Abstract. Azooxanthellate cold-water corals (CWCs) have a global
distribution and have commonly been found in areas of active fluid seepage.
The relationship between the CWCs and these fluids, however, is not well
understood. This study aims to unravel the relationship between CWC
development and hydrocarbon-rich seepage in Pompeia Province (Gulf of
Cádiz, Atlantic Ocean). This region is comprised of mud volcanoes (MVs), coral
ridges and fields of coral mounds, which are all affected by the
tectonically driven seepage of hydrocarbon-rich fluids. These types of seepage, for example, focused, scattered, diffused or eruptive, is tightly controlled by a
complex system of faults and diapirs. Early diagenetic carbonates from the
currently active Al Gacel MV exhibit δ13C signatures down to
−28.77 ‰ Vienna Pee Dee Belemnite (VPDB), which indicate biologically derived methane
as the main carbon source. The same samples contain 13C-depleted lipid
biomarkers diagnostic for archaea such as crocetane (δ13C down
to −101.2 ‰ VPDB) and pentamethylicosane (PMI) (δ13C down to
−102.9 ‰ VPDB), which is evidence of microbially mediated
anaerobic oxidation of methane (AOM). This is further supported by next
generation DNA sequencing data, demonstrating the presence of AOM-related
microorganisms (ANMEs, archaea, sulfate-reducing bacteria) in the carbonate.
Embedded corals in some of the carbonates and CWC fragments exhibit less
negative δ13C values (−8.08 ‰ to −1.39 ‰ VPDB), pointing against the use of methane as the carbon source. Likewise,
the absence of DNA from methane- and sulfide-oxidizing microbes in sampled
coral does not support the idea of these organisms having a chemosynthetic lifestyle.
In light of these findings, it appears that the CWCs benefit rather indirectly
from hydrocarbon-rich seepage by using methane-derived authigenic carbonates
as a substratum for colonization. At the same time, chemosynthetic organisms
at active sites prevent coral dissolution and necrosis by feeding on the
seeping fluids (i.e., methane, sulfate, hydrogen sulfide), allowing
cold-water corals to colonize carbonates currently affected by
hydrocarbon-rich seepage.