A climatic trigger for the giant Troll pockmark field in the northern North Sea
Autor: | Henriette Linge, Stein-Erik Lauritzen, Haflidi Haflidason, Tor Inge Tjelta, Sverre Planke, Carl Fredrik Forsberg, Øyvind Hammer, Henrik Svensen, Adriano Mazzini |
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Jazyk: | angličtina |
Rok vydání: | 2017 |
Předmět: |
010504 meteorology & atmospheric sciences
pockmarks Clathrate hydrate Geochemistry 010502 geochemistry & geophysics 01 natural sciences Modelling law.invention Continental margin Geochemistry and Petrology law Earth and Planetary Sciences (miscellaneous) Deglaciation Radiocarbon dating Younger Dryas Holocene gas hydrates dissociation 0105 earth and related environmental sciences Pockmark Troll Seafloor spreading Norwegian North Sea Geophysics Oceanography 13. Climate action Space and Planetary Science Geology |
Zdroj: | Earth and Planetary Science Letters |
ISSN: | 0012-821X |
Popis: | Pockmarks are seafloor craters usually formed during methane release on continental margins. However, the mechanisms behind their formation and dynamics remain elusive. Here we report detailed investigations on one of the World's largest pockmark fields located in the Troll region in the northern North Sea. Seafloor investigations show that >7000 pockmarks are present in a ∼600 km2 area. A similar density of pockmarks is likely present over a 15,000 km2 region outside our study area. Based on extensive monitoring, coring, geophysical and geochemical analyses, no indications of active gas seepage were found. Still, geochemical data from carbonate blocks collected from these pockmarks indicate a methanogenic origin linked to gas hydrate dissociation and past fluid venting at the seafloor. We have dated the carbonates using the U–Th method in order to constrain the pockmark formation. The carbonates gave an isochron age of 9.59±1.38 ka9.59±1.38 ka, i.e. belonging to the initial Holocene. Moreover, radiocarbon dating of microfossils in the sediments inside the pockmarks is consistent with the ages derived from the carbonates. Based on pressure and temperature modelling, we show that the last deglaciation could have triggered dissociation of gas hydrates present in the region of the northern part of the Norwegian Channel, causing degassing of 0.26 MtCH4/km2 at the seafloor. Our results stress the importance of external climatic forcing of the dynamics of the seafloor, and the role of the rapid warming following the Younger Dryas in pacing the marine gas hydrate reservoir. Mazzini, Adriano, et al. "A climatic trigger for the giant Troll pockmark field in the northern North Sea." Earth and Planetary Science Letters 464 (2017): 24-34. © 2017. This manuscript version is made available under the CC-BY-NC-ND 4.0 license. |
Databáze: | OpenAIRE |
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