Abstract

The ECOMAR project investigated photosynthetically-supported life on the North Mid-Atlantic Ridge (MAR) between the Azores and Iceland focussing on the Charlie–Gibbs Fracture Zone area in the vicinity of the sub-polar front where the North Atlantic Current crosses the MAR. Repeat visits were made to four stations at 2500m depth on the flanks of the MAR in the years 2007–2010; a pair of northern stations at 54°N in cold water north of the sub-polar front and southern stations at 49°N in warmer water influenced by eddies from the North Atlantic Current. At each station an instrumented mooring was deployed with current meters and sediment traps (100 and 1000m above the sea floor) to sample downward flux of particulate matter. The patterns of water flow, fronts, primary production and export flux in the region were studied by a combination of remote sensing and in situ measurements. Sonar, tow nets and profilers sampled pelagic fauna over the MAR. Swath bathymetry surveys across the ridge revealed sediment-covered flat terraces parallel to the axis of the MAR with intervening steep rocky slopes. Otter trawls, megacores, baited traps and a suite of tools carried by the R.O.V. Isis including push cores, grabs and a suction device collected benthic fauna. Video and photo surveys were also conducted using the SHRIMP towed vehicle and the R.O.V. Isis. Additional surveying and sampling by landers and R.O.V. focussed on the summit of a seamount (48°44′N, 28°10′W) on the western crest of the MAR between the two southern stations.

Highlights

  • The Mid-Atlantic Ridge (MAR) was described by Murray and Hjort (1912) as dividing the ocean into eastern and western deep basins from Iceland to at least 531S

  • Heezen and Tharp (1957) in their map of the bathymetry of the North Atlantic Ocean first indicated the discontinuous nature of the MAR with transverse fractures at intervals along the axis of the ridge

  • Many arguments regarding the biology of the seamounts (Rowden et al, 2010; Clark et al, 2010) are applicable to mid-ocean ridges which can be considered as complex aggregations of sea mounts

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Summary

Introduction

The Mid-Atlantic Ridge (MAR) was described by Murray and Hjort (1912) as dividing the ocean into eastern and western deep basins from Iceland to at least 531S. The Census of Marine Life project MAR-ECO (Patterns and Process of the Ecosystems of the North Mid-Atlantic) was organised to investigate photosynthetically-supported life on the segment of the MAR between Iceland and the Azores (Vecchione et al, 2010) As part of this project in 2004 the R.V. GO Sars undertook surveys at 38 superstations from 60118′N to 41122′N sampling fauna from the sea surface to the sea floor using a wide range of devices including sonars, trawls and remotely operated vehicles (ROVs) (Wenneck et al, 2008).

18 August 15 August 9 September
The effect of the Mid-Atlantic Ridge
The effect of the sub-polar front and CGFZ
August 2007 8 June 2010
Materials and methods
Cruises
Station locations
Overview of results
Findings
Conclusions
Full Text
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