Abstract:Zooplankton were 3-8 times more abundant during the day near the surface than elsewhere in the water column over a 1-2.4 m deep back reef in Moorea, French Polynesia. Zooplankton were also significantly more abundant near the surface at night although gradients were most pronounced under moonlight. Zooplankton in a unidirectional current became concentrated near the surface within 2 m of departing a well-mixed trough immediately behind the reef crest, indicating that upward swimming behavior, rather than near-… Show more
“…data), we hypothesize that the approximate coincidence of wave-forced, cross-reef transport and acroporid reproduction produces elevated recruitment along the southwest shore. Thus, the back reef of Moorea is affected by seasonally variable cross-reef transport of offshore water (Hench et al 2008), which transports zooplankters over the reef crest and into the lagoon (Alldredge & King 2009). This flow would also transport coral larvae when coral reproduction is coincident with powerful waves, and influence thermal heterogeneity within the back reef as cross-reef transport varies in intensity.…”
Section: Discussionmentioning
confidence: 99%
“…This flow would also transport coral larvae when coral reproduction is coincident with powerful waves, and influence thermal heterogeneity within the back reef as cross-reef transport varies in intensity. Although we did not measure the transport of coral larvae across the reef crest and, in fact, coral larvae were not found in one recent study that assessed the flux of zooplankton across the reef crest in Moorea (Alldredge & King 2009), the presence of juvenile colonies of outer reef corals (e.g. Pocillopora eydouxi and Astreopora myriophthalma) behind the reef crest in some locations suggests that the delicate coral larvae can pass over the reef crest, settle, and grow into new recruits (P. J. Edmunds pers.…”
In this study, we describe spatio-temporal variation in coral recruitment in the back reef of Moorea, French Polynesia, and explore the extent to which it is associated with community structure, seawater temperature, and wave regimes. Recruitment was assessed with settlement tiles deployed at 10 sites on the north, southeast, and southwest shores and sampled every 5 to 7 mo from 2005 to 2007. Temperature and waves were measured using thermistors and pressure sensors, and community structure was assessed using in situ surveys. Mean recruitment varied from 0 to 6 recruits tile -1 (510 cm 2 ) and was generally greater in the second compared to the first year of the study. Recruitment varied among sites, and this variation was similar between years but differed among sampling periods: acroporids were common on the southwest shore between January and September, but rare from September to January; poritids were common on the north shore between September and January, but rare on the southwest shore from January to September; and pocilloporids were found all year, but at slightly elevated densities between January and September. The mean daily seawater temperature, and the daily range, varied among sites, but neither was closely related to coral recruitment, and both were of biologically small magnitudes. The coral community structure also varied among sites, but likewise, was not associated with coral recruitment. In contrast, outer reef wave energy exposure, which likely played an important role in driving cross-reef transport of seawater into the lagoon, differed between shores and seasons in a pattern consistent with the variation in coral recruitment in the back reef. We hypothesize that coral recruitment in the back reef of Moorea is influenced by the interaction of seasonal variation in wave exposure, family-level differences in coral reproductive timing, and the spatial distribution of adult corals.
“…data), we hypothesize that the approximate coincidence of wave-forced, cross-reef transport and acroporid reproduction produces elevated recruitment along the southwest shore. Thus, the back reef of Moorea is affected by seasonally variable cross-reef transport of offshore water (Hench et al 2008), which transports zooplankters over the reef crest and into the lagoon (Alldredge & King 2009). This flow would also transport coral larvae when coral reproduction is coincident with powerful waves, and influence thermal heterogeneity within the back reef as cross-reef transport varies in intensity.…”
Section: Discussionmentioning
confidence: 99%
“…This flow would also transport coral larvae when coral reproduction is coincident with powerful waves, and influence thermal heterogeneity within the back reef as cross-reef transport varies in intensity. Although we did not measure the transport of coral larvae across the reef crest and, in fact, coral larvae were not found in one recent study that assessed the flux of zooplankton across the reef crest in Moorea (Alldredge & King 2009), the presence of juvenile colonies of outer reef corals (e.g. Pocillopora eydouxi and Astreopora myriophthalma) behind the reef crest in some locations suggests that the delicate coral larvae can pass over the reef crest, settle, and grow into new recruits (P. J. Edmunds pers.…”
In this study, we describe spatio-temporal variation in coral recruitment in the back reef of Moorea, French Polynesia, and explore the extent to which it is associated with community structure, seawater temperature, and wave regimes. Recruitment was assessed with settlement tiles deployed at 10 sites on the north, southeast, and southwest shores and sampled every 5 to 7 mo from 2005 to 2007. Temperature and waves were measured using thermistors and pressure sensors, and community structure was assessed using in situ surveys. Mean recruitment varied from 0 to 6 recruits tile -1 (510 cm 2 ) and was generally greater in the second compared to the first year of the study. Recruitment varied among sites, and this variation was similar between years but differed among sampling periods: acroporids were common on the southwest shore between January and September, but rare from September to January; poritids were common on the north shore between September and January, but rare on the southwest shore from January to September; and pocilloporids were found all year, but at slightly elevated densities between January and September. The mean daily seawater temperature, and the daily range, varied among sites, but neither was closely related to coral recruitment, and both were of biologically small magnitudes. The coral community structure also varied among sites, but likewise, was not associated with coral recruitment. In contrast, outer reef wave energy exposure, which likely played an important role in driving cross-reef transport of seawater into the lagoon, differed between shores and seasons in a pattern consistent with the variation in coral recruitment in the back reef. We hypothesize that coral recruitment in the back reef of Moorea is influenced by the interaction of seasonal variation in wave exposure, family-level differences in coral reproductive timing, and the spatial distribution of adult corals.
“…The description of three-domain spatial patterns within marine microbial communities in the context of the oceanic waters surrounding the coral reef ecosystem of Moorea is a key step in understanding the diversity and stability of planktonic microbial populations between coastal and open water oligotrophic ecosystems. The barrier reef system surrounding Moorea's Paopao Bay and adjacent lagoons has been the subject of several long-term biological (Adjeroud and Salvat, 1996;Adjeroud, 2000;Adjeroud et al, 2002;Penin et al, 2007;Alldredge and King, 2009), biogeochemical and oceanographic (Schrimm et al, 2004;Hench et al, 2008) research studies, though this study and a parallel report (Nelson et al, 2011) are the first to describe this ecosystem's microbial populations, this report being the first one to do so across all three domains of microbial life. A companion study recently demonstrated strong spatial patterns in dissolved organic carbon, bacterioplankton densities and bacterial community structure between and among the inshore and offshore habitats (Nelson et al 2011).…”
The Moorea Coral Reef Long Term Ecological Research (LTER) Site (17.501S, 149.831W) comprises the fringe of coral reefs and lagoons surrounding the volcanic island of Moorea in the Society Islands of French Polynesia. As part of our Microbial Inventory Research Across Diverse Aquatic LTERS biodiversity inventory project, we characterized microbial community composition across all three domains of life using amplicon pyrosequencing of the V6 (bacterial and archaeal) and V9 (eukaryotic) hypervariable regions of small-subunit ribosomal RNA genes. Our survey spanned eight locations along a 130-km transect from the reef lagoon to the open ocean to examine changes in communities along inshore to offshore gradients. Our results illustrate consistent community differentiation between inshore and offshore ecosystems across all three domains, with greater richness in all domains in the reef-associated habitats. Bacterial communities were more homogenous among open ocean sites spanning 4100 km than among inshore sites separated by o1 km, whereas eukaryotic communities varied more offshore than inshore, and archaea showed more equal levels of dissimilarity among subhabitats. We identified signature communities representative of specific geographic and geochemical milieu, and characterized co-occurrence patterns of specific microbial taxa within the inshore ecosystem including several bacterial groups that persist in geographical niches across time. Bacterial and archaeal communities were dominated by few abundant taxa but spatial patterning was consistent through time and space in both rare and abundant communities. This is the first in-depth inventory analysis of biogeographic variation of all three microbial domains within a coral reef ecosystem.
“…Conceivably, competition between photosynthesis and calcification for limited HCO 3 -could impact F v /F m in a pattern dependent on flow and temperature (as in massive Porites; Edmunds & Lenihan 2010), although evidence from Stylophora pistillata suggests this might only occur at very low concentrations of HCO 3 -1 (Furla et al 2000). Flow can impact corals in more ways than mass transfer alone, and on the reef the patterns implicating flow that were detected in a microcosm study would likely be modified through the roles of water motion in modulating the fluxes of zooplanktivorous food (Alldredge & King 2009) and particle capture rates (Sebens et al 1998).…”
Section: Discussionmentioning
confidence: 99%
“…These coral structures, referred to as 'bommies', can reach > 3 m diameter and > 2 m height, and are often colonized by smaller branching corals, other invertebrates, and algae. In a recent demographic survey of branching corals in the back reef of Moorea, we found that growth and survival of juvenile Pocillopora verrucosa (colonies < 40 mm diameter) was higher on bommies compared with the adjacent seafloor, because bommies provide access to increased water flow (Lenihan et al 2008), a greater flux of zooplankton (Alldredge & King 2009), and reduced rates of sedimentation (Lenihan et al 2008). We have found only minor differences in temperature and light between the seafloor and the tops of bommies in this location (Lenihan et al 2008), and differences in these factors are probably not responsible for the observed differences in coral performance on these 2 substrate types.…”
) and fish predation (predators versus no predators), but not temperature, supported results of the microcosm experiment. Growth was greatest for corals in the high-flow, no predator treatment, and relatively high for injured corals in low flow. Together, these results suggest that P. verrucosa, a common branching coral, prioritizes overall growth over repair when injured by fish feeding, which differs from the outcome observed in a companion study in which juvenile colonies of massive Porites were subjected to similar injuries.
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