Contributors | Affiliation | Role |
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Edmunds, Peter J. | California State University Northridge (CSUN) | Principal Investigator |
Copley, Nancy | Woods Hole Oceanographic Institution (WHOI BCO-DMO) | BCO-DMO Data Manager |
Taken from publication in PeerJ
The study focused on Gorgonia ventalina at Yawzi Point and Tektite within Great Lameshur Bay, and the research was completed under permits issued by the Virgin Islands National Park. These reefs have been monitored from 1987 to present, and the present analysis was superimposed on the same study areas. At each site, three permanent transects were installed in 1987, with each ~ 10 m long, parallel to one another, and ~ 5 m apart. Contiguous photoquadrats (1 × 1 m) have been recorded along each transect to quantify the cover of benthic taxa.
Starting in August 2013, colonies of G. ventalina ± 1 m of each transect were surveyed, with their sizes recorded as height. Each colony was mapped through Cartesian coordinates along each transect, and their height was recorded using a flexible tape measure (± 0.5 cm) as the linear distance from the holdfast to the highest distal portion of living tissue. Fans that were symmetrical or slightly imperfect in shape with small areas of mortality were easily measured, but fans that were torn and were affected by partial mortality (i.e., categorized as "ragged" fans) posed challenges for measurement. The size of ragged fans was recorded as their greatest height, which overestimated their size relative to the amount of G. ventalina tissue. Field logistics prevented finer resolution of tissue area (e.g., through photography, but separate analyses of photoquadrats were used to evaluate the abundance of ragged colonies in each year.
The surveys of G. ventalina were repeated annually in August from 2013 to 2019, and on each occasion colonies were mapped and their sizes recorded as above. Sizes and Cartesian coordinates were compared between consecutive years to identify colonies that were evaluated in both years, colonies that had died between years (lost from the reef or reduced to a horny axis without tissue), or small colonies that recruited between years.
Analyses
Mean densities of G. ventalina were compared among times using repeated measures ANOVA in which transects were repeatedly surveyed over time; a non-parametric Friedman test was used when statistical assumptions were not met. Mean colony sizes were compared over time using one-way ANOVA in which each colony was a replicate. The density of G. ventalina recruits was evaluated from colonies = 5 cm tall, and their densities and heights were compared over time as described above. Colonies were considered to have left the recruiting size class when they were > 5 cm tall. The percentage distribution of colonies among sizes classes over time was evaluated using size (height) classes of 10 cm, with the largest class including colonies between 60 and 100 cm tall. The distribution of colonies among size classes was tested for variation among years using chi-squared contingency tables. Growth was recorded as the change in height between consecutive years for colonies that were located in both years, and growth was compared over time using non-parametric Kruskal-Wallis (three or more groups) or Mann-Whitney U-Tests (two groups).
Density-associated effects were explored through analyses of the relationships between mean height and mean density for self-thinning, and between mean density of recruits and mean density of colonies > 5 cm tall, using transects as statistical replicates. Evidence for self-thinning would be revealed by an inverse relationship size and density, and a slope of the log size versus log density relationship of ~ 1.5. Evidence of density-associated recruitment would be revealed by a linear relationship between the density of recruits and larger colonies, and a linear relationship (either positive or negative) between per-capita recruitment and density of colonies > 5 cm tall. Per capita recruitment was calculated by dividing the density of recruits by the density of colonies > 5 cm tall.
BCO-DMO Processing Notes:
- data extracted to .csv from file "Edmunds - Gorgonia paper - sent to bco-dmo.zip/Data in Gorgonia Paper_21_Oct copy.xlsx", sheet "Growth".
- added conventional header with dataset name, PI name, version date
- modified parameter names to conform with BCO-DMO naming conventions
- joined the original table with latitude and longitude positions
File |
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Gorgonia_growth.csv (Comma Separated Values (.csv), 19.42 KB) MD5:2958764ab452136821cf860515de8e01 Primary data file for dataset ID 827897 |
Parameter | Description | Units |
site | Yawzi Point (9m depth) or Tektite (14 m depth) | unitless |
lat | latitude; north is positive | decimal degrees |
lon | longitude; east is positive | decimal degrees |
depth | water depth at site | meters |
Period | year-long period over which growth was measured | unitless |
height_initial | height at the start of the period | millimeters (mm) |
height_final | height at the end of the period | millimeters (mm) |
Dataset-specific Instrument Name | Optic Stowaway loggers and Hobo Aquapro loggers |
Generic Instrument Name | Temperature Logger |
Dataset-specific Description | Used to collect seawater temperature. |
Generic Instrument Description | Records temperature data over a period of time. |
Dataset-specific Instrument Name | Ryan Industries thermistor |
Generic Instrument Name | Thermistor |
Dataset-specific Description | Used to collect seawater temperature. |
Generic Instrument Description | A thermistor is a type of resistor whose resistance varies significantly with temperature, more so than in standard resistors. The word is a portmanteau of thermal and resistor. Thermistors are widely used as inrush current limiters, temperature sensors, self-resetting overcurrent protectors, and self-regulating heating elements.
Thermistors differ from resistance temperature detectors (RTD) in that the material used in a thermistor is generally a ceramic or polymer, while RTDs use pure metals. The temperature response is also different; RTDs are useful over larger temperature ranges, while thermistors typically achieve a higher precision within a limited temperature range, typically 90C to 130C. |
Describing how ecosystems like coral reefs are changing is at the forefront of efforts to evaluate the biological consequences of global climate change and ocean acidification. Coral reefs have become the poster child of these efforts. Amid concern that they could become ecologically extinct within a century, describing what has been lost, what is left, and what is at risk, is of paramount importance. This project exploits an unrivalled legacy of information beginning in 1987 to evaluate the form in which reefs will persist, and the extent to which they will be able to resist further onslaughts of environmental challenges. This long-term project continues a 27-year study of Caribbean coral reefs. The diverse data collected will allow the investigators to determine the roles of local and global disturbances in reef degradation. The data will also reveal the structure and function of reefs in a future with more human disturbances, when corals may no longer dominate tropical reefs.
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Funding Source | Award |
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NSF Division of Environmental Biology (NSF DEB) | |
NSF Division of Ocean Sciences (NSF OCE) |