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)

Website: https://www.bco-dmo.org/dataset/3904
Data Type: Cruise Results
Version:
Version Date: 2013-04-02

Project
» Canyon Krill (Canyon Krill)
ContributorsAffiliationRole
Lawson, GarethWoods Hole Oceanographic Institution (WHOI)Principal Investigator
Copley, NancyWoods Hole Oceanographic Institution (WHOI)Technician, BCO-DMO Data Manager


Dataset Description

Zooplankton displacement volumes from MOCNESS and Tucker Trawl net tows in and around Atlantis and Veatch Canyons south of Cape Cod.


Methods & Sampling

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 µm mesh size that can sample different regions of the water column. The underwater unit used was #169.

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.

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.  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.

SV/Cramer cruises: These are Tucker Trawl samples collected on annual 'JP new student cruises'. 

Displacement Volume Measurement:

Samples were poured into a 1000 ml graduated cylinders and measured.  Then the sample was poured through a 330 um sieve, allowed to drain, and the volume of water measured.  The difference between the two volume measurements was the displacement volume.  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.  Animals larger than 5 cc were measured individually and reported here.


Data Processing Description

Related information:

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.

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.


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Data Files

File
disp_vols_Canyons.csv
(Comma Separated Values (.csv), 17.28 KB)
MD5:311ddcd10ea10c963ca99fd9554102ce
Primary data file for dataset ID 3904

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Parameters

ParameterDescriptionUnits
cruise_id

cruise identification

alphanumeric
date_local

local date of tow

yyyymmdd
tow

MOCNESS tow number

integer
site

location of tow

text
lat_start

latitude at start of cruise; north is positive

decimal degrees
lon_start

longitude at start of cruise; east is positive

decimal degrees
lat_end

latitude at end of cruise; north is positive

decimal degrees
lon_end

longitude at end of cruise; east is positive

decimal degrees
yrday_local

local day and decimal time; e.g. 326.5 for the 326th day of the year November 22 at 1200 hours (noon)

nd
time_local

local time

HHMM
day_night

whether cruise was taken in day or night

text
net

net number

integer
depth_range

depth range of sample

meters
depth_open

depth where net opened

meters
depth_close

depth where net closed

meters
depth_mid

mid-depth of sample

meters
depth_interval

depth interval

meters
vol_filt

volume filtered by net

cubic meters
disp_vol_m3

displacement volume per cubic meter

cc/meter^3
comments_sample

comments pertaining to the sample

text
zoop_gt5cc_id

identification of animals > 5cc

text
disp_vol_lg

displacement volume of large animals

cc
dominants

dominant zooplankton in the sample

text
inst

The instrument used to make zooplankton collections: MOC = MOCNESS 1m^2; TT = Tucker Trawl.

text


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Instruments

Dataset-specific Instrument Name
Generic Instrument Name
Hydroacoustic Technology Incorporated echosounder
Generic Instrument Description
The Hydroacoustic Technology Inc. (HTI) multi-frequency system is a towed digital split-beam/single-beam hydroacoustic system designed specifically to assess the abundance and distribution of fish and plankton. Digital signal processing hardware is combined with a MS Windows2000/XP -based user interface to produce results in real time. (http://www.htisonar.com/multi_frequency_echo_sounder.htm)

Dataset-specific Instrument Name
MOCNESS
Generic Instrument Name
MOCNESS
Dataset-specific Description
1 m^2 MOCNESS with 335 micron mesh, 9 nets.
Generic Instrument Description
The Multiple Opening/Closing Net and Environmental Sensing System or MOCNESS is a family of net systems based on the Tucker Trawl principle. There are currently 8 different sizes of MOCNESS in existence which are designed for capture of different size ranges of zooplankton and micro-nekton Each system is designated according to the size of the net mouth opening and in two cases, the number of nets it carries. The original MOCNESS (Wiebe et al, 1976) was a redesigned and improved version of a system described by Frost and McCrone (1974).(from MOCNESS manual) This designation is used when the specific type of MOCNESS (number and size of nets) was not specified by the contributing investigator.

Dataset-specific Instrument Name
Tucker Trawl
Generic Instrument Name
Tucker Trawl
Dataset-specific Description
1 m^2 mouth opening with 335 micron mesh and 3 nets.
Generic Instrument Description
The original Tucker Trawl, a net with a rectangular mouth opening first built in 1951 by G.H. Tucker, was not an opening/closing system, but shortly thereafter it was modified so that it could be opened and closed.  The original had a 183 cm by 183 cm flexible rectangular mouth opening 914 cm long net with 1.8 cm stretched mesh for the first 457 cm and 1.3 cm mesh for last 457 cm. 152 cm of coarse plankton or muslin netting lined the end of the net. Tucker designed the net to collect animals associated with the deep scattering layers, principally euphausiids, siphonophores, and midwater fish. (from Wiebe and Benfield, 2003). Currently used Tucker Trawls usually have 1-m2 openings and can have a single net or multiple nets on the frame.


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Deployments

CT2010

Website
Platform
R/V Connecticut
Start Date
2010-07-08
End Date
2010-07-16
Description
The CT2010 cruise was supported by funds from Woods Hole Sea Grant, and field work was done on the southern New England Shelf and in nearby slope waters.  This is a different study area from the sites visited by the other Krill project cruises that sampled in the Gulf of Maine.

C223A

Website
Platform
SSV Corwith Cramer
Start Date
2009-06-30
End Date
2009-07-02
Description
WHOI/MIT Joint Program new student cruise

C230A

Website
Platform
SSV Corwith Cramer
Start Date
2010-07-25
End Date
2010-07-26
Description
WHOI/MIT Joint Program new student cruise

C235A

Website
Platform
SSV Corwith Cramer
Start Date
2011-07-02
End Date
2011-07-03
Description
WHOI/MIT Joint Program new student cruise

C241A

Website
Platform
SSV Corwith Cramer
Start Date
2012-07-01
End Date
2012-07-02
Description
WHOI/MIT Joint Program new student cruise


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Project Information

Canyon Krill (Canyon Krill)

Coverage: NW Atlantic slope canyons


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.

From poroposal:

OBJECTIVES:
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:
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.
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.

METHODOLOGY:
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.

RATIONALE:
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.

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.
 



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Funding

Funding SourceAward
Office of Naval Research (ONR)

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