Stable isotope evidence of benthic microalgae-based growth and secondary production in the suspension feeder Cerastoderma edule (Mollusca,Bivalvia) in the Marennes-Oléron Bay

The contribution of natural food sources to the growth and secondary production of the suspension feeding bivalve Cerastoderma edule (L.) was estimated under field conditions in the Marennes-Oléron Bay (Atlantic coast, France). Monthly estimates of abundance, biomass and cockle growth were combined with seasonal analyses of ¹³C and ¹⁵N ratios of juvenile and adult cockles, together with their potential food sources [i.e. suspended particulate organic matter (POM), microphytobenthos, macroalgae and seagrass] sampled at mid-tide level in a muddy sandflat. Adult cockles grew mainly in spring, whereas juveniles grew in summer and autumn, following spat recruitment in early summer. Total annual production and elimination of cockles were estimated to be 32.5 and 34.7 g AFDW m^–2 yr^–1. Relative contributions of each year class to production were ca 40, 41, 11 and 6% for 0-group, 1-, 3- and 4-yr-old cockles in 1995, respectively. Quantitative assessment of proportions of food sources to the annual secondary production of cockles was obtained by using a simple carbon isotope-mixing model with microphytobenthos (¹³C = –16.0±0.6) and POM (¹³C = –22.2±1.1) as end-members. On average, more than 70% of the total annual cockle production originated from microphytobenthos, with a much higher contribution for the 0-group (88%) than for adult cockles (60%). The between-age difference was induced mainly by changes in the availability of food resources (benthic versus planktonic) during the non-synchronous growing seasons of juvenile and adult cockles.     

Geographic Variations in Dorsal and Anal Ray Counts of Juvenile Japanese Flounder, Paralichthys olivaceus, in the Japan Sea

Meristic counts of early and late wild settled juveniles of Japanese flounder, Paralichthys olivaceus (Paralichthyidae), in Wakasa Bay, Japan, were compared, with specimens collected from 26 sites spread along ca. 1700km of coastline facing the Japan Sea. Mean dorsal and anal ray counts of the early settled group at Kyoto were significantly larger than those of the late settled group. A discontinuous geographic boundary in mean dorsal and anal ray counts was found around Wakasa Bay and the Noto Peninsula with both means significantly larger in the southern group than in the northern group. Mean ray counts of the early and late settlers at Kyoto were similar to those of the southern and northern groups, respectively. The effect of water temperature on meristic characters was tested on two groups of laboratory-reared juveniles. Mean dorsal and anal ray counts were larger in juveniles reared at higher water temperatures. The early and late settler groups were estimated to hatch in late February and late April, respectively, representing negative response of meristic characters to water temperatures if these two groups hatched out in Wakasa Bay. Differences in the dorsal and anal ray counts between the early and late settled groups at Kyoto can, therefore be attributed to genotypic, not phenotypic variation. This suggests the possibility of transport of larvae of the early group from areas further south to Wakasa Bay by the warm Tsushima Current, a branch of the Kuroshio, which flows northeastward along the coast of the Japan Sea, particularly when the temperature gradation between the south and north areas during these seasons is considered.     

The occurrence and behaviour of phosphate fractions in Izmir Bay, Aegean Sea

The area around Izmir Bay (Turkey) is heavily urbanized and receives, therefore, high concentrations of phosphate originating from industrial and municipal inputs. During the surveys between April 1993 and July 1994, the total phosphate concentrations were highest in the Inner Bay (6.45 M and 5.59 M in the surface and bottom water, respectively) where very dense anthropogenic pollution occurs. The total phosphate value gradually decreased towards the Outer Bay where 0.70 M and 1.18 M were found in the surface and bottom water, respectively. The distribution of dissolved inorganic, dissolved organic and particulate phosphate along the bay reflected some peculiar spatial and temporal patterns. A high percentage of dissolved organic phosphate was observed in the Outer Bay while the particulate phosphate peaked in the Middle Bay where an upwelling mechanism was observed. In the bay, the biological production was strongly correlated with the variations in the dissolved inorganic, organic and particulate phosphate. The high phosphate concentration in particles caused the particulate phosphate formed in the Inner Bay to be transported to the outer parts of the bay because of the short water residence time. On the other hand, Principal Component Analysis showed that about 35% of the variation in all variables measured were related to the total phosphate, total dissolved phosphate, dissolved inorganic phosphate and particulate phosphate together with ammonium and reactive-Fe while about 14% of the variation was related to the dissolved organic phosphate and the number of phytoplankton cells, chl-a, pH and O₂.     

Contribution of Ciliated Microprotozoans and Dinoflagellates to the diet of three Copepod species in the Bay of Biscay

Predation of three calanoid copepods (Calanus helgolandicus, Temora longicornis and Centropages chierchiae) on phytoplankton, dinoflagellates and ciliates was estimated in the Gironde estuarine plume (Bay of Biscay) during winter by means of in situ incubations. Both phytoplankton and ciliates were part of the diet of those three species, while only Centropages chierchiae also included a significant portion of dinoflagellates in its diet. The clearance rates of Calanus helgolandicus for ciliates and phytoplankton reached 2.8 and 4.0 ml copepod^–1 h^–1, respectively, those of Temora longicornis were 3.2 and 1.8 ml copepod^–1 h^–1, and those of Centropages chierchiae were 4.3 and 0.8 ml copepod^–1 h^–1.Neither Calanus helgolandicus nor Temora longicornis selected dinoflagellates, given the low clearance rates measured for this prey category (0.05 and 0.03 ml copepod^–1 h^–1, respectively). By contrast, Centropages chierchiae included dinoflagellates in its diet, with a clearance rate of 4.9 ml copepod^–1 h^–1. Within a given prey category (ciliates or dinoflagellates), all three copepods selected larger prey types (>40 m) over smaller ones (40 m). This implies a better detection and capture of larger motile prey compared to small ones. The results are discussed with regard to the omnivorous feeding behavior of these copepods observed here, during a late winter phytoplankton bloom.     

LONG-TERM TRENDS IN HARBOR SEAL NUMBERS AT TUGIDAK ISLAND AND NANVAK BAY, ALASKA

We conducted land‐based counts of harbor seals (Phoca vitulina richardii) and collected related environmental data at Tugidak Island (Gulf of Alaska, 1994–2000) and Nanvak Bay (Bristol Bay, 1990–2000) to estimate population trends and identify factors influencing counts. At Tugidak Island, the seal population declined substantially during molting from 1976 through the 1980s, stabilized in the early 1990s, and increased at a moderate rate (3.4%/yr, CI: 1.0%–5.8%) from 1994 to 2000. Pups and all seals ashore during pupping increased at higher annual rates of 5.4% (CI: 2.2%–8.8%) and 8.3% (CI: 4.5%–12.3%) from 1994 to 2000 at Tugidak Island. At Nanvak Bay seals declined in abundance between 1975 and 1990 but increased during the 1990s at 9.2%/yr (CI: 7.2%–11.3%) during pupping and 2.1%/yr (CI: 0.6%–3.6%) during molting. Date and time‐of‐day were significant covariates in all analyses. Factors that led to declines at Tugidak Island and Nanvak Bay have seemingly abated sufficiently such that these populations are currently increasing, though still greatly reduced from the 1970s. Index sites are useful adjuncts to aerial surveys, providing survey‐related information not always available from aerial counts, which is useful in survey design and data analysis.     

Effects of elevated pCO2 on epilithic and endolithic metabolism of reef carbonates

We investigated effects of elevated partial pressure of CO₂ (pCO₂) on the metabolism of epilithic and endolithic phototrophic communities that colonized experimental coral blocks. Blocks of the massive coral Porites lobata were exposed to colonization by epilithic and endolithic organisms at an oceanic site in Kaneohe Bay (Hawaii) for 6 months, and then were transported to laboratory tanks. A bubbling system was used to maintain two treatments for 3 months, one at ambient pCO₂ (400 ppm) and the second at elevated pCO₂ (750 ppm). Net photosynthetic rates of epilithic communities in the high pCO₂ treatment, dominated by encrusting coralline algae, decreased by 35% while respiration rates remained constant. In contrast, metabolism of endolithic phototrophs, comprised of cyanobacteria and algae, was not significantly affected by the elevated pCO₂ even though endoliths contributed about 63% to block production.     

Dietary composition of black drum Pogonias cromis in a hypersaline estuary reflects water quality and prey availability

The Baffin Bay estuary is a hypersaline system in the Gulf of Mexico that supports an important recreational and commercial fishery for black drum Pogonias cromis, a benthic predator. Seasonal measurements of water quality variables, benthic macrofauna densities and biomass, and determination of P. cromis food sources using stomach‐content and stable‐isotope analyses were carried out to determine how P. cromis food sources change with water quality and how this may affect P. cromis diet. Gut‐content analysis indicated P. cromis selectively consumed bivalves Mulinia lateralis and Anomalocardia auberiana. Isotope compositions demonstrated that P. cromis relied on these benthic food resources produced in the Baffin Bay estuary year‐round. Biomass and densities of these bivalves were influenced by changes in water quality variables, particularly salinity and dissolved oxygen. Thus, this paper demonstrates the relationship between water quality variables, benthic macrofauna, and their use as food resources by a carnivorous fish species, and emphasizes the need for integrated assessments when studying the effects of water quality on ecosystem function. Holistic approaches such as these can provide important information for management and conservation of fishery resources and can improve predictions of ecosystem response to climate variability.     

基于土地利用变化和生态系统服务的海岸带生态安全综合评价——以胶州湾为例

以土地利用为主的陆域开发活动能改变近海环境质量,并影响和改变原有海岸带生态系统服务功能的供给模式,对海岸带生态安全产生一定的负面影响.目前在海岸带生态系统研究领域较多采用陆地生态系统研究模式,未能真正体现海岸带作为海陆结合的独立的环境体系的特点,并缺乏对陆域活动驱动与生态系统服务功能响应和生态安全实现之间复杂关系的科学解释.本研究基于海岸带生态系统服务的空间异质性和流动性特点,以“土地利用变化(LUCC)-生态系统服务(ES)-生态系统安全”为研究主线,构建海岸带生态安全评价模型,探讨以土地覆被变化为主的陆域活动对海岸带生态系统服务功能和区域生态安全的影响机理及其时空变异规律.从模型的评价结果上看,作为生态安全系统中主要压力表征的胶州湾陆域土地利用变化,与相应海域内的生态系统服务状况和生态安全状态呈现出一定的相关性和趋势性.随着环胶州湾地区城市化进程中大量用地流转为城乡建设用地,胶州湾中相应海域的生态系统服务状态下降,进而带来该海域生态安全状态恶化.本文所提出的基于压力-状态-响应(PSR)框架的海陆结合的生态安全评价模型,以探讨陆域活动对海岸带生态系统服务功能和区域生态安全的影响及其时空变异规律为目的,可以克服目前研究中只关注陆域部分而忽视陆域活动与海域部分之间的联系和相互影响的缺陷,对海岸带生态安全评价研究具有一定的改进作用.     

A significant range extension and sanctuary for the rare Open Bay Island skink (Oligosoma taumakae)

Abstract

The Open Bay Island skink (Oligosoma taumakae) is one of New Zealand's rarest lizard species. Until 2010, it was known only from two small islands in the Open Bay Island Group, a Māori-owned wildlife sanctuary in South Westland, New Zealand. Skinks on these islands are threatened by predation from weka (Gallirallus australis), a flightless native rail thought to have been introduced to the Open Bay Islands c. 100 years ago. Here, we describe the discovery of Open Bay Island skinks on two vegetated rock stacks located off the coast of Barn Bay, 52 km southwest of the Open Bay Islands. Although small (c. 0.10 and 0.36 ha), the Barn Islands appear to be predator-free, providing an important sanctuary for the skinks. We recommend: (1) a survey of mainland sites with suitable habitat; and (2) an evaluation of the need for island biosecurity measures for detecting and responding to incursions of small mammals.