Data for: Disturbance, dispersal and marine assemblage structure: a case study from the nearshore Southern Ocean
Benthic assemblage structure data was collected form the IceBerg Impact Study grids located in South Cove, Ryder Bay, Adeliade Island, Western Antarctic Peninsula. Recovery Age includes only the sample grid itself and records the number of years since it was last hit. Local Disturbance includes all...
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ftdatacite:10.17632/yd698b9d43.1 2023-05-15T13:48:27+02:00 Data for: Disturbance, dispersal and marine assemblage structure: a case study from the nearshore Southern Ocean Robinson, Ben 2020 https://dx.doi.org/10.17632/yd698b9d43.1 https://data.mendeley.com/datasets/yd698b9d43/1 unknown Mendeley https://dx.doi.org/10.17632/yd698b9d43 https://dx.doi.org/10.1016/j.marenvres.2020.105025 Creative Commons Attribution 4.0 International info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Antarctica Benthic Community Disturbance Ecology Macrofauna Iceberg dataset Dataset 2020 ftdatacite https://doi.org/10.17632/yd698b9d43.1 https://doi.org/10.17632/yd698b9d43 https://doi.org/10.1016/j.marenvres.2020.105025 2021-11-05T12:55:41Z Benthic assemblage structure data was collected form the IceBerg Impact Study grids located in South Cove, Ryder Bay, Adeliade Island, Western Antarctic Peninsula. Recovery Age includes only the sample grid itself and records the number of years since it was last hit. Local Disturbance includes all adjacent squares and the sample square with the proportion that had been hit in the past year recorded. Background Disturbance includes all the squares within the grid and the sample grid square and the rate at which hits have been recorded over the past 7 years. The high-dispersal assemblage diversity and abundance was collected across all samples at a single point in time. Whereas the low-dispersal assemblage is a dataset compiled from 7 years of observations with the presence and absence of each species. The Low-dispersal encrusting assemblages (bryozoans) was sampled from 2009 to 2014.Images of the high-dispersal assemblages within each grid square were captured in January 2016 with a GoPro 3+ (GoPro Inc.) in a deepwater housing. Camera lens distortion (fish-eye) was minimised using a calibration lens file and Hugins photo editing software. Grid squares were selected to ensure replication across depth, age and disturbance regimes. Dataset Antarc* Antarctic Antarctic Peninsula Antarctica Iceberg* Southern Ocean DataCite Metadata Store (German National Library of Science and Technology) Antarctic Antarctic Peninsula Ryder ENVELOPE(-68.333,-68.333,-67.566,-67.566) Ryder Bay ENVELOPE(-68.333,-68.333,-67.567,-67.567) South Cove ENVELOPE(-56.115,-56.115,50.050,50.050) Southern Ocean |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
topic |
Antarctica Benthic Community Disturbance Ecology Macrofauna Iceberg |
spellingShingle |
Antarctica Benthic Community Disturbance Ecology Macrofauna Iceberg Robinson, Ben Data for: Disturbance, dispersal and marine assemblage structure: a case study from the nearshore Southern Ocean |
topic_facet |
Antarctica Benthic Community Disturbance Ecology Macrofauna Iceberg |
description |
Benthic assemblage structure data was collected form the IceBerg Impact Study grids located in South Cove, Ryder Bay, Adeliade Island, Western Antarctic Peninsula. Recovery Age includes only the sample grid itself and records the number of years since it was last hit. Local Disturbance includes all adjacent squares and the sample square with the proportion that had been hit in the past year recorded. Background Disturbance includes all the squares within the grid and the sample grid square and the rate at which hits have been recorded over the past 7 years. The high-dispersal assemblage diversity and abundance was collected across all samples at a single point in time. Whereas the low-dispersal assemblage is a dataset compiled from 7 years of observations with the presence and absence of each species. The Low-dispersal encrusting assemblages (bryozoans) was sampled from 2009 to 2014.Images of the high-dispersal assemblages within each grid square were captured in January 2016 with a GoPro 3+ (GoPro Inc.) in a deepwater housing. Camera lens distortion (fish-eye) was minimised using a calibration lens file and Hugins photo editing software. Grid squares were selected to ensure replication across depth, age and disturbance regimes. |
format |
Dataset |
author |
Robinson, Ben |
author_facet |
Robinson, Ben |
author_sort |
Robinson, Ben |
title |
Data for: Disturbance, dispersal and marine assemblage structure: a case study from the nearshore Southern Ocean |
title_short |
Data for: Disturbance, dispersal and marine assemblage structure: a case study from the nearshore Southern Ocean |
title_full |
Data for: Disturbance, dispersal and marine assemblage structure: a case study from the nearshore Southern Ocean |
title_fullStr |
Data for: Disturbance, dispersal and marine assemblage structure: a case study from the nearshore Southern Ocean |
title_full_unstemmed |
Data for: Disturbance, dispersal and marine assemblage structure: a case study from the nearshore Southern Ocean |
title_sort |
data for: disturbance, dispersal and marine assemblage structure: a case study from the nearshore southern ocean |
publisher |
Mendeley |
publishDate |
2020 |
url |
https://dx.doi.org/10.17632/yd698b9d43.1 https://data.mendeley.com/datasets/yd698b9d43/1 |
long_lat |
ENVELOPE(-68.333,-68.333,-67.566,-67.566) ENVELOPE(-68.333,-68.333,-67.567,-67.567) ENVELOPE(-56.115,-56.115,50.050,50.050) |
geographic |
Antarctic Antarctic Peninsula Ryder Ryder Bay South Cove Southern Ocean |
geographic_facet |
Antarctic Antarctic Peninsula Ryder Ryder Bay South Cove Southern Ocean |
genre |
Antarc* Antarctic Antarctic Peninsula Antarctica Iceberg* Southern Ocean |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Antarctica Iceberg* Southern Ocean |
op_relation |
https://dx.doi.org/10.17632/yd698b9d43 https://dx.doi.org/10.1016/j.marenvres.2020.105025 |
op_rights |
Creative Commons Attribution 4.0 International info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.17632/yd698b9d43.1 https://doi.org/10.17632/yd698b9d43 https://doi.org/10.1016/j.marenvres.2020.105025 |
_version_ |
1766249295068004352 |