Semper's (zoanthid) larvae: pelagic life,parentage and other problems

Semper's larvae were obtained from <300 out of 1800 plankton tows taken in the world's oceans (1964–1993). Zoanthellae (larvae of Sphenopidae) occurred at 217 stations and zoanthinae (larvae of Zoanthidae) at 86, the two larval types showing distributions clearly delimited by a minimum sea temperature (22 °C for zoanthellae, 18 °C for zoanthinae; a statistically significant difference, P<0.001). Length of formalin-fixed zoanthellae was 2–8.6 mm and of zoanthinae 1.5–5.9 mm. Endodermal zooxanthellae were present in 9/24 zoanthinae but in no zoanthellae (of 19). Three larvae contained an endo-commensal/parasitic amphipod. Septa were externally visible in larger zoanthinae and were counted in transverse sections of other larvae, a majority of which (both kinds) had 12 septa, the normal maximum. The pattern was brachycnemic in 40/43 larvae and anomalous (but non-macrocnemic) in three. If macrocnemic genera reproduce by Semper's larvae, they should have been represented in such a large sample. The distribution of adult Epizoanthus was examined: many species are deep sea (recorded down to 5000 m) but shallow-water species are relatively plentiful in, for example, the Adriatic and North Seas. No Semper's larva has ever been recorded from either. Some Parazoanthus species also occur in shallow water, especially associated with western Atlantic reef sponges. If they produce Semper's larvae, these have never been found. It is probable that macrocnemic zoanthids settle from planulae that do not develop into recognizable zoanthellae or zoanthinae.     

The impact of seawater saturation state and bicarbonate ion concentration on calcification by new recruits of two Atlantic corals

Rising concentrations of atmospheric CO₂ are changing the carbonate chemistry of the oceans, a process known as ocean acidification (OA). Absorption of this CO₂ by the surface oceans is increasing the amount of total dissolved inorganic carbon (DIC) and bicarbonate ion (HCO₃ ⁻) available for marine calcification yet is simultaneously lowering the seawater pH and carbonate ion concentration ([CO₃ ²⁻]), and thus the saturation state of seawater with respect to aragonite (Ω_ar). We investigated the relative importance of [HCO₃ ⁻] versus [CO₃ ²⁻] for early calcification by new recruits (primary polyps settled from zooxanthellate larvae) of two tropical coral species, Favia fragum and Porites astreoides. The polyps were reared over a range of Ω_ar values, which were manipulated by both acid-addition at constant pCO₂ (decreased total [HCO₃ ⁻] and [CO₃ ²⁻]) and by pCO₂ elevation at constant alkalinity (increased [HCO₃ ⁻], decreased [CO₃ ²⁻]). Calcification after 2 weeks was quantified by weighing the complete skeleton (corallite) accreted by each polyp over the course of the experiment. Both species exhibited the same negative response to decreasing [CO₃ ²⁻] whether Ω_ar was lowered by acid-addition or by pCO₂ elevation—calcification did not follow total DIC or [HCO₃ ⁻]. Nevertheless, the calcification response to decreasing [CO₃ ²⁻] was nonlinear. A statistically significant decrease in calcification was only detected between Ω_ar = <2.5 and Ω_ar = 1.1–1.5, where calcification of new recruits was reduced by 22–37% per 1.0 decrease in Ω_ar. Our results differ from many previous studies that report a linear coral calcification response to OA, and from those showing that calcification increases with increasing [HCO₃ ⁻]. Clearly, the coral calcification response to OA is variable and complex. A deeper understanding of the biomineralization mechanisms and environmental conditions underlying these variable responses is needed to support informed predictions about future OA impacts on corals and coral reefs.     

Calcification by juvenile corals under heterotrophy and elevated CO2

Ocean acidification (OA) threatens the existence of coral reefs by slowing the rate of calcium carbonate (CaCO₃) production of framework-building corals thus reducing the amount of CaCO₃ the reef can produce to counteract natural dissolution. Some evidence exists to suggest that elevated levels of dissolved inorganic nutrients can reduce the impact of OA on coral calcification. Here, we investigated the potential for enhanced energetic status of juvenile corals, achieved via heterotrophic feeding, to modulate the negative impact of OA on calcification. Larvae of the common Atlantic golf ball coral, Favia fragum, were collected and reared for 3 weeks under ambient (421 μatm) or significantly elevated (1,311 μatm) CO₂ conditions. The metamorphosed, zooxanthellate spat were either fed brine shrimp (i.e., received nutrition from photosynthesis plus heterotrophy) or not fed (i.e., primarily autotrophic). Regardless of CO₂ condition, the skeletons of fed corals exhibited accelerated development of septal cycles and were larger than those of unfed corals. At each CO₂ level, fed corals accreted more CaCO₃ than unfed corals, and fed corals reared under 1,311 μatm CO₂ accreted as much CaCO₃ as unfed corals reared under ambient CO₂. However, feeding did not alter the sensitivity of calcification to increased CO₂; ? calcification/?Ω was comparable for fed and unfed corals. Our results suggest that calcification rates of nutritionally replete juvenile corals will decline as OA intensifies over the course of this century. Critically, however, such corals could maintain higher rates of skeletal growth and CaCO₃ production under OA than those in nutritionally limited environments.     

Planulation patterns of the brooding coral <Emphasis Type="Italic">Favia</Emphasis> <Emphasis Type="Italic">fragum</Emphasis> (Esper) in Bermuda

Planulation by Favia fragum at the high-latitude reef of Bermuda was examined during July and August of 2004–2007. In 2004 and 2005, observations were extended to June and September; however, planulation only occurred in July and August, when temperatures were increasing toward and during the annual high. Planulation peaked 6–12 days after the new moon, corresponding to the pattern found for F. fragum in the Caribbean. Mean monthly fecundity was also similar to that found in the Caribbean; however, annual and monthly fecundity were variable, being lowest in July 2005, which coincided with lowest mean SST. These results indicate that although fecundity and lunar timing of planulation by F. fragum are not affected by latitude, reproductive seasonality may be shorter at high-latitude reefs. Understanding reproductive events at latitudinal extremes gives insight to environmental controls on coral reproduction, which will aid in future management and restoration efforts.     

Effect of seawater temperature on reproductive seasonality and fecundity of Pseudoplexaura porosa (Cnidaria: Octocorallia): latitudinal variation in Caribbean gorgonian reproduction

Abstract. The majority of tagged colonies of Pseudoplexaura porosa in Bermuda were reproductive over 2 months in the summer. They spawned 5–8 d after the full moon, with a peak on the sixth day, similar to colonies in Panama. The months of spawning were August and September in 1998, but July and August in 1999 and 2000. This temporal difference between the months of spawning corresponded to inter-annual variations in seawater temperature profiles. Initial gamete development each year occurred only when the daily mean seawater temperature during the month before spawning exceeded 27°C. There was a significant positive relationship between reproductive effort (gamete volume) of colonies and rising seawater temperature in the month preceding spawning; this was true for both the initial and the second spawning months. The end of the reproductive season each year was triggered by the decline in seawater temperature past the summer maximum. The duration of the reproductive season of conspecifics at the central Caribbean reef of Panama is 2 months longer than in Bermuda. This can be explained by the smaller annual temperature range at the lower latitude and the earlier onset of temperatures favorable for gamete development. Fecundity estimates for members of P. porosa (mean oocyte and spermary densities) in Bermuda were lower than for conspecifics in Panama. The shorter reproductive season in Bermuda, in addition to the lower fecundity of colonies, indicates that reproduction in P. porosa is compromised at this high latitude reef.