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a2026-06-25
en Extreme storms during the last 6500 years from lagoonal sedimentary archives in the Mar Menor (SE Spain) -
Modificado el valor del campo
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del recurso Distribución HTML a2026-06-25
(anteriormente2026-06-23
) en Extreme storms during the last 6500 years from lagoonal sedimentary archives in the Mar Menor (SE Spain)
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| 97 | "notes": "Storms and tsunamis, which may seriously endanger human | 107 | "notes": "Storms and tsunamis, which may seriously endanger human | ||
| 98 | society, are amongst the most devastating marine catastrophes that can | 108 | society, are amongst the most devastating marine catastrophes that can | ||
| 99 | occur in coastal areas. Many such events are known and have been | 109 | occur in coastal areas. Many such events are known and have been | ||
| 100 | reported for the Mediterranean, a region where high-frequency | 110 | reported for the Mediterranean, a region where high-frequency | ||
| 101 | occurrences of these extreme events coincides with some of the most | 111 | occurrences of these extreme events coincides with some of the most | ||
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| 103 | the Mar Menor (SE Spain), we discovered eight coarse-grained layers | 113 | the Mar Menor (SE Spain), we discovered eight coarse-grained layers | ||
| 104 | which document marine incursions during periods of intense storm | 114 | which document marine incursions during periods of intense storm | ||
| 105 | activity or tsunami events. Based on radiocarbon dating, these extreme | 115 | activity or tsunami events. Based on radiocarbon dating, these extreme | ||
| 106 | events occurred around 5250, 4000, 3600, 3010, 2300, 1350, 650, and 80 | 116 | events occurred around 5250, 4000, 3600, 3010, 2300, 1350, 650, and 80 | ||
| 107 | years calaEuro-BP. No comparable events have been observed during the | 117 | years calaEuro-BP. No comparable events have been observed during the | ||
| 108 | 20th and 21st centuries. The results indicate little likelihood of a | 118 | 20th and 21st centuries. The results indicate little likelihood of a | ||
| 109 | tsunami origin for these coarse-grained layers, although historical | 119 | tsunami origin for these coarse-grained layers, although historical | ||
| 110 | tsunami events are recorded in this region. These periods of surge | 120 | tsunami events are recorded in this region. These periods of surge | ||
| 111 | events seem to coincide with the coldest periods in Europe during the | 121 | events seem to coincide with the coldest periods in Europe during the | ||
| 112 | late Holocene, suggesting a control by a climatic mechanism for | 122 | late Holocene, suggesting a control by a climatic mechanism for | ||
| 113 | periods of increased storm activity. Spectral analyses performed on | 123 | periods of increased storm activity. Spectral analyses performed on | ||
| 114 | the sand percentage revealed four major periodicities of 1228aEuro-+/- | 124 | the sand percentage revealed four major periodicities of 1228aEuro-+/- | ||
| 115 | aEuro-327, 732aEuro-+/- aEuro-80, 562aEuro-+/- aEuro-58, and | 125 | aEuro-327, 732aEuro-+/- aEuro-80, 562aEuro-+/- aEuro-58, and | ||
| 116 | 319aEuro-+/- aEuro-16 years. Amongst the well-known proxies that have | 126 | 319aEuro-+/- aEuro-16 years. Amongst the well-known proxies that have | ||
| 117 | revealed a millennial-scale climate variability during the Holocene, | 127 | revealed a millennial-scale climate variability during the Holocene, | ||
| 118 | the ice-rafted debris (IRD) indices in the North Atlantic developed by | 128 | the ice-rafted debris (IRD) indices in the North Atlantic developed by | ||
| 119 | Bond et al. (1997, 2001) present a cyclicity of 1470aEuro-+/- | 129 | Bond et al. (1997, 2001) present a cyclicity of 1470aEuro-+/- | ||
| 120 | aEuro-500 years, which matches the 1228aEuro-+/- aEuro-327-year | 130 | aEuro-500 years, which matches the 1228aEuro-+/- aEuro-327-year | ||
| 121 | periodicity evidenced in the Mar Menor, considering the respective | 131 | periodicity evidenced in the Mar Menor, considering the respective | ||
| 122 | uncertainties in the periodicities. Thus, an in-phase storm activity | 132 | uncertainties in the periodicities. Thus, an in-phase storm activity | ||
| 123 | in the western Mediterranean is found with the coldest periods in | 133 | in the western Mediterranean is found with the coldest periods in | ||
| 124 | Europe and with the North Atlantic thermohaline circulation. However, | 134 | Europe and with the North Atlantic thermohaline circulation. However, | ||
| 125 | further investigations, such as additional coring and high-resolution | 135 | further investigations, such as additional coring and high-resolution | ||
| 126 | coastal imagery, are needed to better constrain the main cause of | 136 | coastal imagery, are needed to better constrain the main cause of | ||
| 127 | these multiple events.", | 137 | these multiple events.", | ||
| 128 | "notes_translated": { | 138 | "notes_translated": { | ||
| 129 | "es": "Storms and tsunamis, which may seriously endanger human | 139 | "es": "Storms and tsunamis, which may seriously endanger human | ||
| 130 | society, are amongst the most devastating marine catastrophes that can | 140 | society, are amongst the most devastating marine catastrophes that can | ||
| 131 | occur in coastal areas. Many such events are known and have been | 141 | occur in coastal areas. Many such events are known and have been | ||
| 132 | reported for the Mediterranean, a region where high-frequency | 142 | reported for the Mediterranean, a region where high-frequency | ||
| 133 | occurrences of these extreme events coincides with some of the most | 143 | occurrences of these extreme events coincides with some of the most | ||
| 134 | densely populated coastal areas in the world. In a sediment core from | 144 | densely populated coastal areas in the world. In a sediment core from | ||
| 135 | the Mar Menor (SE Spain), we discovered eight coarse-grained layers | 145 | the Mar Menor (SE Spain), we discovered eight coarse-grained layers | ||
| 136 | which document marine incursions during periods of intense storm | 146 | which document marine incursions during periods of intense storm | ||
| 137 | activity or tsunami events. Based on radiocarbon dating, these extreme | 147 | activity or tsunami events. Based on radiocarbon dating, these extreme | ||
| 138 | events occurred around 5250, 4000, 3600, 3010, 2300, 1350, 650, and 80 | 148 | events occurred around 5250, 4000, 3600, 3010, 2300, 1350, 650, and 80 | ||
| 139 | years calaEuro-BP. No comparable events have been observed during the | 149 | years calaEuro-BP. No comparable events have been observed during the | ||
| 140 | 20th and 21st centuries. The results indicate little likelihood of a | 150 | 20th and 21st centuries. The results indicate little likelihood of a | ||
| 141 | tsunami origin for these coarse-grained layers, although historical | 151 | tsunami origin for these coarse-grained layers, although historical | ||
| 142 | tsunami events are recorded in this region. These periods of surge | 152 | tsunami events are recorded in this region. These periods of surge | ||
| 143 | events seem to coincide with the coldest periods in Europe during the | 153 | events seem to coincide with the coldest periods in Europe during the | ||
| 144 | late Holocene, suggesting a control by a climatic mechanism for | 154 | late Holocene, suggesting a control by a climatic mechanism for | ||
| 145 | periods of increased storm activity. Spectral analyses performed on | 155 | periods of increased storm activity. Spectral analyses performed on | ||
| 146 | the sand percentage revealed four major periodicities of 1228aEuro-+/- | 156 | the sand percentage revealed four major periodicities of 1228aEuro-+/- | ||
| 147 | aEuro-327, 732aEuro-+/- aEuro-80, 562aEuro-+/- aEuro-58, and | 157 | aEuro-327, 732aEuro-+/- aEuro-80, 562aEuro-+/- aEuro-58, and | ||
| 148 | 319aEuro-+/- aEuro-16 years. Amongst the well-known proxies that have | 158 | 319aEuro-+/- aEuro-16 years. Amongst the well-known proxies that have | ||
| 149 | revealed a millennial-scale climate variability during the Holocene, | 159 | revealed a millennial-scale climate variability during the Holocene, | ||
| 150 | the ice-rafted debris (IRD) indices in the North Atlantic developed by | 160 | the ice-rafted debris (IRD) indices in the North Atlantic developed by | ||
| 151 | Bond et al. (1997, 2001) present a cyclicity of 1470aEuro-+/- | 161 | Bond et al. (1997, 2001) present a cyclicity of 1470aEuro-+/- | ||
| 152 | aEuro-500 years, which matches the 1228aEuro-+/- aEuro-327-year | 162 | aEuro-500 years, which matches the 1228aEuro-+/- aEuro-327-year | ||
| 153 | periodicity evidenced in the Mar Menor, considering the respective | 163 | periodicity evidenced in the Mar Menor, considering the respective | ||
| 154 | uncertainties in the periodicities. Thus, an in-phase storm activity | 164 | uncertainties in the periodicities. Thus, an in-phase storm activity | ||
| 155 | in the western Mediterranean is found with the coldest periods in | 165 | in the western Mediterranean is found with the coldest periods in | ||
| 156 | Europe and with the North Atlantic thermohaline circulation. However, | 166 | Europe and with the North Atlantic thermohaline circulation. However, | ||
| 157 | further investigations, such as additional coring and high-resolution | 167 | further investigations, such as additional coring and high-resolution | ||
| 158 | coastal imagery, are needed to better constrain the main cause of | 168 | coastal imagery, are needed to better constrain the main cause of | ||
| 159 | these multiple events." | 169 | these multiple events." | ||
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