Contributors | Affiliation | Role |
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Lasker, Howard | State University of New York at Buffalo (SUNY Buffalo) | Principal Investigator |
Tonra, Kaitlyn | State University of New York at Buffalo (SUNY Buffalo) | Scientist, Contact |
Wells, Christopher | State University of New York at Buffalo (SUNY Buffalo) | Scientist |
Anderson, Emily | State University of New York at Buffalo (SUNY Buffalo) | Technician |
York, Amber D. | Woods Hole Oceanographic Institution (WHOI BCO-DMO) | BCO-DMO Data Manager |
Methodology:
Eleven female and four male branches of Plexaura homomalla were collected from adult colonies on an octocoral-dominated reef in Round Bay, St. John, USVI on July 14–15, 2019. All branches were about 15 cm long. Colonies were determined to be gravid in the field by cutting a 5-cm piece diagonally and looking for spermaries or eggs. Colonies were transported to the Virgin Islands Environmental Research Station and maintained in a sea table.
We monitored for signs of spawning for 5 hr starting at sunset starting one night after the full moon from July 17–23, 2019. Eggs and sperm were collected together with 60- mL syringes as they were released from the colonies and were stored in water from the tank for 30 min to ensure fertilization. We refer to the time at which gametes were collected as t = 0. On the second night of spawning, 100 eggs were placed in an isolated container and the number of cells was counted in triplicate by two different observers. Counts were taken every 0.5 hr from 2.5 to 7 hr after fertilization, hourly until 10 h after fertilization, and at 15, 18, and 24 hr after fertilization.
Instruments:
dissecting microscope, hand lens
BCO-DMO data manager processing notes:
* Data from file NSF.Phomomalla_development_coarse_monitoring.xlsx sheet "data" imported into the BCO-DMO data system.
* Added column ISO_DateTime_UTC_Start from times and dates provided in local time UTC-4.
File |
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p_homomalla_dev_coarse.csv (Comma Separated Values (.csv), 3.12 KB) MD5:b69f6a0dd09c2a71dbba3b05de2e92fa Primary data file for dataset ID 855766 |
Parameter | Description | Units |
container | monitoring dish containing the eggs (either A or B). after hour 7, containers A and B were split to ease tracking of developing eggs (A1 and A2 or B1 and B2) | unitless |
start_time | start time of that counting period in format HH:MM (in Atlantic Standard time zone, UTC-4) | unitless |
end_time | end time for that counting period in format HH:MM (in Atlantic Standard time zone, UTC-4) | unitless |
time | time relative to the average time corals were spawning and eggs were fertilized (i.e., 22:08) in hours | unitless |
date | date of observation (Altantic Standard Time, UTC-4) | unitless |
cell_1 | number of eggs/embryos that were 1 cell | unitless |
cell_2 | number embryos that were 2 cells | unitless |
cell_4 | number embryos that were 4 cells | unitless |
cell_8 | number embryos that were 8 cells | unitless |
cell_16 | number embryos that were 16 cells | unitless |
cell_32 | number embryos that were 32 cells | unitless |
cell_64 | number embryos that were 64 or more cells | unitless |
total | total number of eggs/embryos | unitless |
ISO_DateTime_UTC_Start | start Datetime of that counting period in ISO 8601 format yyyy-mm-ddTHH:MMZ (UTC). | unitless |
NSF Award Abstract:
Coral reefs are exposed to a diversity of natural and anthropogenic disturbances, and the consequences for ecosystem degradation have been widely publicized. However, the reported changes have been biased towards fishes and stony corals, and for Caribbean reefs, the most notable example of this bias are octocorals ("soft corals"). Although they are abundant and dominate many Caribbean reefs, they are rarely included in studies due to the difficulty of both identifying them and in quantifying their abundances. In some places there is compelling evidence that soft corals have increased in abundance, even while stony corals have become less common. This suggests that soft corals are more resilient than stony corals to the wide diversity of disturbances that have been impacting coral corals. The best coral reefs on which to study these changes are those that have been studied for decades and can provide a decadal context to more recent events, and in this regard the reefs of St. John, US Virgin Islands are unique. Stony corals on the reefs have been studied since 1987, and the soft corals from 2014. This provides unrivalled platform to evaluate patterns of octocoral abundance and recruitment; identify the patterns of change that are occurring on these reefs, and identify the processes responsible for the resilience of octocoral populations. The project will extend soft coral monitoring from 4 years to 8 years, and within this framework will examine the roles of baby corals, and their response to seafloor roughness, seawater flow, and seaweed, in determining the success of soft corals. The work will also assess whether the destructive effects of Hurricanes Irma and Maria have modified the pattern of change. In concert with these efforts the project will be closely integrated with local high schools at which the investigators will host marine biology clubs and provide independent study opportunities for their students and teachers. Unique training opportunities will be provided to undergraduate and graduate students, as well as a postdoctoral researcher, all of whom will study and work in St. John, and the investigators will train coral reef researchers to identify the species of soft corals through a hands-on workshop to be conducted in the Florida Keys.
Understanding how changing environmental conditions will affect the community structure of major biomes is the ecological objective defining the 21st century. The holistic effects of these conditions on coral reefs will be studied on shallow reefs within the Virgin Islands National Park in St. John, US Virgin Islands, which is the site of one of the longest-running, long-term studies of coral reef community dynamics in the region. With NSF-LTREB support, the investigators have been studying long-term changes in stony coral communities in this location since 1987, and in 2014 NSF-OCE support was used to build an octocoral "overlay" to this decadal perspective. The present project extends from this unique history, which has been punctuated by the effects of Hurricanes Irma and Maria, to place octocoral synecology in a decadal context, and the investigators exploit a rich suite of legacy data to better understand the present and immediate future of Caribbean coral reefs. This four-year project will advance on two concurrent fronts: first, to extend time-series analyses of octocoral communities from four to eight years to characterize the pattern and pace of change in community structure, and second, to conduct a program of hypothesis-driven experiments focused on octocoral settlement that will uncover the mechanisms allowing octocorals to more effectively colonize substrata than scleractinian corals on present day reefs. Specifically, the investigators will conduct mensurative and manipulative experiments addressing four hypotheses focusing on the roles of: (1) habitat complexity in distinguishing between octocoral and scleractinian recruitment niches, (2) the recruitment niche in mediating post-settlement success, (3) competition in algal turf and macroalgae in determining the success of octocoral and scleractian recruits, and (4) role of octocoral canopies in modulating the flux of particles and larvae to the seafloor beneath. The results of this study will be integrated to evaluate the factors driving higher ecological resilience of octocorals versus scleractinians on present-day Caribbean reefs.
This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.
Funding Source | Award |
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NSF Division of Ocean Sciences (NSF OCE) |