|van Woesik, Robert||Florida Institute of Technology (FIT)||Principal Investigator, Contact|
|York, Amber D.||Woods Hole Oceanographic Institution (WHOI BCO-DMO)||BCO-DMO Data Manager|
These data were published in van Woesik & Cacciapaglia (2018) and van Woesik & Cacciapaglia (2019).
Field data were collected at the site list locations in Palau (June 2nd to 24th, 2017), Yap (June 25th to July 6th, 2017), the Federated States of Micronesia (FSM) (2018), and Kiritimati and Majuro (2019). The maximum length of each fish species was taken from the literature and the maximum size of each fish was estimated from our field surveys. The scar proportion and bite volume was estimated using the maximum size of the fish species. Professor Peter Mumby provided bite conversion values.
BCO-DMO Data Manager Processing Notes:
- This dataset was originally submitted to BCO-DMO as files;
- removed trailing and leading spaces;
- added a conventional header with dataset name, PI name, version date;
- modified parameter names to conform with BCO-DMO naming conventions;
- Added "ScientificName" which combines Genus and Species columns;
- Species names changed to accepted name after using World Register of Marine Species taxa match tool and communication with PI:
Bulbometopon muricatum to Bolbometopon muricatum
Scarus prasiognathus to Scarus prasiognathos
Scarus psitticus to Scarus psittacus
Scarus spinos to Scarus spinus
Scarus japenensis to Chlorurus japanensis
|bite_volume_constant||Constant to scale-bite volume based on size of individual fish||unitless|
|scar_proportion||Probability of scarring coral in a bite (number of scars/bites)||unitless|
|bite_conv_val||Constant of scale-bite rate and size of fish species relative to erosion impact||unitless|
|max_length||The size of largest individual fish of that species||centimeters (cm)|
|max_bite_volume||Volume of coral that the largest sized individual fish could remove in a single bite||centimeters cubed (cm^3)|
|Start Date|| |
|End Date|| |
|Start Date|| |
|End Date|| |
|Start Date|| |
NSF Award Abstract:
Increases in ocean temperatures and sea-level rise are threatening coral reef ecosystems worldwide. Indeed, some island nations are no more than 1 m above modern sea level. Yet, building sea walls on tropical coasts, to keep out the ocean, as they do in the Netherlands, is a substantial economic burden on small-island nations. Healthy coral reefs, however, have the capacity to lay down sufficient calcium carbonate to grow vertically and keep up with sea-level rise, as they did in the geological past. By contrast, damaged coral reefs do not have the capacity to keep up with sea-level rise, making the coastal communities vulnerable, and inflicting a large economic burden on the coastal societies to build sea walls. In addition, and very recently, coral reefs are being subjected to high water temperatures that are causing considerable damage to corals. This study will ask some critical questions: Are coral reefs in the western Pacific Ocean keeping up with sea-level rise? Where are reefs keeping up with sea-level rise, and what is preventing reefs in some localities from keeping up? This study will also examine whether geographical differences in ocean temperatures influence the capacity of reefs to keep up with sea-level rise. Where coral reefs cannot keep up with sea-level rise, these natural storm barriers will disappear, resulting in the loss of habitable land for millions of people worldwide. The broader impacts of the study will focus on training a post-doctoral researcher, and developing and running one-week training workshops in the proposed study locations in Palau, Yap, Chuuk, Pohnpei, Kosrae, Majuro, and Kiribati. The investigators will work with local stakeholders on the various islands, focusing on connecting science to management practices to reduce local stressors to coral reefs.
Coral reefs are one of the world's most diverse and valuable marine ecosystems. Since the mid-Holocene, some 5000 years ago, coral reefs in the Pacific Ocean have been vertically constrained by sea level. Contemporary sea-level rise is releasing these constraints, providing accommodation space for vertical reef expansion. Yet recently corals have been repeatedly subjected to thermal-stress events, and we know little about whether modern coral reefs can "keep up" with projected future sea-level rise as the ocean temperatures continue to increase. This study will examine whether and where coral reefs are keeping up with sea-level rise across a temperature gradient in the Pacific Ocean, from Palau in the west to Kiribati in the east. The spatial differences in the capacity to keep up with sea level will be explored, and it is hypothesized that differential rates of coral growth and capacity to keep up with sea-level rise will be a function of regional temperatures, local water-flow rates, and land-use. One of the major tasks of this study is to determine the contribution of the various components of each reef to potential carbonate production, across the geographical temperature gradient. The investigators will quantify the rates of carbonate production, by corals and calcareous algae, and the rates of carbonate destruction, by reef eroders, by measuring the space occupied by each benthic component at each study site. The team will then sum that information to interpret the overall capacity of the reef to produce carbonate. At each study site mobile benthic eroders will be estimated, as counts and size measurements of echinoids and herbivorous fishes. The investigators will measure the densities of the different coral species, from different habitats, and develop models that relate the coral morphologies with the potential rate of carbonate deposition. This study will assess the contribution of sea surface temperature, flow rates, and land-use practice to the capacity of reefs to keep up with sea-level rise. Two different approaches will be used to predict the relationship between carbonate production and sea-level rise. The first model will assume that the capacity of vertical reef accretion is directly related to the extension of Porites microatolls at the various island locations. The second model will take a hierarchical Bayesian approach to examine reef growth, which depends on the presence and density of calcifying organisms, and on physical, chemical, and biological erosional processes.