Coral reefs in Fatu Huku Island, Marquesas Archipelago, French Polynesia

Author(s):  
Antoine Collin ◽  
Jean Laporte ◽  
Benjamin Koetz ◽  
François-Régis Martin-Lauzer ◽  
Yves-Louis Desnos
Keyword(s):  
Coral Reefs ◽  
2021 ◽  
Author(s):  
Eleanor J. Vaughan ◽  
Shaun K. Wilson ◽  
Samantha J. Howlett ◽  
Valeriano Parravicini ◽  
Gareth J. Williams ◽  
...  

AbstractScleractinian corals are engineers on coral reefs that provide both structural complexity as habitat and sustenance for other reef-associated organisms via the release of organic and inorganic matter. However, coral reefs are facing multiple pressures from climate change and other stressors, which can result in mass coral bleaching and mortality events. Mass mortality of corals results in enhanced release of organic matter, which can cause significant alterations to reef biochemical and recycling processes. There is little known about how long these nutrients are retained within the system, for instance, within the tissues of other benthic organisms. We investigated changes in nitrogen isotopic signatures (δ15N) of macroalgal tissues (a) ~ 1 year after a bleaching event in the Seychelles and (b) ~ 3 months after the peak of a bleaching event in Mo’orea, French Polynesia. In the Seychelles, there was a strong association between absolute loss in both total coral cover and branching coral cover and absolute increase in macroalgal δ15N between 2014 and 2017 (adjusted r2 = 0.79, p = 0.004 and adjusted r2 = 0.86, p = 0.002, respectively). In Mo’orea, a short-term transplant experiment found a significant increase in δ15N in Sargassum mangarevense after specimens were deployed on a reef with high coral mortality for ~ 3 weeks (p < 0.05). We suggest that coral-derived nutrients can be retained within reef nutrient cycles, and that this can affect other reef-associated organisms over both short- and long-term periods, especially opportunistic species such as macroalgae. These species could therefore proliferate on reefs that have experienced mass mortality events, because they have been provided with both space and nutrient subsidies by the death and decay of corals.


PLoS ONE ◽  
2017 ◽  
Vol 12 (6) ◽  
pp. e0178795 ◽  
Author(s):  
Marc Besson ◽  
Camille Gache ◽  
Rohan M. Brooker ◽  
Rakamaly Madi Moussa ◽  
Viliame Pita Waqalevu ◽  
...  

2020 ◽  
Vol 8 (6) ◽  
pp. 406
Author(s):  
Isabelle Bonnard ◽  
Louis Bornancin ◽  
Klervi Dalle ◽  
Mireille Chinain ◽  
Mayalen Zubia ◽  
...  

In the last decades, an apparent increase in the frequency of benthic cyanobacterial blooms has occurred in coral reefs and tropical lagoons, possibly in part because of global change and anthropogenic activities. In the frame of the survey of marine benthic cyanobacteria proliferating in the lagoon of Moorea Island (French Polynesia), 15 blooms were collected, mainly involving three species—Anabaena sp.1, Lyngbya majuscula and Hydrocoleum majus-B. Their chemical fingerprints, obtained through high performance liquid chromatography combined with UV detection and mass spectrometry (HPLC-UV-MS) analyses, revealed a high extent of species-specificity. The chemical profile of Anabaena sp.1 was characterized by three major cyclic lipopeptides of the laxaphycin family, whereas the one of L. majuscula was characterized by a complex mixture including tiahuramides, trungapeptins and serinol-derived malyngamides. Toxicity screening analyses conducted on these cyanobacterial samples using Artemia salina and mouse neuroblastoma cell-based (CBA-N2a) cytotoxic assays failed to show any toxicity to a degree that would merit risk assessment with regard to public health. However, the apparently increasing presence of blooms of Lyngbya, Hydrocoleum, Anabaena or other benthic cyanobacteria on coral reefs in French Polynesia encourages the implementation of ad hoc monitoring programs for the surveillance of their proliferation and potential assessment of associated hazards.


2019 ◽  
pp. 74-102
Author(s):  
David O. McKay

McKay’s steamship docked at Honolulu, Hawaii, on February 4, 1921. The tropical beauty of the islands impressed McKay as he ventured throughout the islands. Mormon missionaries had enjoyed proselyting success in the Hawaiian Islands since their arrival in the 1850s. McKay spoke at well-attended conferences across the islands, visited church-owned plantations and schools, and were immersed in the local culture. McKay noted the multicultural composition of the local church membership, enjoyed homemade luaus prepared by local Latter-day Saints, offered guidance to young missionaries, and marveled at geographic landmarks, including volcanoes, coral reefs, and waterfalls. On February 26, 1921, McKay and Cannon boarded a steamer bound for San Francisco, California, where they planned to transfer steamers and travel to French Polynesia.


1994 ◽  
Vol 25 (3) ◽  
pp. 189-216 ◽  
Author(s):  
C. Gabrié ◽  
S. Planes ◽  
J. Baldwin ◽  
J. Bonvallot ◽  
C. Chauvet ◽  
...  

2017 ◽  
Vol 14 (14) ◽  
pp. 3549-3560 ◽  
Author(s):  
Steeve Comeau ◽  
Peter J. Edmunds ◽  
Coulson A. Lantz ◽  
Robert C. Carpenter

Abstract. The threat represented by ocean acidification (OA) for coral reefs has received considerable attention because of the sensitivity of calcifiers to changing seawater carbonate chemistry. However, most studies have focused on the organismic response of calcification to OA, and only a few have addressed community-level effects, or investigated parameters other than calcification, such as photosynthesis. Light (photosynthetically active radiation, PAR) is a driver of biological processes on coral reefs, and the possibility that these processes might be perturbed by OA has important implications for community function. Here we investigate how CO2 enrichment affects the relationships between PAR and community net O2 production (Pnet), and between PAR and community net calcification (Gnet), using experiments on three coral communities constructed to match (i) the back reef of Mo'orea, French Polynesia, (ii) the fore reef of Mo'orea, and (iii) the back reef of O'ahu, Hawaii. The results were used to test the hypothesis that OA affects the relationship between Pnet and Gnet. For the three communities tested, pCO2 did not affect the Pnet–PAR relationship, but it affected the intercept of the hyperbolic tangent curve fitting the Gnet–PAR relationship for both reef communities in Mo'orea (but not in O'ahu). For the three communities, the slopes of the linear relationships between Pnet and Gnet were not affected by OA, although the intercepts were depressed by the inhibitory effect of high pCO2 on Gnet. Our result indicates that OA can modify the balance between net calcification and net photosynthesis of reef communities by depressing community calcification, but without affecting community photosynthesis.


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