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Smooth Bottom Net Trawl Fishing Gear Effect on - New England ...

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NOAA/NMFS Unallied Science Project, Cooperative Agreement NA16FL2264 May 2005<br />

<str<strong>on</strong>g>Smooth</str<strong>on</strong>g> <str<strong>on</strong>g>Bottom</str<strong>on</strong>g> <str<strong>on</strong>g>Net</str<strong>on</strong>g> <str<strong>on</strong>g>Trawl</str<strong>on</strong>g> <str<strong>on</strong>g>Fishing</str<strong>on</strong>g> <str<strong>on</strong>g>Gear</str<strong>on</strong>g> <str<strong>on</strong>g>Effect</str<strong>on</strong>g> <strong>on</strong> the Seabed:<br />

Investigati<strong>on</strong> of Temporal and Cumulative <str<strong>on</strong>g>Effect</str<strong>on</strong>g>s BKAM/CR<br />

Figure 3.2.2.4 –1b November 2002 grab sample locati<strong>on</strong>s al<strong>on</strong>g Mud Hole Lane 1 at stati<strong>on</strong> B.<br />

Mud Hole C<strong>on</strong>trol Lane 2 in the Vicinity of Stati<strong>on</strong> B<br />

Bathymetric data shows that stati<strong>on</strong> MH-2B is located at the toe of a slope that rises to the<br />

northwest (Figure 3.2.1-1) in an area that appears to be characterized by flat sandy mud (see<br />

Appendix 3.2A Figure TS-6). Pre-trawl s<strong>on</strong>ar data for stati<strong>on</strong> MH-2B shows faint background<br />

trawl gear impacts.<br />

Lane 2 in Mud Hole was designated a c<strong>on</strong>trol lane, however, some project-related gear impacts<br />

were observed in the western porti<strong>on</strong>s of the September 30 th and November 20 th s<strong>on</strong>ar imagery in<br />

the vicinity of MH-2B. These gear impacts appear to have come within approximately 25meters<br />

of the centerline of lane 2, i.e. just within the western edge of this c<strong>on</strong>trol lane. As shown<br />

<strong>on</strong> Figure 3.2.2.4-2a (below) two of the grab samples collected in October may have been<br />

compromised by these trawl impacts (i.e. the MH2B grain size sample and the MH-2B benthic<br />

grab replicate 1). All November grab samples were collected from n<strong>on</strong>-impacted areas closer to<br />

the center of this c<strong>on</strong>trol lane (Figure 3.2.2.4-2b). Background door marks were still visible <strong>on</strong><br />

the September and November side-scan imagery. Again trawl scours in November appeared<br />

broader and less distinct than in previous records and likely due to sediment transport from<br />

bottom currents associated with the November storm.<br />

29

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