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            <gco:CharacterString>Cite this dataset as: Lawson, G. (2013) Zooplankton biovolumes from R/V Connecticut, SSV Corwith Cramer, CT2010, C223A, C230A, C235A, C241A from Atlantis and Veatch Canyons, Atlantic Ocean from 2009-2012 (Canyon Krill project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). Version Date 2013-04-02 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/3904 [access date]</gco:CharacterString>
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        <gco:CharacterString>Zooplankton biovolumes from Atlantis and Veatch Canyons, 2009 to 2012 Dataset Description: &amp;lt;p&amp;gt;Zooplankton displacement volumes from MOCNESS and Tucker Trawl net tows in and around Atlantis and Veatch Canyons south of Cape Cod.&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;CT2010: A standard 1m^2 Multiple Opening/Closing Net and Environmental  Sensing System (MOCNESS) was used to collect zooplankton in order to  determine the taxonomic composition of the zooplankton in the study  region and also to ground truth acoustic data collected with the HTI  multi-frequency and Edgetech broadband systems. The MOCNESS has 9 nets  with a 335 &amp;amp;micro;m mesh size that can sample different regions of the water  column. The underwater unit used was #169.&amp;lt;/p&amp;gt;
&amp;lt;p&amp;gt;In addition to the standard temperature and conductivity probes the  system also had a beta-type strobe-light unit for reducing avoidance of  the nets by some zooplankton, notably krill, and possibly small fish.  The strobe system has two units each with 12 LED sets (LUXEON Rebel LED)  with peak output between 490-520 nm. Two of the 24 LED sets were  working inconsistently at the start of the sampling. The LEDs are  powered by the MOCNESS battery and their pulse width, amplitude, flash  rate period, and on/off are controlled by the MOCNESS software. For  EN484, the pulse width was 2 ms, the relative amplitude was 99%, and the  flash interval was 100 ms. For EN487, the pulse width was 40 ms, the  relative amplitude was 99%, and the flash interval was 1000 ms.&amp;lt;/p&amp;gt;
&amp;lt;p&amp;gt;The MOCNESS was launched and recovered from the stern A-frame.  Samples  were brought into the wet lab for processing. Net 0 typically  went form the surface to depth and nets 1-8 fished at discrete depths  from depth to the surface.&amp;amp;nbsp; Nets 1-8 were preserved in  buffered  formalin. Often the net 0 samples were so large that they  would have  taken multiple jars so either the entirety or a large  fraction was  frozen in the -80C freezer, in the hopes that they might be  useful.&amp;lt;/p&amp;gt;
&amp;lt;p&amp;gt;SV/Cramer cruises: These are Tucker Trawl samples collected on annual 'JP new student cruises'.&amp;amp;nbsp;&amp;lt;/p&amp;gt;
&amp;lt;p&amp;gt;&amp;lt;b&amp;gt;Displacement Volume Measurement:&amp;lt;/b&amp;gt;&amp;lt;/p&amp;gt;
&amp;lt;p&amp;gt;Samples were poured into a 1000 ml graduated cylinders and measured.&amp;amp;nbsp;  Then the sample was poured through a 330 um sieve, allowed to drain,  and the volume of water measured.&amp;amp;nbsp; The difference between the two volume  measurements was the displacement volume.&amp;amp;nbsp; The displacement volume of  each sample was divided by the volume filtered by the net (m^3) and the  result is reported here in units of cc/m^3.&amp;amp;nbsp; Animals larger than 5 cc  were measured individually and reported here.&amp;lt;/p&amp;gt;</gco:CharacterString>
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                            <gco:CharacterString>&lt;p&gt;Study of the krill populations in and around Atlantis and Veatch Canyons along the Slope Waters south of Cape Cod.  Zooplankton samples were collected with MOCNESS nets on th RV/Connecticut in 2010 and with a Tucker Trawl annually on the SVV/Corwith Cramer as part of the MIT/WHOI Joint Program new student cruise. The RV/Conncecticut cruise included broadband acoustics measurements of the water column to be correlated with the net samples.&lt;/p&gt;
&lt;p&gt;From poroposal:&lt;/p&gt;
&lt;p&gt;&lt;b&gt;OBJECTIVES:&lt;/b&gt;&lt;br /&gt;
The proposed work seeks to understand how physical forcing interacting with local bathymetry and with euphausiid active behaviors leads to the formation, persistence, and availability to predators of euphausiid aggregations in the deep canyons of the New England continental shelf break, using newly-available broadband acoustic scattering techniques. The specific objectives are:&lt;br /&gt;
1. To identify and track a euphausiid aggregation in a shelf break canyon in order to quantify changes in aggregation structure and position associated with variations in environmental conditions. Specifically, we will address the hypothesis that the formation and variability of euphausiid aggregations in such canyons relate to the interaction of the flow field, especially upwelling, with the sloping canyon topography and with the euphausiids’ vertical movements and active aggregative behaviors.&lt;br /&gt;
2. To test and demonstrate the power of newly-available broadband acoustic scattering techniques for remotely discriminating euphausiids from other sources of acoustic scattering and making accurate and highresolution estimates of euphausiid abundance and size.&lt;/p&gt;
&lt;p&gt;&lt;b&gt;METHODOLOGY:&lt;/b&gt;&lt;br /&gt;
To achieve these objectives, we propose an innovative and comprehensive field program targeting Atlantis Canyon, southwest of Georges Bank. An initial 24-hour 'canyon' survey will be conducted to characterize the overall distribution of euphausiids, other zooplankton (especially copepods), higher predators, and the physical environment. This will be followed by a 48-hour 'tracking' survey of an individual euphausiid aggregation. Surveys will be conducted in September 2010, timed to occur shortly after the Northeast Fisheries Science Center bottom trawl survey of the greater region. In both survey modes, the primary sampling instrument will be a broadband acoustic scattering system (40-600 kHz). Broadband measurements, supplemented by measurements from a more traditional narrowband multi-frequency acoustic system (43, 120, 200, 420 kHz), will be used to quantify the abundance, size, and aggregation structure of euphausiids, as well as the abundance of fish predators and other zooplankton (e.g., copepods). These acoustic estimates of biological quantities will be validated via direct samples collected concurrently with a depth-stratified net system and an image-forming optical system. Characterization of the physical environment and flow field will be achieved via an Acoustic Doppler Current Profiler (ADCP) and a Conductivity-Temperature-Depth (CTD) system also equipped with a fluorometer to estimate the abundance of phytoplankton. During analysis, measurements of the characteristics, movements, and distribution of euphausiid aggregations will be related to these concurrent measurements of the physical and biological environment.&lt;/p&gt;
&lt;p&gt;&lt;b&gt;RATIONALE:&lt;/b&gt;&lt;br /&gt;
Euphausiids are common crustacean members of North Atlantic pelagic ecosystems, but their ecological role in the waters off New England is only poorly understood. Previous studies in the Gulf of Maine region have suggested that euphausiids (especially Meganyctiphanes norvegica and Thysanoessa spp.) can be locally abundant and a key prey item for a variety of higher predators, including commercially-exploited fish and squid. Euphausiids are also notable among zooplankton for their strong swimming capabilities and occurrence in dense aggregations; the formation of such aggregations is thought to be instrumental in determining the availability of euphausiids to higher predators. Overall, however, relatively little is known about the biological and physical processes leading to the formation and persistence of euphausiid aggregations, the interaction of euphausiids with their predators, and the overall significance of euphausiids in the New England Shelf/Slope ecosystem.&lt;/p&gt;
&lt;p&gt;Large and dense aggregations of euphausiids have been observed in the canyons of the New England shelf break. The continental shelf break represents a frontier region in current understanding of the dynamics of the western North Atlantic Ocean and its inhabitants, and this project is motivated by the hypothesis advanced in the literature that these aggregations play an important role in subsidizing the productivity of commercial fish and squid stocks in shallower reaches of the shelf. By addressing the bio-physical factors that lead to the aggregation of euphausiids and that determine their availability to higher predators in these canyon regions, the proposed work will take a necessary first step towards defining the essential habitat of fish predators that target euphausiids and quantifying their interaction for the development of ecosystem-based management models. Beneficiaries of the project thus include scientists and managers with National Marine Fisheries Service, the fishing industry, and society as a whole. The project furthermore will demonstrate the feasibility of using newly-available broadband acoustic scattering techniques for quantifying the abundance and size of euphausiids and other pelagic animals, which we anticipate will be of substantial use in the monitoring of marine pelagic habitats globally.&lt;br /&gt;
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	Name: cruise_id
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	Description: &lt;p&gt;cruise identification&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/33531.rdf
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http://lod.bco-dmo.org/id/dataset-parameter/33532.rdf
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	Units: integer
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http://lod.bco-dmo.org/id/dataset-parameter/33533.rdf
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http://lod.bco-dmo.org/id/dataset-parameter/33534.rdf
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	Units: decimal degrees
	Description: &lt;p&gt;latitude at start of cruise; north is positive&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/33535.rdf
	Name: lon_start
	Units: decimal degrees
	Description: &lt;p&gt;longitude at start of cruise; east is positive&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/33536.rdf
	Name: lat_end
	Units: decimal degrees
	Description: &lt;p&gt;latitude at end of cruise; north is positive&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/33537.rdf
	Name: lon_end
	Units: decimal degrees
	Description: &lt;p&gt;longitude at end of cruise; east is positive&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/33538.rdf
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http://lod.bco-dmo.org/id/dataset-parameter/33539.rdf
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http://lod.bco-dmo.org/id/dataset-parameter/33540.rdf
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	Units: text
	Description: &lt;p&gt;whether cruise was taken in day or night&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/33541.rdf
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	Units: integer
	Description: &lt;p&gt;net number&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/33542.rdf
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	Units: meters
	Description: &lt;p&gt;depth range of sample&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/33543.rdf
	Name: depth_open
	Units: meters
	Description: &lt;p&gt;depth where net opened&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/33544.rdf
	Name: depth_close
	Units: meters
	Description: &lt;p&gt;depth where net closed&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/33545.rdf
	Name: depth_mid
	Units: meters
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http://lod.bco-dmo.org/id/dataset-parameter/33546.rdf
	Name: depth_interval
	Units: meters
	Description: &lt;p&gt;depth interval&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/33547.rdf
	Name: vol_filt
	Units: cubic meters
	Description: &lt;p&gt;volume filtered by net&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/33548.rdf
	Name: disp_vol_m3
	Units: cc/meter^3
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http://lod.bco-dmo.org/id/dataset-parameter/33549.rdf
	Name: comments_sample
	Units: text
	Description: &lt;p&gt;comments pertaining to the sample&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/33550.rdf
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	Units: text
	Description: &lt;p&gt;identification of animals &amp;gt; 5cc&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/33551.rdf
	Name: disp_vol_lg
	Units: cc
	Description: &lt;p&gt;displacement volume of large animals&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/33552.rdf
	Name: dominants
	Units: text
	Description: &lt;p&gt;dominant zooplankton in the sample&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/33553.rdf
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&amp;lt;p&amp;gt;In addition to the standard temperature and conductivity probes the  system also had a beta-type strobe-light unit for reducing avoidance of  the nets by some zooplankton, notably krill, and possibly small fish.  The strobe system has two units each with 12 LED sets (LUXEON Rebel LED)  with peak output between 490-520 nm. Two of the 24 LED sets were  working inconsistently at the start of the sampling. The LEDs are  powered by the MOCNESS battery and their pulse width, amplitude, flash  rate period, and on/off are controlled by the MOCNESS software. For  EN484, the pulse width was 2 ms, the relative amplitude was 99%, and the  flash interval was 100 ms. For EN487, the pulse width was 40 ms, the  relative amplitude was 99%, and the flash interval was 1000 ms.&amp;lt;/p&amp;gt;
&amp;lt;p&amp;gt;The MOCNESS was launched and recovered from the stern A-frame.  Samples  were brought into the wet lab for processing. Net 0 typically  went form the surface to depth and nets 1-8 fished at discrete depths  from depth to the surface.&amp;amp;nbsp; Nets 1-8 were preserved in  buffered  formalin. Often the net 0 samples were so large that they  would have  taken multiple jars so either the entirety or a large  fraction was  frozen in the -80C freezer, in the hopes that they might be  useful.&amp;lt;/p&amp;gt;
&amp;lt;p&amp;gt;SV/Cramer cruises: These are Tucker Trawl samples collected on annual 'JP new student cruises'.&amp;amp;nbsp;&amp;lt;/p&amp;gt;
&amp;lt;p&amp;gt;&amp;lt;b&amp;gt;Displacement Volume Measurement:&amp;lt;/b&amp;gt;&amp;lt;/p&amp;gt;
&amp;lt;p&amp;gt;Samples were poured into a 1000 ml graduated cylinders and measured.&amp;amp;nbsp;  Then the sample was poured through a 330 um sieve, allowed to drain,  and the volume of water measured.&amp;amp;nbsp; The difference between the two volume  measurements was the displacement volume.&amp;amp;nbsp; The displacement volume of  each sample was divided by the volume filtered by the net (m^3) and the  result is reported here in units of cc/m^3.&amp;amp;nbsp; Animals larger than 5 cc  were measured individually and reported here.&amp;lt;/p&amp;gt;</gco:CharacterString>
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&amp;lt;p&amp;gt;Wiebe, P.H., K.H. Burt, S.H. Boyd, and A.W. Morton, A multiple  opening-closing net and environmental sensing system for sampling  zooplankton, J. Mar. Res., 34, 312-326, 1976.&amp;lt;br /&amp;gt;
&amp;lt;br /&amp;gt;
Wiebe, P.H., A.W. Morton, A.M. Bradley, J.E. Craddock, T.J. Cowles, V.A.  Barber, R.H. Backus, and G.R. Flierl, New developments in the MOCNESS,  an apparatus for sampling zooplankton and micronekton, Mar. Biol., 87,  313-323, 1985.&amp;lt;/p&amp;gt;</gco:CharacterString>
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