scholarly journals Influence of the Blue Coral Heliopora coerulea on Scleractinian Coral Larval Recruitment

2017 ◽  
Vol 2017 ◽  
pp. 1-5 ◽  
Author(s):  
Michael Atrigenio ◽  
Porfirio Aliño ◽  
Cecilia Conaco

The octocoral Heliopora coerulea has emerged as one of the most dominant reef-building corals in the Bolinao Reef Complex, northern Philippines. One of the possible mechanisms that may contribute to the success of H. coerulea over scleractinian corals is its ability to compete effectively for space on the reef by inhibiting the settlement of coral larvae in its immediate vicinity. To determine whether H. coerulea can indeed inhibit larval recruitment, settlement tiles were deployed inside H. coerulea aggregations or on hard substrate at a distance of about 2 to 3 meters away. After three months of deployment, only a single H. coerulea recruit was observed on tiles placed within aggregations whereas many different coral recruits were observed on tiles placed on substrate away from the blue coral. These results suggest that adult H. coerulea can inhibit the settlement of scleractinian larvae. This effect may be mediated by various mechanisms, such as the production of allelopathic compounds, deployment of mesenterial filaments, and sweeper tentacles. However, further studies are needed to determine the modes of competition that are used by the coral.

Author(s):  
Jarosław Stolarski ◽  
Ismael Coronado ◽  
Jack G. Murphy ◽  
Marcelo V. Kitahara ◽  
Katarzyna Janiszewska ◽  
...  

One of the most conserved traits in the evolution of biomineralizing organisms is the taxon-specific selection of skeletal minerals. All modern scleractinian corals are thought to produce skeletons exclusively of the calcium-carbonate polymorph aragonite. Despite strong fluctuations in ocean chemistry (notably the Mg/Ca ratio), this feature is believed to be conserved throughout the coral fossil record, spanning more than 240 million years. Only one example, the Cretaceous scleractinian coral Coelosmilia (ca. 70 to 65 Ma), is thought to have produced a calcitic skeleton. Here, we report that the modern asymbiotic scleractinian coral Paraconotrochus antarcticus living in the Southern Ocean forms a two-component carbonate skeleton, with an inner structure made of high-Mg calcite and an outer structure composed of aragonite. P. antarcticus and Cretaceous Coelosmilia skeletons share a unique microstructure indicating a close phylogenetic relationship, consistent with the early divergence of P. antarcticus within the Vacatina (i.e., Robusta) clade, estimated to have occurred in the Mesozoic (ca. 116 Mya). Scleractinian corals thus join the group of marine organisms capable of forming bimineralic structures, which requires a highly controlled biomineralization mechanism; this capability dates back at least 100 My. Due to its relatively prolonged isolation, the Southern Ocean stands out as a repository for extant marine organisms with ancient traits.


Coral Reefs ◽  
2016 ◽  
Vol 36 (1) ◽  
pp. 97-104 ◽  
Author(s):  
E. M. Graham ◽  
A. H. Baird ◽  
S. R. Connolly ◽  
M. A. Sewell ◽  
B. L. Willis

2013 ◽  
Vol 64 (1) ◽  
pp. 63-69 ◽  
Author(s):  
Elżbieta Morycowa ◽  
Barbara Olszewska

Abstract The paper deals with benthic foraminifera occurring with the scleractinian corals in the Jurassic biohermal and peribiohermal coral-bearing limestones of the Vršatec area (Czorsztyn Succession, Slovak Pieniny Klippen Belt). The coral community is dominated by branching forms of the genus Thecosmilia. Co-occurring abundant benthic foraminifera belong to the species Rumanolina seiboldi, R. elevata, Paalzowella turbinella and Troglotella incrustans. The coral-bearing limestones were initially assigned to the Oxfordian on the basis of the microfacies analyses and bivalve and scleractinian faunas. In recent papers they are assigned to the Bajocian on the basis of ammonites found in the neptunic dykes and stratigraphic superimposition criteria. However, the stratigraphic distribution of the majority of the identified foraminifera indicates that like most scleractinian coral taxa they are not known earlier than in the Late Jurassic. The Late Jurassic age of these coral-bearing limestones is also suggested by an encrusting microproblematic organism Iberopora bodeuri.


2018 ◽  
Vol 39 (1) ◽  
pp. e12482 ◽  
Author(s):  
Ana Carolina Grillo ◽  
Roberta Martini Bonaldo ◽  
Bárbara Segal

Oecologia ◽  
2013 ◽  
Vol 173 (2) ◽  
pp. 431-438 ◽  
Author(s):  
Erin M. Graham ◽  
Andrew H. Baird ◽  
Bette L. Willis ◽  
Sean R. Connolly

Coral Reefs ◽  
2008 ◽  
Vol 27 (3) ◽  
pp. 529-539 ◽  
Author(s):  
E. M. Graham ◽  
A. H. Baird ◽  
S. R. Connolly

Zootaxa ◽  
2006 ◽  
Vol 1188 (1) ◽  
pp. 55 ◽  
Author(s):  
MICHEL R. CLAEREBOUDT

A new species of scleractinian coral, Porites decasepta spec. nov. (Scleractinia, Poritidae) is described from the Bar Al-Hikman reef complex along the Arabian Sea coast of the Sultanate of Oman. Porites decasepta spec. nov. forms encrusting, bright blue colonies rarely exceeding 7 cm in diameter. Corallites, about 1mm in diameter, have only 10 septa: the two lateral septa of the ventral triplet typical of Porites septal arrangement are missing or strongly reduced. Une nouvelle espèce de scleractiniaire, Porites decasepta spec. nov. (Scleractinia Poritidae) est décrite du complex récifal de Bar Al-Hikman situé le long de la côte de la mer d’arabie du Sultanat d’Oman. La nouvelle espèce forme de petites colonies encroûtantes, de couleur bleu-violet, ne dépassant guère 7 cm de diamètre. Les corallites d’à peu près 1mm de diamètre n’ont que 10 septa: les deux septa latéraux du triplet ventral étant le plus souvent manquants ou fortement réduits.


2009 ◽  
Vol 50 (47) ◽  
pp. 6606-6609 ◽  
Author(s):  
Makoto Kitamura ◽  
Peter J. Schupp ◽  
Yoshikatsu Nakano ◽  
Daisuke Uemura

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