Holocene growth history of an eastern Pacific fringing reef,Punta Islotes,Costa Rica

Rock and sediment cores reveal that a well-developed fringing reef in Golfo Dulce, Pacific Costa Rica, up to 9 m thick was established on Cretaceous basalt about 5500 y BP. It is presently being smothered with fine sediments and is almost completely dead. This reef is made up of three main facies that are represented by comparable extant reef zones: reef-flat branching coral, fore-reef slope massive coral, and fore-reef talus sediment facies. Reef growth began with the establishment of small patch reefs dominantly formed by the branching coral Pocillopora damicornis. P. damicornis spread across the basalt bench and massive colonies of Porites lobata grew on the outer slopes, eventually blocking the seaward transport of Pocillopora fragments to the fore-reef talus sediments. The reef flourished until 500 years ago. Lower accumulation rates during the past 500 years may be due to deteriorating environmental conditions rather than slower growth after the reef reached sea level. Present-day reef communities are severely degraded with less than 2% living coral cover. The increased turbidity associated with the final stage of degradation of this reef is probably related to human activity on the adjacent shores, including deforestation, mining, and road construction.     

Checklist of recent brachiopod species collected during the Terrasses and Exbodi cruises in the New Caledonian region,SW Pacific

Twenty species belonging to 16 genera, i.e. Neoancistrocrania, Novocrania, Basiliola, Basiliolella, Ebiscothyris, Stenosarina, Kanakythyris, Xenobrochus, Terebratulina, Eucalathis, Fallax, Frenulina, Septicollarina, Campages, Annuloplatidia, and Thecidellina have been identified in the material collected during the Terrasses and Exbodi cruises in the New Caledonian region, SW Pacific. The species Basiliolella grayi (Woodward, 1855) and Fallax neocaledonensis Laurin, 1997 are the most common in the studied collection, while Eucalathis murrayi (Davidson, 1878) is reported for the first time from the New Caledonian region.     

Coral reef development under naturally turbid conditions: fringing reefs near Broad Sound,Australia

Reef coring and NOAA/AVHRR imagery were used to examine differences in reef colonisation and accumulation across a gradient of increasing tidal range and turbidity. AVHRR channel-1 reflectance, which was strongly correlated with suspended sediment concentration (SSC), demonstrated that SSC is due to tidal resuspension of sediments, and increases with increasing tidal range. Underwater surveys and reef coring revealed that reef development diminishes with increasing SSC toward Broad Sound. Few reefs near Broad Sound have formed reef flats; those that have are thinner and accumulated more slowly during the Holocene. The many submerged reefs in this area represent a mixture of reef turn-ons and turn-offs. Some are probably incipient reefs in the early stages of reef growth. Others appear to be coral communities growing as thin veneers on exposed rock surfaces, rather than coral reef communities with capacity for reef-building. Still others developed reef flats earlier in the Holocene, and have since turned-off.     

The Acropora inheritance: A reinterpretation of the development of fringing reefs in Barbados,West Indies

The discovery of the widespread occurrence of the remains of the reef coral Acropora palmata within the fabric of the fringing reefs on the west coast of Barbados requires a new interpretation of their Holocene development. Radiocarbon dating of the A. palmata framework suggests that reef construction by this species began as early as 2,300 years B.P. A. palmata probably flourished in Barbados into the present century but has now declined. The present fringing reefs are characterized by a core and base of A. palmata upon which subsequent colonization took place, especially by Montastrea annularis, Porites porites and coralline algae.     

Shelters and their use by fishes on fringing coral reefs

Coral reef fish density and species richness are often higher at sites with more structural complexity. This association may be due to greater availability of shelters, but surprisingly little is known about the size and density of shelters and their use by coral reef fishes. We quantified shelter availability and use by fishes for the first time on a Caribbean coral reef by counting all holes and overhangs with a minimum entrance diameter ≥3 cm in 30 quadrats (25 m(2)) on two fringing reefs in Barbados. Shelter size was highly variable, ranging from 42 cm(3) to over 4,000,000 cm(3), with many more small than large shelters. On average, there were 3.8 shelters m(-2), with a median volume of 1,200 cm(3) and a total volume of 52,000 cm(3) m(-2). The number of fish per occupied shelter ranged from 1 to 35 individual fishes belonging to 66 species, with a median of 1. The proportion of shelters occupied and the number of occupants increased strongly with shelter size. Shelter density and total volume increased with substrate complexity, and this relationship varied among reef zones. The density of shelter-using fish was much more strongly predicted by shelter density and median size than by substrate complexity and increased linearly with shelter density, indicating that shelter availability is a limiting resource for some coral reef fishes. The results demonstrate the importance of large shelters for fish density and support the hypothesis that structural complexity is associated with fish abundance, at least in part, due to its association with shelter availability. This information can help identify critical habitat for coral reef fishes, predict the effects of reductions in structural complexity of natural reefs and improve the design of artificial reefs.     

Storms may disrupt top-down control of algal turf on fringing reefs

Coral Reefs - Storms strongly affect coral reefs; one unstudied but potentially important outcome may be a decrease in herbivory, presumably through changes to freshwater, sediment and nutrient...     

Evolution of fringing reefs: space and time constraints from the Gulf of Aqaba

This study documents the pattern and rate of reef growth during the late Holocene as revealed by unique geological conditions at the subsiding NW Gulf of Aqaba. We discovered that the modern fringing reef near the city Elat grows on top of a fossil submerged mid-Holocene reef platform. Four coral cores from the fossil platform were dated using the radiocarbon and U-Th methods. The fossil corals range from 5.6±0.1 to 2.4±0.03 ka, constraining the initiation of the modern reef to 2,400 years ago at most. We documented the detailed morphology of the reef using aerial photographs and scuba diving. The survey shows that at its northern end, growth of the 2-km-long reef is inhibited by an active alluvial fan, and it is composed of isolated knolls that are just approaching the sea surface. Towards the south, the knolls are progressively larger and closer together, until they form a continuous reef platform. Along this north-to-south trend we follow the evolution of reef morphology, changes in coral distribution, and the development of a lagoon separated from the open sea. Based on these observations, we suggest a four-stage reef growth model: (a) the reef initiates as coral colonies, forms knolls, and begins to grow upward, limited by the sea surface. (b) Upon reaching the surface, the knolls spread laterally, preferentially parallel to the dominant wave direction assuming an elongated morphology. (c) Continued growth results in adjacent knolls eventually coalescing to form a continuous jagged reef. We interpret the spurs-and-grooves morphology that can be traced across the reef at Elat as remnants of the original trends of knolls. (d) While reef expansion continues, the original knoll trends may be obscured as a massive reef front takes shape. Considering reef growth rates and observations from the modern reef at Elat, this evolution scheme predicts an age range of 10³ years for corals on the reef platform. The range and distribution of radiometric ages we obtained from the fossil reef platform underlying the living Elat reef confirm this hypothesis.     

Molecular phylogeny of Pacific Island Colymbetinae: radiation of New Caledonian and Fijian species (Coleoptera, Dytiscidae)

We present a molecular phylogeny and taxonomic review of the Pacific island colymbetine diving beetles, focusing on the Fijian and New Caledonian faunas. Four new species are described: Rhantus monteithi and R. poellerbauerae from New Caledonia, and R. kini and R. bula from Fiji. We also describe the 3rd instar larvae of R. monteithi and R. poellerbauerae spp. nov., assigned to adults using mtDNA sequence data and discuss larval characters in the light of phylogeny. The phylogenetic hypotheses derived from both parsimony and Bayesian inference based on 3508 aligned nucleotides from a combination of mitochondrial (cox1, cob and rrnL‐tRNALeu‐Nad1) and nuclear genes (18S rRNA and H3) reveal a clade comprising R. novaecaledoniae, R. alutaceus, R. pseudopacificus, R. monteithi sp. nov. and R. poellerbauerae sp. nov., which agrees with the R. pacificus group sensu Balke (1993). Carabdytes upin was included within this clade, possibly indicating paraphyly of the genus Rhantus. Rhantus annectens, R. bacchusi, R. supranubicus, R. suturalis, R. simulans, and the Palearctic R. exsoletus, R. latitans and R. bistriatus formed a clade corresponding to the R. suturalis group sensu Balke (2001). Rhantus vitiensis, previously assigned to the R. pacificus group, was included in the R. suturalis clade. We find some support for a scenario where the Pacific was colonized out of the Northern hemisphere only during the past c. 12 million years, rejecting a Gondwanan origin of the morphologically isolated endemics. The new species are all characterized by mtDNA haplotype clusters, the degree of divergence between sister species pairs ranging from 1.3 to 7%, while R. novaecaledoniae individuals from all over New Caledonia apparently form one morphospecies, with moderate genetic diversity (up to 2.3% mtDNA divergence between populations). The sisters R. pollerbauerae sp. nov. + R. monteithi sp. nov. occur sympatrically on Mont Panié but appear ecologically segregated, while the sisters R. vitiensis + R. bula sp. nov. were encountered syntopically on Viti Levu. Comparing genetic and morphological data of Fijian Rhantus and Copelatus diving beetles, we here show that even in island radiations it is not per se possible to know if mitochondrial DNA barcoding would perform well (Rhantus: YES, Copelatus: NO). At the same time we show that fixed cutoff values, as sometimes used to discriminate between barcodes, thus species, might be meaningless. We underpin the importance of morphology for sustainable exploration of global diversity.     

Biology and geology of eastern Pacific coral reefs

Coral Reefs -  The tropical eastern Pacific region has historically been characterized as devoid of coral reefs. The physical conditions of the region are apparently not conducive to reef...     

Holocene emergence in the Cook Islands,South Pacific

There is evidence of Holocene emergence on several of the Cook Islands. On Suwarrow Atoll there are extensive outcrops of emergent, but truncated, reef on the northern atoll rim, radiocarbon-dated 4680–4310 years B. P., overlain by younger cemented boulder conglomerates. On the northeast of the atoll there are fossil algal ridges indicating up to 1 m of emergence; the landwardmost has been dated 4220 years B. P., the intermediate one 3420 years B. P. and the present one 1250 years B. P. On Mitiaro, a makatea island in the Southern Cooks, there are emergent reefal deposits in the centre of the reef flat dated 5140–3620 years B. P. Similar thought poorly preserved deposits occur on Mauke, and an erosional bench and notch occurs on Atiu. Emergence on all islands appears synchronous with that reported on Mangaia, where a relative fall of sea level of at least 1.7 m in the last 3400 years has been reported. The evidence for emergence is broadly similar to that described from French Polynesia, though timing of emergence appears to differ.     

Environmental factors influencing urchin spatial distributions on disturbed coral reefs (New Caledonia, South Pacific)

Few works have examined the relative contributions of habitat variables to the distribution of coral reef urchins. In the present study, the spatial distribution of two common urchin species (Diadema setosum and Echinometra mathaei) was studied in the fringing reefs of two urban bays in New Caledonia (South Pacific). Urchins were surveyed at 105 stations with contrasted habitat structure/anthropic disturbance levels; 32 environmental variables (water/sediment characteristics, reef structuring species) were considered. Moderate densities were generally observed at station scale (mean 0.5 individuals m^− 2). The combination of univariate and multivariate techniques highlighted patchy distributions for Diadema as well as Echinometra, with distinct species/habitat associations; environmental gradients occurring within the bays did not seem to influence the species patterns. For Diadema, the spatial variability was better explained by sediment type than by biotic cover; increasing densities occurred across habitats with larger sediment sizes and decreasing coral complexity/macrophytes cover. In contrast, the distribution of E. mathaei exhibited weak relationships with habitat variables. In coral reefs, small-scale heterogeneity may thus be responsible for most of urchins spatial variability.     

Symbiosis, fisheries and economic development on coral reefs

Life-history traits of commercially important species, physiological attributes of the framework species, and characteristics of ecosystem processes make coral reefs especially vulnerable to export of biomass. Organisms in ecosystems driven by upwelling and terrestrial nutrient input are more amenable to biomass yield. Nonexportive approaches to resource management, exemplified by Palau, are compatible with the attributes of coral-reef ecosystems; they satisfy to a greater degree the economic demands and pressures of growing human populations, and they provide motivation to manage.     

Anthropogenic impacts to coral reefs in Palau,western Micronesia during the Late Holocene

The Palauan archipelago contains one of the most ecologically diverse coral reef systems in the Indo-Pacific that was as attractive for humans prehistorically as it is today. New evidence is emerging that during the past few thousand years there has been increasing exploitation of coral reef resources, particularly finfish and mollusks, leading to a decline in taxa numbers, richness, and diversity in various locales. This paper examines the historical interactions between human populations and coral reef ecologies in Palau by combining known archaeological data and results from modern biological data of different reef fauna. The integration of these data sources provides a framework for attempting to explain variations in taxa composition between islands in the archipelago and how this may relate to human exploitation or other phenomena through time. By using this perspective to link past events with present-day conditions, we can gain a better sense of the extent to which anthropogenic changes may have affected island environments in western Micronesia during the Late Holocene. The study also illustrates the many difficulties researchers face in attempting to synthesize and explain past and present human predation behavior when using disparate sources of data.