2014
DOI: 10.1007/s00367-014-0368-0
|View full text |Cite
|
Sign up to set email alerts
|

Geophysical exploration of an active pockmark field in the Bay of Concarneau, southern Brittany, and implications for resident suspension feeders

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

2
28
0
2

Year Published

2014
2014
2022
2022

Publication Types

Select...
6
1

Relationship

2
5

Authors

Journals

citations
Cited by 25 publications
(32 citation statements)
references
References 52 publications
2
28
0
2
Order By: Relevance
“…about 2 pocks km −2 , or 500 pockmarks altogether, in the 179 km 2 of the inner Oslo fjord, Norway) (Webb et al 2009c) or higher densities of about 200 pocks km −2 in Belfast Bay (United Kingdom) (Hovland & Judd 1988, Kelley et al 1994. To our knowledge, the highest densities of pockmarks found to date are those discovered in muddy sediments of South Brittany (France), where up to 2500 pocks km −2 were recorded (Baltzer et al 2014).…”
Section: Introductionmentioning
confidence: 75%
See 2 more Smart Citations
“…about 2 pocks km −2 , or 500 pockmarks altogether, in the 179 km 2 of the inner Oslo fjord, Norway) (Webb et al 2009c) or higher densities of about 200 pocks km −2 in Belfast Bay (United Kingdom) (Hovland & Judd 1988, Kelley et al 1994. To our knowledge, the highest densities of pockmarks found to date are those discovered in muddy sediments of South Brittany (France), where up to 2500 pocks km −2 were recorded (Baltzer et al 2014).…”
Section: Introductionmentioning
confidence: 75%
“…1A−C). Several thousand pockmarks have recently been mapped in this area of 36 km 2 (Baltzer et al 2014). This bay resembles many coastal embayments in Brittany be cause it is sheltered by a succession of rocky islets and is characterized by soft-bottom substrates, spanning from mud to muddy sand, with depths ranging from 15 to 35 m (Ehrhold et al 2006).…”
Section: Study Sitementioning
confidence: 99%
See 1 more Smart Citation
“…The two main habitats engineered by H. nirae (termed hereafter “ Haploops habitats”) in the northeastern Atlantic are located on the Brittany coast, in the Bay of Concarneau and the Bay of Vilaine (Ehrhold, Hamon, & Guillaumont, ; Glémarec, Le Bris, & Le Guellec, ; Rigolet, ). Opportunistic video surveys revealed continuous expansion of the two Haploops habitats over the last two decades (Baltzer et al., ; Ehrhold et al., ). To explain the ecological succession of these habitats, it was suggested that Haploops colonization of surrounding habitats is facilitated by the presence of the tubiculous polychaete Maldane glebifex (Glémarec et al., ), which is associated with the Amphiura filiformis sandy‐mud habitat.…”
Section: Introductionmentioning
confidence: 99%
“…1). Although the initial pockmark craters are thought to be formed during seismic events (Baltzer et al, 2014), pockmarks could be activated when the tidal pressure would be high enough during spring tides, leading to the formation of plumes in the water column.…”
Section: Triggering and Control Mechanismsmentioning
confidence: 99%