Jump to main content
US EPA
United States Environmental Protection Agency
Search
Search
Main menu
Environmental Topics
Laws & Regulations
About EPA
Health & Environmental Research Online (HERO)
Contact Us
Print
Feedback
Export to File
Search:
This record has one attached file:
Add More Files
Attach File(s):
Display Name for File*:
Save
Citation
Tags
HERO ID
3469564
Reference Type
Journal Article
Title
Pockmarks and methanogenic carbonates above the giant Troll gas field in the Norwegian North Sea
Author(s)
Mazzini, A; Svensen, HH; Planke, S; Forsberg, CF; Tjelta, TI
Year
2016
Is Peer Reviewed?
1
Journal
Marine Geology
ISSN:
0025-3227
EISSN:
1872-6151
Volume
373
Page Numbers
26-38
DOI
10.1016/j.margeo.2015.12.012
Web of Science Id
WOS:000371364700003
Abstract
Acoustic imaging has revealed more than 7000 pockmarks on the seafloor above the Troll East gas field in the Norwegian North Sea. We present the first comprehensive study conducted on one of the World's largest pockmark fields complementing the acoustic data with extensive sampling, geochemical and petrographical studies. Specifically, we aimed at detecting possible active seepage still present over this vast area.The pockmarks are present as isolated structures, on average similar to 35 m wide and up to 100 m in size. In addition, smaller satellite pockmarks surround some of the pockmarks. In contrast to the muddy surroundings, parts of the investigated pockmarks contain laterally extensive carbonate deposits or meter sized carbonate blocks. These blocks provide shelter to abundant colonies of benthic megafauna. The carbonate blocks are comprised of micritic Mg-calcite and calcite, micritic aragonite, and botryoidal aragonite. Framboidal pyrite is also commonly present. Carbon isotopic values of the carbonates are C-13-depleted (delta C-13 as low as - 59.7 parts per thousand) and with delta O-18 up to 4.5 parts per thousand, indicating a methanogenic origin, possibly linked to gas hydrate dissociation. Pore water extracted from shallow cores from the centre and the flanks of the pockmarks show similar Cl and SO4 profiles as the reference cores outside the pockmarks, ruling out active methane seepage. This conclusion is also supported by seafloor video observations that did not reveal any evidence of visual fluid seepage, and by the absence of microbial mats and by the fact that the carbonate blocks are exposed on the seafloor and party oxidized on the surface. We conclude that methane seepage formed this extensive gas field following to gas hydrate dissociation. (C) 2016 Elsevier B.V. All rights reserved.
Keywords
Norwegian North Sea; Troll; Methanogenic carbonates; Pockmarks; Gas hydrates
Home
Learn about HERO
Using HERO
Search HERO
Projects in HERO
Risk Assessment
Transparency & Integrity