http://lod.bco-dmo.org/id/dataset/546069
eng; USA
utf8
dataset
Highest level of data collection, from a common set of sensors or instrumentation, usually within the same research project
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
2015-01-21
ISO 19115-2 Geographic Information - Metadata - Part 2: Extensions for Imagery and Gridded Data
ISO 19115-2:2009(E)
Current velocities from 4 depths recorded by ADCP deployed in Kimbe Bay, New Britain, Papua New Guinea from 2010-2011 (Pop connectivity of coral reef fishes project)
2014-05-01
publication
2014-05-01
revision
BCO-DMO Linked Data URI
2014-05-01
creation
http://lod.bco-dmo.org/id/dataset/546069
Simon Thorrold
Woods Hole Oceanographic Institution
principalInvestigator
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
publisher
Cite this dataset as: Thorrold, S. (2014) Current velocities from 4 depths recorded by ADCP deployed in Kimbe Bay, New Britain, Papua New Guinea from 2010-2011 (Pop connectivity of coral reef fishes project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 01 May 2014) Version Date 2014-05-01 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/546069 [access date]
Current velocities from 4 depths recorded by ADCP deployed in Kimbe Bay, New Britain, Papua New Guinea. Dataset Description: <p>Current velocities from 4 depths recorded by acoustic Doppler current profilers (ADCP) deployed at locations in Kimbe Bay, New Britain, Papua New Guinea.</p>
<p>Original MatLab files are provided.</p> Methods and Sampling: <p>Standard bottom-mounted (i.e. looking up) deployment of ADCPs.</p>
Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-0928442 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=0928442
completed
Simon Thorrold
Woods Hole Oceanographic Institution
508-289-3366
266 Woods Hole Rd, MS #50
Woods Hole
MA
02543
USA
sthorrold@whoi.edu
pointOfContact
asNeeded
Dataset Version: 01 May 2014
Unknown
depth
matlab_file
Bottom-mounted ADCP
theme
None, User defined
depth
file_link
featureType
BCO-DMO Standard Parameters
Acoustic Doppler Current Profiler
instrument
BCO-DMO Standard Instruments
Thorrold_ADCP_Kimbe
service
Deployment Activity
Kimbe Bay, New Britain, Papua New Guinea
place
Locations
otherRestrictions
otherRestrictions
Access Constraints: none. Use Constraints: Please follow guidelines at: http://www.bco-dmo.org/terms-use Distribution liability: Under no circumstances shall BCO-DMO be liable for any direct, incidental, special, consequential, indirect, or punitive damages that result from the use of, or the inability to use, the materials in this data submission. If you are dissatisfied with any materials in this data submission your sole and exclusive remedy is to discontinue use.
Larval Dispersal and Retention Among Sub-populations of Coral Reef Fishes: A Multi-Technique Approach
https://osprey.bco-dmo.org/project/514412
Larval Dispersal and Retention Among Sub-populations of Coral Reef Fishes: A Multi-Technique Approach
<p><em>Description from NSF award abstract:</em></p>
<p>Population connectivity, the degree to which geographically-separated groups are linked by dispersal, is a critical parameter in the dynamics of marine populations. Connectivity rates determine colonization patterns of new habitats, the resiliency of populations to harvest, and the design of networks of No Take Marine Reserves (NTMRs). Quantifying exchange rates in marine organisms is extremely difficult because natal origins of adults are almost invariably unknown. This lack of knowledge is primarily due to the difficulty of conducting mark-recapture studies in species with large numbers of small pelagic offspring that suffer high initial mortality rates. This project will continue a multi-technique approach combining mass-marking of fish embryos using TRAnsgenerational Isotope Labeling (TRAIL) of otoliths and paternity analyses based on hypervariable microsatellite DNA markers to measure dispersal distances of coral reef fishes. Population connectivity will be estimated for two species (<em>Amphiprion percula</em> and <em>Chaetodon vagabundus</em>) in Kimbe Bay, Papua New Guinea.</p>
<p>Coral reef organisms are usually distributed across a mosaic of reefs that are sometimes separated by the ocean. It has been presumed that at small scales, reefs must be open populations, with significant exchange of larvae among neighboring reefs. At larger scales, populations must effectively be closed, with late-stage larvae returning to the same population as their parents. The scale over which this transition takes place is unknown. Recent evidence suggests that ecologically significant self-recruitment may occur at scales of individual reefs or islands. If accurate, these findings have important implications for management strategies for marine species, including the design of networks of NTMRs, because knowledge of dispersal distances determines the scale over which populations can be completely protected. It also determines the appropriate spacing of reserves to allow protected populations to replenish adjacent fished areas. This project will quantify population connectivity of coral reef fishes in Kimbe Bay, Papua New Guinea and broaden the spatial scale from examining the fate of larvae spawned at a single location (Kimbe Island) to examining connectivity among 5 designated NTMRs.</p>
<p>This award is funded under the American Recovery and Reinvestment Act of 2009 (Public Law 111-5).</p>
<p><strong>Publications Produced as a Result of this Project:</strong><br />
Saenz-Agudelo, P., G. P. Jones, S. R. Thorrold, and S. Planes. 2011. Detrimental effects of host anemone bleaching on anemonefish populations. <em>Coral Reefs</em>, v.30, p. 497. doi: <a href="http://dx.doi.org/10.1007/s00338-010-0716-0" target="_blank">10.1007/s00338-010-0716-0</a></p>
<p>Saenz-Agudelo, P., G. P. Jones, S. R. Thorrold, and S. Planes. 2011. Connectivity dominates larval replenishment in a coastal reef fish metapopulation<em>. Proc. Royal Soc. B</em>, v.278, p. 2954. doi: <a href="http://dx.doi.org/10.1098/rspb.2010.2780" target="_blank">10.1098/rspb.2010.2780 </a></p>
<p>Saenz-Agudelo, P., G. P. Jones, S. R. Thorrold, and S. Planes. 2012. Patterns and persistence of larval retention and connectivity in a marine fish metapopulation<em>. Molecular Ecology</em>, v.21, p. 4695. doi: <a href="http://dx.doi.org/10.1111/j.1365-294X.2012.05726.x" target="_blank">10.1111/j.1365-294X.2012.05726.x</a></p>
<p>Buston, P. M., G. P. Jones, S. Planes, and S. R. Thorrold. 2011. Probability of successful larval dispersal declines fivefold over 1 kilometre in a coral reef fish<em>. Proc. Royal Soc. B</em>, v.279. doi: <a href="http://dx.doi.org/10.1098/rspb.2011.2041" target="_blank">10.1098/rspb.2011.2041</a></p>
<p>Berumen, M. L., H. J. Walsh, N. Raventos, S. Planes, G. P. Jones, V. Starczak, and S. R. Thorrold. 2010. Otolith geochemistry does not reflect dispersal history of clownfish larvae<em>. Coral Reefs</em>, v.29, p. 883. doi: <a href="http://dx.doi.org/10.1007/s00338-010-0652-z" target="_blank">10.1007/s00338-010-0652-z</a></p>
<p>Berumen, M. L., G. Almany, S. Planes, G. P. Jones, and S. R. Thorrold. 2012. Persistence of self-recruitment and patterns of larval connectivity in a marine protected area network<em>. Ecology and Evolution</em>, v.2. doi: <a href="http://dx.doi.org/10.1002/ece3.208" target="_blank">10.1002/ece3.208</a></p>
<p>Dixson, D. L., G. P. Jones, P. L. munday, M. S. Pratchett, M. Srinivasan, S. Planes, and S. R. Thorrold. 2011. Terrestrial chemical cues help coral reef fish larvae locate settlement habitat surrounding islands<em>. Ecology and Evolution</em>, v.1, p. 586. doi: <a href="http://dx.doi.org/10.1002/ece3.53" target="_blank">10.1002/ece3.53</a></p>
<p>Harrison, H. B., D. H. Williamson, R. D. Evans, G. R. Almany, S. R. Thorrold, G. R. Russ, K. A. Feldheim, L. van Herwerden, S. Planes, M. Srinivasan, M. L. Berumen, and G. P. Jones. 2012. Larval export from marine reserves benefits fish and fisheries<em>. Current Biology</em>, v.22, p. 1023. doi: <a href="http://dx.doi.org/10.1016/j.cub.2012.04.008" target="_blank">10.1016/j.cub.2012.04.008</a></p>
<p>Roy, A. S., A. J. Frisch, C. Sims, S. R. Thorrold, and G. P. Jones. 2012. Retention of a transgenerational marker (137Ba) in tissues of adult female anemone fish and assessment of physiological stress. <em>Environmental Biology of Fishes</em>. doi: <a href="http://dx.doi.org/10.1007/s10641-012-0029-y" target="_blank">10.1007/s10641-012-0029-y</a></p>
Pop connectivity of coral reef fishes
largerWorkCitation
project
eng; USA
oceans
Kimbe Bay, New Britain, Papua New Guinea
2014-05-01
Kimbe Bay, Papua New Guinea
0
BCO-DMO catalogue of parameters from Current velocities from 4 depths recorded by ADCP deployed in Kimbe Bay, New Britain, Papua New Guinea from 2010-2011 (Pop connectivity of coral reef fishes project)
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
http://lod.bco-dmo.org/id/dataset-parameter/557543.rdf
Name: depth
Units: meters
Description: <p>Depth in meters.</p>
http://lod.bco-dmo.org/id/dataset-parameter/557544.rdf
Name: matlab_file
Units: text
Description: <p>Link to MatLab file for download.</p>
GB/NERC/BODC > British Oceanographic Data Centre, Natural Environment Research Council, United Kingdom
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
545
https://datadocs.bco-dmo.org/file/g77yqAKsqZEjwA/Kimbe_Bay_ADCP.csv
Kimbe_Bay_ADCP.csv
Primary data file for dataset ID 546069
download
https://osprey.bco-dmo.org/dataset/546069/data/download
download
onLine
dataset
<p>Standard bottom-mounted (i.e. looking up) deployment of ADCPs.</p>
Specified by the Principal Investigator(s)
<p>Current velocities from the ADCPs have been processed into u (east-west) and v (north-south) components.</p>
<p>These datasets contain the results from the deployment of bottom-mounted acoustic Doppler current profilers to measure depth-stratified currents at a number of locations in Kimbe Bay.&nbsp; Variables as follows:&nbsp; site name; lat; lon; time (serial date); u (cm/sec); v (cm/sec).</p>
Specified by the Principal Investigator(s)
asNeeded
7.x-1.1
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
Bottom-mounted ADCP
Bottom-mounted ADCP
PI Supplied Instrument Name: Bottom-mounted ADCP PI Supplied Instrument Description:Standard bottom-mounted (i.e. looking up) ADCPs were deployed at locations in Kimbe Bay. Instrument Name: Acoustic Doppler Current Profiler Instrument Short Name:ADCP Instrument Description: The ADCP measures water currents with sound, using a principle of sound waves called the Doppler effect. A sound wave has a higher frequency, or pitch, when it moves to you than when it moves away. You hear the Doppler effect in action when a car speeds past with a characteristic building of sound that fades when the car passes. The ADCP works by transmitting "pings" of sound at a constant frequency into the water. (The pings are so highly pitched that humans and even dolphins can't hear them.) As the sound waves travel, they ricochet off particles suspended in the moving water, and reflect back to the instrument. Due to the Doppler effect, sound waves bounced back from a particle moving away from the profiler have a slightly lowered frequency when they return. Particles moving toward the instrument send back higher frequency waves. The difference in frequency between the waves the profiler sends out and the waves it receives is called the Doppler shift. The instrument uses this shift to calculate how fast the particle and the water around it are moving. Sound waves that hit particles far from the profiler take longer to come back than waves that strike close by. By measuring the time it takes for the waves to bounce back and the Doppler shift, the profiler can measure current speed at many different depths with each series of pings. (More from WHOI instruments listing). Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/115/
Deployment: Thorrold_ADCP_Kimbe
Thorrold_ADCP_Kimbe
Kimbe Bay
shoreside
Thorrold_ADCP_Kimbe
Simon Thorrold
Woods Hole Oceanographic Institution
Kimbe Bay
shoreside