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Medellín-Maldonado F, Cruz-Ortega I, Pérez-Cervantes E, Norzogaray-López O, Carricart-Ganivet JP, López-Pérez A, Alvarez-Filip L. Newly deceased Caribbean reef-building corals experience rapid carbonate loss and colonization by endolithic organisms. Commun Biol 2023; 6:934. [PMID: 37699971 PMCID: PMC10497637 DOI: 10.1038/s42003-023-05301-3] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/27/2022] [Accepted: 08/29/2023] [Indexed: 09/14/2023] Open
Abstract
Coral mortality triggers the loss of carbonates fixed within coral skeletons, compromising the reef matrix. Here, we estimate rates of carbonate loss in newly deceased colonies of four Caribbean reef-building corals. We use samples from living and recently deceased colonies following a stony coral tissue loss disease (SCTLD) outbreak. Optical densitometry and porosity analyses reveal a loss of up to 40% of the calcium carbonate (CaCO3) content in dead colonies. The metabolic activity of the endolithic organisms colonizing the dead skeletons is likely partially responsible for the observed dissolution. To test for the consequences of mass mortality events over larger spatial scales, we integrate our estimates of carbonate loss with field data of the composition and size structure of coral communities. The dissolution rate depends on the relative abundance of coral species and the structural properties of their skeletons, yet we estimate an average reduction of 1.33 kg CaCO3 m-2, nearly 7% of the total amount of CaCO3 sequestered in the entire system. Our findings highlight the importance of including biological and chemical processes of CaCO3 dissolution in reef carbonate budgets, particularly as the impacts of global warming, ocean acidification, and disease likely enhance dissolution processes.
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Affiliation(s)
- Francisco Medellín-Maldonado
- Posgrado en Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México, Av. Ciudad Universitaria 3000, Coyoacán, 04510, Ciudad de México, Mexico.
- Biodiversity and Reef Conservation Laboratory, Unidad Académica de Sistemas Arrecifales en Puerto Morelos, ICML, UNAM, 77580, Puerto Morelos, Mexico.
- Laboratorio de Arrecifes y Biodiversidad, Universidad Autónoma Metropolitana, 09340, Ciudad de México, Mexico.
| | - Israel Cruz-Ortega
- Laboratorio de Esclerocronología de Corales Arrecifales, Unidad Académica de Sistemas Arrecifales en Puerto Morelos, ICML, UNAM, 77580, Puerto Morelos, Mexico
| | - Esmeralda Pérez-Cervantes
- Posgrado en Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México, Av. Ciudad Universitaria 3000, Coyoacán, 04510, Ciudad de México, Mexico
| | - Orion Norzogaray-López
- Instituto de Investigaciones Oceanológicas y Facultad de Ciencias Marinas, Universidad Autónoma de Baja California, 22860, Ensenada, BC, Mexico
| | - Juan P Carricart-Ganivet
- Laboratorio de Esclerocronología de Corales Arrecifales, Unidad Académica de Sistemas Arrecifales en Puerto Morelos, ICML, UNAM, 77580, Puerto Morelos, Mexico
| | - Andrés López-Pérez
- Laboratorio de Arrecifes y Biodiversidad, Universidad Autónoma Metropolitana, 09340, Ciudad de México, Mexico
| | - Lorenzo Alvarez-Filip
- Biodiversity and Reef Conservation Laboratory, Unidad Académica de Sistemas Arrecifales en Puerto Morelos, ICML, UNAM, 77580, Puerto Morelos, Mexico
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2
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Lange ID, Molina-Hernández A, Medellín-Maldonado F, Perry CT, Álvarez-Filip L. Structure-from-motion photogrammetry demonstrates variability in coral growth within colonies and across habitats. PLoS One 2022; 17:e0277546. [PMID: 36383546 PMCID: PMC9668137 DOI: 10.1371/journal.pone.0277546] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/14/2022] [Accepted: 10/29/2022] [Indexed: 11/17/2022] Open
Abstract
Coral growth is an important metric of coral health and underpins reef-scale functional attributes such as structural complexity and calcium carbonate production. There persists, however, a paucity of growth data for most reef-building regions, especially for coral species whose skeletal architecture prevents the use of traditional methods such as coring and Alizarin staining. We used structure-from-motion photogrammetry to quantify a range of colony-scale growth metrics for six coral species in the Mexican Caribbean and present a newly developed workflow to measure colony volume change over time. Our results provide the first growth metrics for two species that are now major space occupiers on Caribbean reefs, Agaricia agaricites and Agaricia tenuifolia. We also document higher linear extension, volume increase and calcification rates within back reef compared to fore reef environments for four other common species: Orbicella faveolata, Porites astreoides, Siderastrea siderea and Pseudodiploria strigosa. Linear extension rates in our study were lower than those obtained via computed tomography (CT) scans of coral cores from the same sites, as the photogrammetry method averages growth in all dimensions, while the CT method depicts growth only along the main growth axis (upwards). The comparison of direct volume change versus potential volume increase calculated from linear extension emphasizes the importance of assessing whole colony growth to improve calcification estimates. The method presented here provides an approach that can generate accurate calcification estimates alongside a range of other whole-colony growth metrics in a non-invasive way.
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Affiliation(s)
- Ines D. Lange
- Geography, Faculty of Environment, Science and Economy, University of Exeter, Exeter, United Kingdom
- * E-mail:
| | - Ana Molina-Hernández
- Biodiversity and Reef Conservation Laboratory, Unidad Académica de Sistemas Arrecifales, Instituto de Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México, Puerto Morelos, Quintana Roo, México
| | - Francisco Medellín-Maldonado
- Biodiversity and Reef Conservation Laboratory, Unidad Académica de Sistemas Arrecifales, Instituto de Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México, Puerto Morelos, Quintana Roo, México
| | - Chris T. Perry
- Geography, Faculty of Environment, Science and Economy, University of Exeter, Exeter, United Kingdom
| | - Lorenzo Álvarez-Filip
- Biodiversity and Reef Conservation Laboratory, Unidad Académica de Sistemas Arrecifales, Instituto de Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México, Puerto Morelos, Quintana Roo, México
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3
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González-Barrios FJ, Cabral-Tena RA, Alvarez-Filip L. Recovery disparity between coral cover and the physical functionality of reefs with impaired coral assemblages. GLOBAL CHANGE BIOLOGY 2021; 27:640-651. [PMID: 33131196 DOI: 10.1111/gcb.15431] [Citation(s) in RCA: 21] [Impact Index Per Article: 7.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/31/2020] [Revised: 10/22/2020] [Accepted: 10/25/2020] [Indexed: 06/11/2023]
Abstract
The ecology and structure of many tropical coral reefs have been markedly altered over the past few decades. Although long-term recovery has been observed in terms of coral cover, it is not clear how novel species configurations shape reef functionality in impaired reefs. The identities and life-history strategies of the corals species that recover are essential for understanding reef functional dynamics. We used a species identity approach to quantify the physical functionality outcomes over a 13 year period across 56 sites in the Mexican Caribbean. This region was affected by multiple stressors that converged and drastically damaged reefs in the early 2000s. Since then, the reefs have shown evidence of a modest recovery of coral cover. We used Bayesian linear models and annual rates of change to estimate temporal changes in physical functionality and coral cover. Moreover, a functional diversity framework was used to explore changes in coral composition and the traits of those assemblages. Between 2005 and 2018, physical functionality increased at a markedly lower rate compared to that of coral cover. The disparity between recovery rates depended on the identity of the species that increased (mainly non-framework and foliose-digitate corals). No changes in species dominance or functional trait composition were observed, whereas non-framework building corals consistently dominated most reefs. Although the observed recovery of coral cover and functional potential may provide some ecological benefits, the long-term effects on reef frameworks remain unclear, as changes in the cover of key reef-building species were not observed. Our findings are likely to be representative of many reefs across the wider Caribbean basin, as declines in coral cover and rapid increases in the relative abundance of weedy corals have been reported regionally. A coral identity approach to assess species turnover is needed to understand and quantify changes in the functionality of coral reefs.
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Affiliation(s)
- F Javier González-Barrios
- Biodiversity and Reef Conservation Laboratory, Unidad Académica de Sistemas Arrecifales, Instituto de Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México, Puerto Morelos, México
- Department of Marine Ecology, Centro de Investigación Científica y de Educación Superior de Ensenada, Ensenada, México
| | - Rafael A Cabral-Tena
- Department of Marine Ecology, Centro de Investigación Científica y de Educación Superior de Ensenada, Ensenada, México
| | - Lorenzo Alvarez-Filip
- Biodiversity and Reef Conservation Laboratory, Unidad Académica de Sistemas Arrecifales, Instituto de Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México, Puerto Morelos, México
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Mapping coral calcification strategies from in situ boron isotope and trace element measurements of the tropical coral Siderastrea siderea. Sci Rep 2021; 11:472. [PMID: 33436642 PMCID: PMC7804963 DOI: 10.1038/s41598-020-78778-1] [Citation(s) in RCA: 7] [Impact Index Per Article: 2.3] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/18/2020] [Accepted: 11/30/2020] [Indexed: 02/02/2023] Open
Abstract
Boron isotopic and elemental analysis of coral aragonite can give important insights into the calcification strategies employed in coral skeletal construction. Traditional methods of analysis have limited spatial (and thus temporal) resolution, hindering attempts to unravel skeletal heterogeneity. Laser ablation mass spectrometry allows a much more refined view, and here we employ these techniques to explore boron isotope and co-varying elemental ratios in the tropical coral Siderastrea siderea. We generate two-dimensional maps of the carbonate parameters within the calcification medium that deposited the skeleton, which reveal large heterogeneities in carbonate chemistry across the macro-structure of a coral polyp. These differences have the potential to bias proxy interpretations, and indicate that different processes facilitated precipitation of different parts of the coral skeleton: the low-density columella being precipitated from a fluid with a carbonate composition closer to seawater, compared to the high-density inter-polyp walls where aragonite saturation was ~ 5 times that of external seawater. Therefore, the skeleton does not precipitate from a spatially homogeneous fluid and its different parts may thus have varying sensitivity to environmental stress. This offers new insights into the mechanisms behind the response of the S. siderea skeletal phenotype to ocean acidification.
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Coral calcification responses to the North Atlantic Oscillation and coral bleaching in Bermuda. PLoS One 2020; 15:e0241854. [PMID: 33175884 PMCID: PMC7657549 DOI: 10.1371/journal.pone.0241854] [Citation(s) in RCA: 4] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/20/2020] [Accepted: 10/21/2020] [Indexed: 01/24/2023] Open
Abstract
The North Atlantic Oscillation (NAO) has been hypothesized to drive interannual variability in Bermudan coral extension rates and reef-scale calcification through the provisioning of nutritional pulses associated with negative NAO winters. However, the direct influence of the NAO on Bermudan coral calcification rates remains to be determined and may vary between species and reef sites owing to implicit differences in coral life history strategies and environmental gradients across the Bermuda reef platform. In this study, we investigated the connection between negative NAO winters and Bermudan Diploria labyrinthiformis, Pseudodiploria strigosa, and Orbicella franksi coral calcification rates across rim reef, lagoon, and nearshore reef sites. Linear mixed effects modeling detected an inverse correlation between D. labyrinthiformis calcification rates and the winter NAO index, with higher rates associated with increasingly negative NAO winters. Conversely, there were no detectable correlations between P. strigosa or O. franksi calcification rates and the winter NAO index suggesting that coral calcification responses associated with negative NAO winters could be species-specific. The correlation between coral calcification rates and winter NAO index was significantly more negative at the outer rim of the reef (Hog Reef) compared to a nearshore reef site (Whalebone Bay), possibly indicating differential influence of the NAO as a function of the distance from the reef edge. Furthermore, a negative calcification anomaly was observed in 100% of D. labyrinthiformis cores in association with the 1988 coral bleaching event with a subsequent positive calcification anomaly in 1989 indicating a post-bleaching recovery in calcification rates. These results highlight the importance of assessing variable interannual coral calcification responses between species and across inshore-offshore gradients to interannual atmospheric modes such as the NAO, thermal stress events, and potential interactions between ocean warming and availability of coral nutrition to improve projections for future coral calcification rates under climate change.
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6
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Klepac CN, Barshis DJ. Reduced thermal tolerance of massive coral species in a highly variable environment. Proc Biol Sci 2020; 287:20201379. [PMID: 32811319 DOI: 10.1098/rspb.2020.1379] [Citation(s) in RCA: 22] [Impact Index Per Article: 5.5] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/04/2023] Open
Abstract
Coral bleaching events are increasing in frequency and severity, resulting in widespread losses in coral cover. However, branching corals native to highly variable (HV) thermal environments can have higher bleaching resistance than corals from more moderate habitats. Here, we investigated the response of two massive corals, Porites lobata and Goniastrea retiformis, from a moderately variable (MV) and a low variability (LV) pool transplanted into a HV pool on Ofu Island in American Samoa. Paired transplant and native ramets were exposed to an acute thermal stress after 6 and 12 months of exposure to the HV pool to evaluate changes in thermal tolerance limits. For both species, photosynthetic efficiency and chlorophyll loss following acute heat stress did not differ between ramets transplanted into the HV pool and respective native pool. Moreover, HV native P. lobata exhibited the greatest bleaching susceptibility compared to MV and LV natives and there was no effect of acute heat stress on MV P. lobata. There was also a thermal anomaly during the study, where Ofu's backreef thermal regime surpassed historical records-2015 had 8 degree heating weeks (DHW) and 2016 had up to 5 DHW (in comparison to less than or equal to 3 over the last 10 years)-which may have exceeded the upper thermal limits of HV native P. lobata. These results strongly contrast with other research on coral tolerance in variable environments, potentially underscoring species-specific mechanisms and regional thermal anomalies that may be equally important in shaping coral responses to extreme temperatures.
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Affiliation(s)
- C N Klepac
- Department of Biology, Old Dominion University, Norfolk, VA 23529, USA
| | - D J Barshis
- Department of Biology, Old Dominion University, Norfolk, VA 23529, USA
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de la Vega E, Foster GL, Martínez-Botí MA, Anagnostou E, Field MP, Kim MH, Watson P, Wilson PA. Automation of boron chromatographic purification for δ 11 B analysis of coral aragonite. RAPID COMMUNICATIONS IN MASS SPECTROMETRY : RCM 2020; 34:e8762. [PMID: 32067285 DOI: 10.1002/rcm.8762] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/27/2019] [Revised: 01/31/2020] [Accepted: 02/17/2020] [Indexed: 06/10/2023]
Abstract
RATIONALE To detect the small changes in past pH, the boron isotope ratio of coral carbonates, expressed as the δ11 B value, needs to be both precise and accurate (2sd <<1‰). Boron measurements by Multi-Collector Inductively Coupled Plasma Mass Spectrometry (MC-ICPMS) require the boron to be carefully purified before analysis, which is time consuming, and requires specialist training. Here, we use the prepFAST-MC method that enables the automatic extraction of B (up to 25 ng load) from a CaCO3 matrix. METHODS Samples were purified using the prepFAST-MC automated system with a ~25-μL column of Amberlite IRA743 resin. Boron isotope measurements were performed by MC-ICPMS. The effects of matrix load, speed of sample loading onto the column, and blank contamination were tested to evaluate the effects on the purification process. The optimised protocol was tested on various standards and samples of aragonite corals. RESULTS The blank contribution for the approach is ~60 pg and is negligible given our sample size (<0.2% sample size). Efficiency of matrix removal is demonstrated with the addition of up to 1.6 mg of dissolved low-B calcium carbonate to NIST SRM 951 with no impact on the accuracy of δ11 B values. The Japanese Geological Survey Porites reference material JCp-1, boric acid standard NIST SRM 951, and seawater, all processed on the prepFAST-MC system, give δ11 B values within error of literature values (δ11 BJCp-1 = 24.31 ± 0.20‰ (2sd, n = 20); δ11 BNIST 951 = -0.02 ± 0.15‰ (2sd, n = 13) and δ11 BSeawater = 39.50 ± 0.06‰ (2sd, n = 2)). Results obtained from the coral Siderastrea siderea purified with the prepFAST-MC system show an average offset from the manual ion-exchange protocols of Δδ11 B = 0.01 ± 0.28‰ (2sd, n = 12). CONCLUSIONS Our study demonstrates the capacity of the prepFAST-MC method to generate accurate and reproducible δ11 B values for a range of materials, without fractionation, with efficient matrix removal and with negligible blank contribution.
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Affiliation(s)
- Elwyn de la Vega
- School of Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Southampton, SO14 3ZH, UK
| | - Gavin L Foster
- School of Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Southampton, SO14 3ZH, UK
| | - Miguel Angel Martínez-Botí
- School of Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Southampton, SO14 3ZH, UK
| | - Eleni Anagnostou
- School of Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Southampton, SO14 3ZH, UK
- GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstraße 1-3, 24148, Kiel, Germany
| | - M Paul Field
- Elemental Scientific, Inc, 7277 World Communications Drive, Omaha, NE, 68122, USA
| | - M Hwan Kim
- Elemental Scientific, Inc, 7277 World Communications Drive, Omaha, NE, 68122, USA
| | - Paul Watson
- Elemental Scientific, Inc, 7277 World Communications Drive, Omaha, NE, 68122, USA
| | - Paul A Wilson
- School of Ocean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Southampton, SO14 3ZH, UK
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Baumann JH, Ries JB, Rippe JP, Courtney TA, Aichelman HE, Westfield I, Castillo KD. Nearshore coral growth declining on the Mesoamerican Barrier Reef System. GLOBAL CHANGE BIOLOGY 2019; 25:3932-3945. [PMID: 31456305 DOI: 10.1111/gcb.14784] [Citation(s) in RCA: 12] [Impact Index Per Article: 2.4] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 02/01/2019] [Revised: 07/23/2019] [Accepted: 07/23/2019] [Indexed: 06/10/2023]
Abstract
Anthropogenic global change and local stressors are impacting coral growth and survival worldwide, altering the structure and function of coral reef ecosystems. Here, we show that skeletal extension rates of nearshore colonies of two abundant and widespread Caribbean corals (Siderastrea siderea, Pseudodiploria strigosa) declined across the Belize Mesoamerican Barrier Reef System (MBRS) over the past century, while offshore coral conspecifics exhibited relatively stable extension rates over the same temporal interval. This decline has caused nearshore coral extension rates to converge with those of their historically slower growing offshore coral counterparts. For both species, individual mass coral bleaching events were correlated with low rates of skeletal extension within specific reef environments, but no single bleaching event was correlated with low skeletal extension rates across all reef environments. We postulate that the decline in skeletal extension rates for nearshore corals is driven primarily by the combined effects of long-term ocean warming and increasing exposure to higher levels of land-based anthropogenic stressors, with acute thermally induced bleaching events playing a lesser role. If these declining trends in skeletal growth of nearshore S. siderea and P. strigosa continue into the future, the structure and function of these critical nearshore MBRS coral reef systems is likely to be severely impaired.
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Affiliation(s)
- Justin H Baumann
- Department of Marine Sciences, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina
- Biology Department, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina
| | - Justin B Ries
- Department of Marine and Environmental Sciences, Marine Science Center, Northeastern University, Nahant, Massachusetts
| | - John P Rippe
- Department of Marine Sciences, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina
| | - Travis A Courtney
- Department of Marine Sciences, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina
- Department of Marine and Environmental Sciences, Marine Science Center, Northeastern University, Nahant, Massachusetts
- Scripps Institution of Oceanography, University of California San Diego, La Jolla, California
| | - Hannah E Aichelman
- Department of Marine Sciences, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina
- Department of Biological Sciences, Boston University, Boston, Massachusetts
| | - Isaac Westfield
- Department of Marine and Environmental Sciences, Marine Science Center, Northeastern University, Nahant, Massachusetts
| | - Karl D Castillo
- Department of Marine Sciences, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina
- Environment, Ecology, and Energy Program, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina
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Rippe JP, Baumann JH, De Leener DN, Aichelman HE, Friedlander EB, Davies SW, Castillo KD. Corals sustain growth but not skeletal density across the Florida Keys Reef Tract despite ongoing warming. GLOBAL CHANGE BIOLOGY 2018; 24:5205-5217. [PMID: 30102827 DOI: 10.1111/gcb.14422] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 04/10/2018] [Revised: 07/11/2018] [Accepted: 08/06/2018] [Indexed: 06/08/2023]
Abstract
Through the continuous growth of their carbonate skeletons, corals record information about past environmental conditions and their effect on colony fitness. Here, we characterize century-scale growth records of inner and outer reef corals across ~200 km of the Florida Keys Reef Tract (FKRT) using skeletal cores extracted from two ubiquitous reef-building species, Siderastrea siderea and Pseudodiploria strigosa. We find that corals across the FKRT have sustained extension and calcification rates over the past century but have experienced a long-term reduction in skeletal density, regardless of reef zone. Notably, P. strigosa colonies exhibit temporary reef zone-dependent reductions in extension rate corresponding to two known extreme temperature events in 1969-1970 and 1997-1998. We propose that the subtropical climate of the FKRT may buffer corals from chronic growth declines associated with climate warming, though the significant reduction in skeletal density may indicate underlying vulnerability to present and future trends in ocean acidification.
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Affiliation(s)
- John P Rippe
- Department of Marine Sciences, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina
| | - Justin H Baumann
- Department of Marine Sciences, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina
| | - Daphne N De Leener
- Department of Marine Sciences, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina
| | - Hannah E Aichelman
- Department of Marine Sciences, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina
- Department of Biology, Boston University, Boston, Massachusetts
| | - Eric B Friedlander
- Department of Statistics and Operations Research, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina
| | - Sarah W Davies
- Department of Marine Sciences, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina
- Department of Biology, Boston University, Boston, Massachusetts
| | - Karl D Castillo
- Department of Marine Sciences, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina
- Curriculum for Environment and Ecology, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina
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10
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Baumann JH, Davies SW, Aichelman HE, Castillo KD. Coral Symbiodinium Community Composition Across the Belize Mesoamerican Barrier Reef System is Influenced by Host Species and Thermal Variability. MICROBIAL ECOLOGY 2018; 75:903-915. [PMID: 29098358 DOI: 10.1007/s00248-017-1096-6] [Citation(s) in RCA: 15] [Impact Index Per Article: 2.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/22/2017] [Accepted: 10/24/2017] [Indexed: 06/07/2023]
Abstract
Reef-building corals maintain a symbiotic relationship with dinoflagellate algae of the genus Symbiodinium, and this symbiosis is vital for the survival of the coral holobiont. Symbiodinium community composition within the coral host has been shown to influence a coral's ability to resist and recover from stress. A multitude of stressors including ocean warming, ocean acidification, and eutrophication have been linked to global scale decline in coral health and cover in recent decades. Three distinct thermal regimes (highTP, modTP, and lowTP) following an inshore-offshore gradient of declining average temperatures and thermal variation were identified on the Belize Mesoamerican Barrier Reef System (MBRS). Quantitative metabarcoding of the ITS-2 locus was employed to investigate differences and similarities in Symbiodinium genetic diversity of the Caribbean corals Siderastrea siderea, S. radians, and Pseudodiploria strigosa between the three thermal regimes. A total of ten Symbiodinium lineages were identified across the three coral host species. S. siderea was associated with distinct Symbiodinium communities; however, Symbiodinium communities of its congener, S. radians and P. strigosa, were more similar to one another. Thermal regime played a role in defining Symbiodinium communities in S. siderea but not S. radians or P. strigosa. Against expectations, Symbiodinium trenchii, a symbiont known to confer thermal tolerance, was dominant only in S. siderea at one sampled offshore site and was rare inshore, suggesting that coral thermal tolerance in more thermally variable inshore habitats is achieved through alternative mechanisms. Overall, thermal parameters alone were likely not the only primary drivers of Symbiodinium community composition, suggesting that environmental variables unrelated to temperature (i.e., light availability or nutrients) may play key roles in structuring coral-algal communities in Belize and that the relative importance of these environmental variables may vary by coral host species.
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Affiliation(s)
- J H Baumann
- Department of Marine Sciences, University of North Carolina at Chapel Hill, Chapel Hill, NC, 27599-3300, USA.
| | - S W Davies
- Department of Marine Sciences, University of North Carolina at Chapel Hill, Chapel Hill, NC, 27599-3300, USA
- Department of Biology, Boston University, 5 Cummington Mall, Boston, MA, 02215, USA
| | - H E Aichelman
- Department of Marine Sciences, University of North Carolina at Chapel Hill, Chapel Hill, NC, 27599-3300, USA
- Department of Biological Sciences, Old Dominion University, 302 Miles Godwin building, Norfolk, VA, 23529, USA
| | - K D Castillo
- Department of Marine Sciences, University of North Carolina at Chapel Hill, Chapel Hill, NC, 27599-3300, USA
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11
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Banks S, Foster K. Baseline Levels of <i>Siderastrea siderea</i> Bleaching under Normal Environmental Conditions in Little Cayman. ACTA ACUST UNITED AC 2017. [DOI: 10.4236/ojms.2017.71011] [Citation(s) in RCA: 5] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/20/2022]
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12
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Madin JS, Anderson KD, Andreasen MH, Bridge TC, Cairns SD, Connolly SR, Darling ES, Diaz M, Falster DS, Franklin EC, Gates RD, Hoogenboom MO, Huang D, Keith SA, Kosnik MA, Kuo CY, Lough JM, Lovelock CE, Luiz O, Martinelli J, Mizerek T, Pandolfi JM, Pochon X, Pratchett MS, Putnam HM, Roberts TE, Stat M, Wallace CC, Widman E, Baird AH. The Coral Trait Database, a curated database of trait information for coral species from the global oceans. Sci Data 2016; 3:160017. [PMID: 27023900 PMCID: PMC4810887 DOI: 10.1038/sdata.2016.17] [Citation(s) in RCA: 98] [Impact Index Per Article: 12.3] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/06/2015] [Accepted: 01/28/2016] [Indexed: 01/19/2023] Open
Abstract
Trait-based approaches advance ecological and evolutionary research because traits provide a strong link to an organism's function and fitness. Trait-based research might lead to a deeper understanding of the functions of, and services provided by, ecosystems, thereby improving management, which is vital in the current era of rapid environmental change. Coral reef scientists have long collected trait data for corals; however, these are difficult to access and often under-utilized in addressing large-scale questions. We present the Coral Trait Database initiative that aims to bring together physiological, morphological, ecological, phylogenetic and biogeographic trait information into a single repository. The database houses species- and individual-level data from published field and experimental studies alongside contextual data that provide important framing for analyses. In this data descriptor, we release data for 56 traits for 1547 species, and present a collaborative platform on which other trait data are being actively federated. Our overall goal is for the Coral Trait Database to become an open-source, community-led data clearinghouse that accelerates coral reef research.
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Affiliation(s)
- Joshua S. Madin
- Department of Biological Sciences, Macquarie University, New South Wales 2109, Australia
| | - Kristen D. Anderson
- Australian Research Council Centre of Excellence for Coral Reef Studies, James Cook University, Townsville 4811, Australia
| | - Magnus Heide Andreasen
- Center for Macroecology, Evolution & Climate, Natural History Museum of Denmark, University of Copenhagen, Copenhagen DK-2100, Denmark
| | - Tom C.L. Bridge
- Australian Research Council Centre of Excellence for Coral Reef Studies, James Cook University, Townsville 4811, Australia
- Australian Institute of Marine Science, PMB #3, Townsville MC, Townsville 4810, Australia
| | - Stephen D. Cairns
- Department of Invertebrate Zoology, National Museum of Natural History, Smithsonian, Washington, District Of Columbia 20013, USA
| | - Sean R. Connolly
- Australian Research Council Centre of Excellence for Coral Reef Studies, James Cook University, Townsville 4811, Australia
- College of Marine and Environmental Sciences, James Cook University, Townsville 4811, Australia
| | - Emily S. Darling
- Marine Program, Wildlife Conservation Society, Bronx, New York 10460, USA
| | - Marcela Diaz
- Department of Biological Sciences, Macquarie University, New South Wales 2109, Australia
| | - Daniel S. Falster
- Department of Biological Sciences, Macquarie University, New South Wales 2109, Australia
| | - Erik C. Franklin
- University of Hawaii, Hawaii Institute of Marine Biology, School of Ocean and Earth Science and Technology, Kaneohe, Hawaii 96744, USA
| | - Ruth D. Gates
- University of Hawaii, Hawaii Institute of Marine Biology, School of Ocean and Earth Science and Technology, Kaneohe, Hawaii 96744, USA
| | - Mia O. Hoogenboom
- Australian Research Council Centre of Excellence for Coral Reef Studies, James Cook University, Townsville 4811, Australia
- College of Marine and Environmental Sciences, James Cook University, Townsville 4811, Australia
| | - Danwei Huang
- Department of Biological Sciences and Tropical Marine Science Institute, National University of Singapore, Singapore 117543, Singapore
| | - Sally A. Keith
- Center for Macroecology, Evolution & Climate, Natural History Museum of Denmark, University of Copenhagen, Copenhagen DK-2100, Denmark
| | - Matthew A. Kosnik
- Department of Biological Sciences, Macquarie University, New South Wales 2109, Australia
| | - Chao-Yang Kuo
- Australian Research Council Centre of Excellence for Coral Reef Studies, James Cook University, Townsville 4811, Australia
| | - Janice M. Lough
- Australian Research Council Centre of Excellence for Coral Reef Studies, James Cook University, Townsville 4811, Australia
- Australian Institute of Marine Science, PMB #3, Townsville MC, Townsville 4810, Australia
| | - Catherine E. Lovelock
- School of Biological Sciences, The University of Queensland, St Lucia, Queensland 4072, Australia
| | - Osmar Luiz
- Department of Biological Sciences, Macquarie University, New South Wales 2109, Australia
| | - Julieta Martinelli
- Department of Biological Sciences, Macquarie University, New South Wales 2109, Australia
| | - Toni Mizerek
- Department of Biological Sciences, Macquarie University, New South Wales 2109, Australia
| | - John M. Pandolfi
- Australian Research Council Centre of Excellence for Coral Reef Studies, School of Biological Sciences, The University of Queensland, St Lucia, Queensland 4072, Australia
| | - Xavier Pochon
- Environmental Technologies, Coastal & Freshwater Group, The Cawthron Institute, Nelson 7010, New Zealand
- Institute of Marine Science, The University of Auckland, Auckland 1142, New Zealand
| | - Morgan S. Pratchett
- Australian Research Council Centre of Excellence for Coral Reef Studies, James Cook University, Townsville 4811, Australia
| | - Hollie M. Putnam
- University of Hawaii, Hawaii Institute of Marine Biology, School of Ocean and Earth Science and Technology, Kaneohe, Hawaii 96744, USA
| | - T. Edward Roberts
- Australian Research Council Centre of Excellence for Coral Reef Studies, James Cook University, Townsville 4811, Australia
| | - Michael Stat
- Trace and Environmental DNA Laboratory, Department of Environment and Agriculture, Curtin University, Perth, Western Australia 6102, Australia
| | - Carden C. Wallace
- Biodiversity and Geosciences Program, Queensland Museum Network, South Brisbane, Queensland 4101, Australia
| | - Elizabeth Widman
- School of Life Sciences, The University of Warwick, Coventry CV4 7AL, UK
| | - Andrew H. Baird
- Australian Research Council Centre of Excellence for Coral Reef Studies, James Cook University, Townsville 4811, Australia
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13
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Influence of land development on Holocene Porites coral calcification at Nagura Bay, Ishigaki Island, Japan. PLoS One 2014; 9:e88790. [PMID: 24586393 PMCID: PMC3933341 DOI: 10.1371/journal.pone.0088790] [Citation(s) in RCA: 20] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 05/13/2013] [Accepted: 01/11/2014] [Indexed: 11/19/2022] Open
Abstract
To evaluate the relationships between coral calcification, thermal stress, and sedimentation and eutrophication linked to human impact (hereafter referred to as "land development") by river discharge, we analyzed growth characteristics in the context of a paleoenvironment that was reconstructed from geochemical signals in modern and fossil (1.2 cal kyr BP and 3.5 cal kyr BP, respectively) massive Porites corals from Nagura Bay ("Nagura") and from modern Porites corals from the estuary of the Todoroki River, Shiraho Reef ("Todoroki"). Both sites are on Ishigaki Island, Japan, and Nagura is located approximately 12 km west of Todoroki. At Nagura, the individual corals provide time windows of 13 (modern), 10 (1.2 cal kyr BP), and 38 yr in length (3.5 cal kyr BP). Here, we present the coral annual calcification for Nagura and Todoroki, and (bi) monthly resolved records of Sr/Ca (a proxy of sea surface temperature (SST)) and Ba/Ca (a proxy of sedimentation and nutrients related to land development) for Nagura. At Nagura, the winter SST was cooler by 2.8°C in the 1.2 cal kyr BP, and the annual and winter SSTs in the 3.5 cal kyr BP were cooler by 2.6°C and 4.6°C, respectively. The annual periodicity of Ba/Ca in modern coral is linked to river discharge and is associated with land development including sugar cane cultivation. Modern coral calcification also has declined with SST warming and increasing Ba/Ca peaks in winter. However, calcification of fossil corals does not appear to have been influenced by variations in Sr/Ca and Ba/Ca. Modern coral growth characteristics at Nagura and Todoroki indicate that coral growth is both spatially and temporally influenced by river discharge and land development. At Nagura, our findings suggest that land development induces negative thermal sensitivity for calcification in winter due to sugar cane harvest, which is a specifically modern phenomenon.
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