Russell C. Babcock

Mass Spawning in Tropical Reef Corals

Synchronous multispecific spawning by a total of 32 coral species occurred a few nights after late spring full moons in 1981 and 1982 at three locations on the Great Barrier Reef, Australia. The data invalidate the generalization that most corals have internally fertilized, brooded planula larvae. In every species observed, gametes were released; external fertilization and development then followed. The developmental rates of externally fertilized eggs and longevities of planulae indicate that planulae may be dispersed between reefs.

Synchronous spawnings of 105 scleractinian coral species on the Great Barrier Reef

Following observations of mass spawning of hermatypic corals on the Great Barrier Reef in 1981 and 1982, spawning dates were successfully predicted and documented at five reefs on the Central and Northern Great Barrier Reef in 1983. During the predicted times, 105 species from 36 genera and 11 families were observed to spawn. Of these, 15 species were shown to have an annual gametogenic cycle. All but two of the species observed during mass spawnings shed gametes which underwent external fertilization and development. Synchronous spawning was observed both within and between the five reefs studied, which were separated by as much as 5° of latitude (500 km) or almost a quarter of the length of the Great Barrier Reef. The mass spawning of corals took place on only a few nights of the year, between the full and lastquarter moon in late spring. Maturation of gametes coincided with rapidly rising spring sea temperatures. Lunar and diel cycles may provide cues for the synchronization of gamete release in these species. The hour and night on which the greatest number of species and individuals spawned coincided with low-amplitude tides. Multispecific synchronous spawning, or “mass spawning”, of scleractinian and some alcyonacean corals represents a phenomenon which is, so far, unique in both marine and terrestrial communities.

Global warming and recurrent mass bleaching of corals

During 2015–2016, record temperatures triggered a pan-tropical episode of coral bleaching, the third global-scale event since mass bleaching was first documented in the 1980s. Here we examine how and why the severity of recurrent major bleaching events has varied at multiple scales, using aerial and underwater surveys of Australian reefs combined with satellite-derived sea surface temperatures. The distinctive geographic footprints of recurrent bleaching on the Great Barrier Reef in 1998, 2002 and 2016 were determined by the spatial pattern of sea temperatures in each year. Water quality and fishing pressure had minimal effect on the unprecedented bleaching in 2016, suggesting that local protection of reefs affords little or no resistance to extreme heat. Similarly, past exposure to bleaching in 1998 and 2002 did not lessen the severity of bleaching in 2016. Consequently, immediate global action to curb future warming is essential to secure a future for coral reefs.

A baited underwater video system for the determination of relative density of carnivorous reef fish

Estimates of the relative density of fishes form the basis of many marine ecological studies as well as the assessment of effects of fishing or pollution. Plasticity in the behavioural response of large reef fishes to SCUBA divers means that commonly used underwater visual census (UVC) techniques do not always provide reliable estimates of relative density. The paper describes the system configuration, deployment methods, testing and use of a remotely deployed baited underwater video (BUV) system for the survey of carnivorous reef fishes (snapper, Pagrus auratus and blue cod,Parapercis colias) in marine reserves of northern New Zealand. Concurrent UVC and BUV surveys inside and outside a marine reserve showed that, whereas UVC detected few snapper in either area (resulting in little confidence in statistically significant results), BUV demonstrated significant differences in relative density. Conversely, blue cod were found to occur at significantly higher densities within the reserve by UVC, but not by BUV. The provision of accurate estimates of fish size (<20 mm error) from video footage also illustrated differences in size structure between protected and fished populations. The data suggest that a combination of survey techniques is likely to be necessary where multispecies assemblages are being assessed.

Burdens of evidence and the benefits of marine reserves: putting Descartes before des horse?

An extensive literature has appeared since 1990 on the study of ‘no-take’ marine reserves and their potential to make significant contributions to the conservation and management of fisheries, especially in tropical environments (see Polunin 1990; Roberts & Polunin 1991; DeMartini 1993; Roberts 1997; Allison et al. 1998; Guenette et al. 1998). The literature describes many potential benefits of marine reserves to fisheries, including increases in spawner-biomass-per-recruit and increases in larval supply from protecting ‘source’ populations (Jennings 2000). The important word here is ‘potential’. Some claims made by advocates of marine reserves might be regarded as optimistic, whereas critics of reserves might sometimes have been unduly harsh. Conservation goals for marine reserves are often poorly defined, and differences of opinion regarding the efficacy of reserves for fulfilling any of their stated goals can frequently be attributed to a lack of good information with which to predict their effects. Here, we critically examine the literature from 1990–2001 to determine (1) the relative effort put into empirical and theoretical approaches to predict reserve effects, and (2) the quality of empirical evidence available to support theoretical predictions. It is not the purpose of this article to single out particular studies for criticism (although this is sometimes inevitable to provide examples), nor to draw conclusions concerning the efficacy of marine reserves.

Coral recruitment: consequences of settlement choice for early growth and survivorship in two scleractinians

Settlement, early survivorship and growth of two species of reef-building corals were studied in order to assess the importance of these processes in determining the distribution of adult corals. Experiments were conducted using larvae of Platygyra sinensis (Edwards and Haime), a shallow water species with a massive morphology, and Oxypora lacera (Verrill), a shade-loving or deep water species with a laminar morphology. Settlement orientations in experimental field enclosures varied according to depth, Oxypora choosing more cryptic microhabitats than Platygyra. Laboratory settlement experiments utilising different light intensities indicated that light level was the variable responsible for changes in settlement orientation with depth. Total numbers of larvae settled at a range of depths did not correspond with adult distribution for either species, though there were significant variations in settlement with depth. For juveniles of each species, variations in growth and survivorship with depth were inconsistent with adult distributions. These results, in combination with the settlement experiments, suggest that pre-settlement factors may play an important role in determining reef-scale distribution patterns. Settlement orientation on experimental substrata influenced growth rates, which were highly correlated with survivorship. In the first few months after settlement, mortality was highest on highly sedimented upper surfaces. However, growth and survivorship were highest on these upper surfaces during the following 5 months, presumably because of higher light levels there than on undersurfaces. There was no correlation between settlement density on experimental surfaces and subsequent survivorship. This may be due to the fact that the susceptibility of newly settled corals to different sources of mortality changes over time. No single settlement orientation provided a means to optimise survivorship through the course of these changes.

Larval development of certain gamete-spawning scleractinian corals

Embryogenesis and larval development were documented in 19 species of hermatypic scleractinians which release gametes during the summer coral spawning season on the Great Barrier Reef. Cleavage of fertilized eggs began approximately 2 h after spawning in all species, and gave rise to blastulae after 7–10 h. Endoderm formation in Platygyra sinensis was by invagination, and this appeared to occur in all species studied. All species observed at 36 h after spawing were mobile and full mobility was reached by 48 h. Settlement of planulae placed in aquaria occurred between 4 and 7 days after fertilization. These results suggest that larval corals produced by most gamete-releasing coral species are likely to be dispersed away from the parent reef.

Climate-driven regime shift of a temperate marine ecosystem

No turning back? Ecosystems over time have endured much disturbance, yet they tend to remain intact, a characteristic we call resilience. Though many systems have been lost and destroyed, for systems that remain physically intact, there is debate as to whether changing temperatures will result in shifts or collapses. Wernburg et al. show that extreme warming of a temperate kelp forest off Australia resulted not only in its collapse, but also in a shift in community composition that brought about an increase in herbivorous tropical fishes that prevent the reestablishment of kelp. Thus, many systems may not be resilient to the rapid climate change that we face. Science, this issue p. 169 Rapid warming tropicalizes a temperate kelp forest. Ecosystem reconfigurations arising from climate-driven changes in species distributions are expected to have profound ecological, social, and economic implications. Here we reveal a rapid climate-driven regime shift of Australian temperate reef communities, which lost their defining kelp forests and became dominated by persistent seaweed turfs. After decades of ocean warming, extreme marine heat waves forced a 100-kilometer range contraction of extensive kelp forests and saw temperate species replaced by seaweeds, invertebrates, corals, and fishes characteristic of subtropical and tropical waters. This community-wide tropicalization fundamentally altered key ecological processes, suppressing the recovery of kelp forests.

Experimental hybridization and breeding incompatibilities within the mating systems of mass spawning reef corals

Abstract. Synchronous spawning of many coral species that co-occur on Indo-Pacific reefs raises the possibility that hybridization plays a role in their evolution. Here we use experimental crosses to examine mating compatibilities and breeding barriers in a group of sessile animals whose mating systems are primarily governed by interactions among free-spawned gametes. We found hybridization occurs readily in more than one-third of 42 species pairs from the common genera Acropora, Montipora and Platygyra. Mean fertilization success ranged from 1% to 50% in species crosses, but standard deviations about these means were large and in some cases, fertilization success in individual colony matings was greater than 95%. Cases of high fertility in individual, interspecific matings were found in all three genera. Hybridization occurred most readily between species that were morphologically similar, identifying areas where current taxonomic judgements may require further testing. However, cases of significant hybridization also occurred between species that are morphologically distinct. Evidence of in vitro hybridization combined with the lack of either temporal or spatial barriers to interbreeding among field populations of these species, indicates that natural hybridization may occur commonly between congeneric corals that are currently recognized as distinct species. We also detected mating incompatibilities between some colonies within some species. In some cases, incompatible colonies corresponded to distinct morphotypes, but not in others. Thus some breeding groups in scleractinian corals are potentially larger, but others are smaller, than would be predicted using morphological criteria. Gamete incompatibilities within a morphospecies that readily hybridizes with other species may be the result of a mating system that is governed by gamete-level interactions. Imprecision in the alignment of morphological and breeding boundaries suggests a single species concept may not apply to scleractinian corals and challenges the tacit assumption that currently defined coral species encompass biological, evolutionary and phylogenetic species. Hybridization between supposedly isolated species introduces a reticulate nature to the evolution of corals and has profound implications for present understanding of the population genetics, phylogenetics, and evolutionary biology of scleractinian corals.

Spiny lobster, Jasus edwardsii, recovery in New Zealand marine reserves

The abundance, size, biomass and reproductive output of spiny lobsters, Jasus edwardsii, from replicated sites nested within four marine reserves and similar non-reserve locations in north-eastern New Zealand were compared. No time–series data were available from three of the reserves so the ages of the reserves (3–21 years) were used to infer temporal patterns of lobster population recovery. Linear models indicated that the mean density of the total lobster population increased 3.9 and 9.5% in shallow ( 10 m depth), respectively, for each year in which the reserves were established, while the mean size of lobsters was estimated to increase by 1.14 mm per year of protection. As a consequence lobster biomass (kg/500 m−2) was conservatively estimated to increase by 5.4% per year of protection in shallow sites and 10.9% per year of protection in the deep sites and egg production (eggs/500 m−2) by 4.8 and 9.1% per year of protection for shallow and deep sites respectively.