Carbonate blocks found in muddy sediment off Cape Breton Island, Nova Scotia: pieces of small authigenic carbonate mounds and vents related to hydrocarbon seeps?

• Published in: Atlantic Geology
• Main Authors: Wallace, Peter, Harrington, Matt, Cook, Ryan
• Format: Article in Journal/Newspaper
• Language: English
• Published: Atlantic Geoscience Society 2006
• Subjects: Breton Island; Dee
• Online Access: https://journals.lib.unb.ca/index.php/ag/article/view/2783

Carbonate blocks brought up from the seafloor during drag fishing in a small restricted area offshore northern Cape Breton Island are irregularly shaped and range in size from 6 cm3 to > 1 m3. They have smooth to "clinkery", dendritic, or "popcorn-surface" structures, can be layered to massive, and are porous. Many are highly porous and/or eroded. They contain fine-grained siliciclastic material (mud to granule sized) with minor amounts of bioclasts cemented by calcite. Three blocks have vent structures and some have pores lined by fine-grained sparite. Seismic lines in the vicinity of the discovery area show acoustic turbidity, bright spots interpreted to be hydrocarbon seeps, diaper-like structures, and columnar sediment disturbances that reach to bedrock. Outside the immediate area, pock marks occur on the sediment surface. Carbon isotope values from shelly material cemented in the blocks range from δ13C = -9.41 to -35.27 ‰ PDB (Pee Dee Belemnite) with an algae encrustation or bacterial mat yielding -61.38 ‰ PDB. From the isotopic analysis and the seismic interpretation we are confident that these blocks are pieces of carbonate mounds and vents formed by methanogenesis of hydrocarbon from slow seeps on the seafloor, the hydrocarbon originating either within the recent sediment and/or from bedrock, most likely the latter. The ecology of these mounds has not been studied and needs further work in this area of active commercial fishing. RÉSUMÉ Les blocs de roches carbonatées repêchées du fond de la mer par des chalutiers dans un petit secteur à accès restreint au large, au nord de l'île du Cap-Breton, sont d'apparence irrégulière et leur taille varie entre 6 cm3 et plus de 1 m3. Ils sont de texture lisse à « scoriacée », sont de nature dendritique et présentent une surface de « maïs éclaté »; les blocs peuvent être stratifiés ou d'apparence massive, et ils sont poreux. Un bon nombre des blocs sont très poreux ou érodés, ou les deux. Ils contiennent du matériau silicoclastique à grain fin (entre la boue et les ...