juan C. Braga, the chief author and a researcher at the Stratigraphy and Paleontology Department of the UGR explained to SINC.

The study, which was published recently in Palaeogeography Palaeoclimatology Palaeoecology, describes and interprets the disappearance of the last Messinian coral reefs (between 7.24 and 5.3 million years ago) in the Mediterranean Sea. «In subsequent, more recent eras, this sea has not had the right oceanographic conditions (above all a high enough temperature) to house coral reefs,» Braga added.

When Tropical Coral Reefs Became Atlantic

During the period studied by the scientists through the coralline algae fossils found in the Mediterranean, the last few reefs boasted very little coralline diversity. «This is the result of the long history of global cooling over the last 20 million years and the isolation (separation) of the Mediterranean from the Indian Ocean, some 15 million years ago,» the research says.

According to the results of the research, the relative abundance of coralline algae in reefs and slope deposits is 1-5% and 18% lower respectively in the Sorbas basin (Almería) than in Salento (Italy). Furthermore, the main components of the coralline algae assemblages found in shallow water are extant species that are very common in the Mediterranean.

Other species, such as Spongites fruticulosus and Phymatolithon calcareum, have lived in the western Mediterranean for more than 25 million years. However, the typical components of present-day coral reefs, such as Hydrolithon species with thick thalli, which were no longer present in the western region of the Mediterranean 7 million years ago.

«Just like reef corallines, algae flora reflects the cooling of the Mediterranean and its isolation from the Indian Ocean, and only a few tropical biotas existed in the Messinian era. Moreover, most of them already had Atlantic affinities and resembled the algae that still inhabits our coasts today», Braga states.

The Mediterranean-Atlantic characteristics of Messinian reef corallines therefore reflect the decrease in tropical biotas that occurred during the Miocene (around 20 million years ago). According to the research team, the widespread decline of this type of algae was due to global cooling and the isolation of the Mediterranean during the middle Miocene.
Descargar


Coralline Algae In The Mediterranean Lost Their Tropical Element Between 5 and 7 Million Years Ago

Coralline Algae In The Mediterranean Lost Their Tropical Element Between 5 and 7 Million Years Ago

An international team of researchers has studied the coralline algae fossils that lived on the last coral reefs of the Mediterranean Sea between 7.24 and 5.3 million years ago. Mediterranean algae and coral reefs began to resemble present day reefs following the isolation of the Mediterranean from the Indian Ocean and global cooling 15 and 20 million years ago respectively.

The research team from the University of Granada (UGR) and the University of Modena and Reggio Emilia (Italia) show coralline algae distribution patterns in the west and centre of the Mediterranean Sea (in Salento, Italy and Almería, Spain) by way of a fossil register of 21 species collected in the two areas.

«Coralline algae are calcareous algae that are very common nowadays, although unknown to the general public, including naturalists, and quite often in fossil form, particularly in relatively modern rocks», Juan C. Braga, the chief author and a researcher at the Stratigraphy and Paleontology Department of the UGR explained to SINC.

The study, which was published recently in Paleogeography Paleoclimatology Paleoecology, describes and interprets the disappearance of the last Messinian coral reefs (between 7.24 and 5.3 million years ago) in the Mediterranean Sea . «In subsequent, more recent eras, this sea has not had the right oceanographic conditions (above all a high enough temperature) to house coral reefs,» Braga added.

When Tropical Coral Reefs Became Atlantic

During the period studied by the scientists through the coralline algae fossils found in the Mediterranean, the last few reefs boasted very little coralline diversity. «This is the result of the long history of global cooling over the last 20 million years and the isolation (separation) of the Mediterranean from the Indian Ocean, some 15 million years ago,» the research says.

According to the results of the research, the relative abundance of coralline algae in reefs and slope deposits is 1-5% and 18% lower respectively in the Sorbas basin (Almería) than in Salento (Italy). Furthermore, the main components of the coralline algae assemblages found in shallow water are extant species that are very common in the Mediterranean.

Other species, such as Spongites fruticulosus and Phymatolithon calcareum, have lived in the western Mediterranean for more than 25 million years. However, the typical components of present-day coral reefs, such as Hydrolithon species with thick thalli, which were no longer present in the western region of the Mediterranean 7 million years ago.

«Just like reef corallines, algae flora reflects the cooling of the Mediterranean and its isolation from the Indian Ocean, and only a few tropical biotas existed in the Messinian era. Moreover, most of them already had Atlantic affinities and resembled the algae that still inhabits our coasts today», Braga states.

The Mediterranean-Atlantic characteristics of Messinian reef corallines therefore reflect the decrease in tropical biotas that occurred during the Miocene (around 20 million years ago). According to the research team, the widespread decline of this type of algae was due to global cooling and the isolation of the Mediterranean during the middle Miocene.
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A funny kind of subject

A funny kind of subject

Heard the one about the academics who gathered at the University of Granada for a sober “International Symposium on Humour And Laughter”? Now that’s funny. But was anything else about the conference? Whenever someone sets about a solemn analysis of humour, you wilt a little. The American writer E. B. White was convinced not only that humour cannot be explained, but also that you shouldn’t even try. “Humour can be dissected as a frog can,” White said, “but the thing dies in the process and the innards are discouraging to any but the pure scientific mind.”

Not that there has been any shortage of pure minds that have mulled the nature of humour, from Plato and Schopenhauer to Kant and Freud. Hemingway, astutely and typically, confined his thoughts on the subject to the brisk observation that: “It always seemed to me that in those who make jokes in life the seeds are covered with better soil and with a higher grade of manure.”

Why not just leave it at that? Because who can say for sure what will make someone else laugh? Each joke is like a blind date: some work for you, others don’t. It’s personal taste. You can say: “I can see that Ulysses is a great novel, but I didn’t enjoy it.” But you can’t say: “I know that’s funny, but it just didn’t make me laugh.” Yes, there are broad demarcation lines: Groucho Marx is funny; Karl Marx, not so much. Sometimes what was funny, no longer is: Brian Rix farces, say. And what wasn’t funny, now is; politicians, for instance.

A Swiss professor told the conference that Britons are among the most likely to fear that they are the butt of a joke. Given that Darwin thought laughter was man’s way of sublimating the ancient urge to kill, is this reaction really so funny?
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