Abondance index variation and North Atlantic Oscillation Index

We tested for statistical associations among several combinations of the NAO time series and temporal fluctuations of three variables used as proxies of relative abundance. Variation in Nb was used as a proxy for relative variation in the number of breeders. Allelic richness (Ar), measured for each...

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Main Authors: Côté, Caroline, Castonguay, Martin, Gagnaire, Pierre-Alexandre, Bourret, Vincent, Verreault, Guy, Bernatchez, Louis
Format: Report
Language:unknown
Published: 2012
Subjects:
Online Access:http://hdl.handle.net/10255/dryad.42543
https://doi.org/10.5061/dryad.39jb0/2
id ftdryad:oai:v1.datadryad.org:10255/dryad.42543
record_format openpolar
spelling ftdryad:oai:v1.datadryad.org:10255/dryad.42543 2023-05-15T17:22:26+02:00 Abondance index variation and North Atlantic Oscillation Index Côté, Caroline Castonguay, Martin Gagnaire, Pierre-Alexandre Bourret, Vincent Verreault, Guy Bernatchez, Louis Florida 30.02N -81.33W Guana River Dam Georgia 31.31N -81.47W Mornings-AR South Carolina 32.93N -80.01W Cooper River North Carolina 34.77N -76.81W Black Creek Virginia 37.22N -76.49W Wormley Creek York Delaware 38.59N -75.29W Millsboro Pond Spillway New Jersey 39.56N -74.58W Patcong Creak Linwood Pennsylvania 40.05N -74.98W Crum Creek Connecticut 41.30N -72.40W Tyler River Massachusetts 41.68N -70.92W Parker River New Hampshire 42.93N -70.86W Tayler River Nova Scotia 44.59N -64.17W Mira River Newfoundland 47.84N -59.26W Codroy River Québec 48.78N -67.69W Grande Rivière Blanche Prince Edward Island 46.43N -63.24W Rustico Bay Ontario 45.01N -74.79W Moses-Saunders Dam Québec 45.31N -73.90W Beauharnois Dam Québec 45.44N -73.26W Chambly Dam Québec 48.28N -68.95W Rivière du Sud-Ouest Québec 49.52N -67.28W Rivière de la Petite Trinité Québec 48.82N -64.83W Rivière Saint-Jean Maine 43.84N -69.65W West Harbor Pond New Brunswick 47.52N -64.91W Tracadie River New Brunswick 47.09N -65.22W Miramichi Estuary New Brunswick 45.87N -66.15W Grand-Lake Nova Scotia 44.36N -64.46W La Have River Nova Scotia 45.84N -60.80W Bras d’Or Lake Nova Scotia 46.43N -61.10W Margaree Harbour Newfoundland 47.60N -53.26W Roberts Bay Mesozoic 2012-10-25T17:48:52Z http://hdl.handle.net/10255/dryad.42543 https://doi.org/10.5061/dryad.39jb0/2 unknown doi:10.5061/dryad.39jb0 doi:10.5061/dryad.39jb0/2 http://hdl.handle.net/10255/dryad.42543 http://creativecommons.org/publicdomain/zero/1.0/ CC0 PDM Conservation Biology Conservation Genetics Ecological Genetics Fisheries Management Population Genetics - Empirical Wildlife Management Dataset untilArticleAppears 2012 ftdryad https://doi.org/10.5061/dryad.39jb0/2 https://doi.org/10.5061/dryad.39jb0 2020-01-01T14:57:58Z We tested for statistical associations among several combinations of the NAO time series and temporal fluctuations of three variables used as proxies of relative abundance. Variation in Nb was used as a proxy for relative variation in the number of breeders. Allelic richness (Ar), measured for each cohort, was used as a proxy for the relative abundance of recruits since it has previously been proposed to correlate with offspring recruitment (McCusker & Bentzen 2010). YCSI was used as a second proxy of recruit abundance. We first tested for pairwise correlations between Nb, Ar, and YCSI, and time series of these three parameters were then compared with the monthly normalized NAO (http://www.cgd.ucar.edu). The “corresponding year” between time series represented the year when glass eels reached the continent for the Ar, Nb, and YCSI time series. To test environmental influence on previous life stages, +2 to -2 year lags were also tested. To assess the statistical significance of climate influence on eel abundance, multivariate models were run where the explanatory variables considered were the NAO time series. Stepwise regressions of the three relative abundance variables (Nb, Ar, and YCSI) were fitted to the explanatory variables to determine which ones were significant. The Akaike Information Criterion (AIC) was used to select models. Cross-validation R2 was computed to determine the prediction strength of the selected model and semi-partial R2 were computed to assess the relative importance of each selected variable. Analyses were performed using SAS 9.2 software. Report Newfoundland North Atlantic North Atlantic oscillation Prince Edward Island Dryad Digital Repository (Duke University) Blanche ENVELOPE(140.018,140.018,-66.663,-66.663) Creak ENVELOPE(162.150,162.150,-76.600,-76.600) Mira ENVELOPE(10.500,10.500,-70.417,-70.417) Moses ENVELOPE(-99.183,-99.183,-74.550,-74.550) Rivière du Sud ENVELOPE(70.132,70.132,-49.346,-49.346) Roberts Bay ENVELOPE(-99.064,-99.064,57.290,57.290) Saunders ENVELOPE(-45.316,-45.316,-60.700,-60.700)
institution Open Polar
collection Dryad Digital Repository (Duke University)
op_collection_id ftdryad
language unknown
topic Conservation Biology
Conservation Genetics
Ecological Genetics
Fisheries Management
Population Genetics - Empirical
Wildlife Management
spellingShingle Conservation Biology
Conservation Genetics
Ecological Genetics
Fisheries Management
Population Genetics - Empirical
Wildlife Management
Côté, Caroline
Castonguay, Martin
Gagnaire, Pierre-Alexandre
Bourret, Vincent
Verreault, Guy
Bernatchez, Louis
Abondance index variation and North Atlantic Oscillation Index
topic_facet Conservation Biology
Conservation Genetics
Ecological Genetics
Fisheries Management
Population Genetics - Empirical
Wildlife Management
description We tested for statistical associations among several combinations of the NAO time series and temporal fluctuations of three variables used as proxies of relative abundance. Variation in Nb was used as a proxy for relative variation in the number of breeders. Allelic richness (Ar), measured for each cohort, was used as a proxy for the relative abundance of recruits since it has previously been proposed to correlate with offspring recruitment (McCusker & Bentzen 2010). YCSI was used as a second proxy of recruit abundance. We first tested for pairwise correlations between Nb, Ar, and YCSI, and time series of these three parameters were then compared with the monthly normalized NAO (http://www.cgd.ucar.edu). The “corresponding year” between time series represented the year when glass eels reached the continent for the Ar, Nb, and YCSI time series. To test environmental influence on previous life stages, +2 to -2 year lags were also tested. To assess the statistical significance of climate influence on eel abundance, multivariate models were run where the explanatory variables considered were the NAO time series. Stepwise regressions of the three relative abundance variables (Nb, Ar, and YCSI) were fitted to the explanatory variables to determine which ones were significant. The Akaike Information Criterion (AIC) was used to select models. Cross-validation R2 was computed to determine the prediction strength of the selected model and semi-partial R2 were computed to assess the relative importance of each selected variable. Analyses were performed using SAS 9.2 software.
format Report
author Côté, Caroline
Castonguay, Martin
Gagnaire, Pierre-Alexandre
Bourret, Vincent
Verreault, Guy
Bernatchez, Louis
author_facet Côté, Caroline
Castonguay, Martin
Gagnaire, Pierre-Alexandre
Bourret, Vincent
Verreault, Guy
Bernatchez, Louis
author_sort Côté, Caroline
title Abondance index variation and North Atlantic Oscillation Index
title_short Abondance index variation and North Atlantic Oscillation Index
title_full Abondance index variation and North Atlantic Oscillation Index
title_fullStr Abondance index variation and North Atlantic Oscillation Index
title_full_unstemmed Abondance index variation and North Atlantic Oscillation Index
title_sort abondance index variation and north atlantic oscillation index
publishDate 2012
url http://hdl.handle.net/10255/dryad.42543
https://doi.org/10.5061/dryad.39jb0/2
op_coverage Florida 30.02N -81.33W Guana River Dam
Georgia 31.31N -81.47W Mornings-AR
South Carolina 32.93N -80.01W Cooper River
North Carolina 34.77N -76.81W Black Creek
Virginia 37.22N -76.49W Wormley Creek York
Delaware 38.59N -75.29W Millsboro Pond Spillway
New Jersey 39.56N -74.58W Patcong Creak Linwood
Pennsylvania 40.05N -74.98W Crum Creek
Connecticut 41.30N -72.40W Tyler River
Massachusetts 41.68N -70.92W Parker River
New Hampshire 42.93N -70.86W Tayler River
Nova Scotia 44.59N -64.17W Mira River
Newfoundland 47.84N -59.26W Codroy River
Québec 48.78N -67.69W Grande Rivière Blanche
Prince Edward Island 46.43N -63.24W Rustico Bay
Ontario 45.01N -74.79W Moses-Saunders Dam
Québec 45.31N -73.90W Beauharnois Dam
Québec 45.44N -73.26W Chambly Dam
Québec 48.28N -68.95W Rivière du Sud-Ouest
Québec 49.52N -67.28W Rivière de la Petite Trinité
Québec 48.82N -64.83W Rivière Saint-Jean
Maine 43.84N -69.65W West Harbor Pond
New Brunswick 47.52N -64.91W Tracadie River
New Brunswick 47.09N -65.22W Miramichi Estuary
New Brunswick 45.87N -66.15W Grand-Lake
Nova Scotia 44.36N -64.46W La Have River
Nova Scotia 45.84N -60.80W Bras d’Or Lake
Nova Scotia 46.43N -61.10W Margaree Harbour
Newfoundland 47.60N -53.26W Roberts Bay
Mesozoic
long_lat ENVELOPE(140.018,140.018,-66.663,-66.663)
ENVELOPE(162.150,162.150,-76.600,-76.600)
ENVELOPE(10.500,10.500,-70.417,-70.417)
ENVELOPE(-99.183,-99.183,-74.550,-74.550)
ENVELOPE(70.132,70.132,-49.346,-49.346)
ENVELOPE(-99.064,-99.064,57.290,57.290)
ENVELOPE(-45.316,-45.316,-60.700,-60.700)
geographic Blanche
Creak
Mira
Moses
Rivière du Sud
Roberts Bay
Saunders
geographic_facet Blanche
Creak
Mira
Moses
Rivière du Sud
Roberts Bay
Saunders
genre Newfoundland
North Atlantic
North Atlantic oscillation
Prince Edward Island
genre_facet Newfoundland
North Atlantic
North Atlantic oscillation
Prince Edward Island
op_relation doi:10.5061/dryad.39jb0
doi:10.5061/dryad.39jb0/2
http://hdl.handle.net/10255/dryad.42543
op_rights http://creativecommons.org/publicdomain/zero/1.0/
op_rightsnorm CC0
PDM
op_doi https://doi.org/10.5061/dryad.39jb0/2
https://doi.org/10.5061/dryad.39jb0
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