Variable responses within epiphytic and benthic microalgal communities to nutrient enrichment

We evaluated how changes in nutrient supply altered the composition of epiphytic and benthic microalgal communities in a Thalassia testudinum (turtle grass) bed in Florida Bay. We established study plots at four sites in the bay and added nitrogen (N) and phosphorus (P) to the sediments in a factorial design. After 18, 24, and 30 months of fertilization we measured the pigment concentrations in the epiphytic and benthic microalgal assemblages using high performance liquid chromatography. Overall, the epiphytic assemblage was P-limited in the eastern portion of the bay, but each phototrophic group displayed unique spatial and temporal responses to N and P addition. Epiphytic chlorophyll a, an indicator of total microalgal load, and epiphytic fucoxanthin, an indicator of diatoms, increased in response to P addition at one eastern bay site, decreased at another eastern bay site, and were not affected by P or N addition at two western bay sites. Epiphytic zeaxanthin, an indicator of the cyanobacterial/coralline red algae complex, and epiphytic chlorophyll b, an indicator of green algae, generally increased in response to P addition at both eastern bay sites but did not respond to P or N addition in the western bay. Benthic chlorophyll a, chlorophyll b, fucoxanthin, and zeaxanthin showed complex responses to N and P addition in the eastern bay, suggesting that the benthic assemblage is limited by both N and P. Benthic assemblages in the western bay were variable over time and displayed few responses to N or P addition. The contrasting nutrient limitation patterns between the epiphytic and benthic communities in the eastern bay suggest that altering nutrient input to the bay, as might occur during Everglades restoration, can shift microalgal community structure, which may subsequently alter food web support for upper trophic levels.     

Variation in soil phosphorus, sulfur, and iron pools among south Florida wetlands

To determine relationships between soil nutrient status and known gradients in primary production, we collected and analyzed soils from 17 LTER sampling sites along two transects through south Florida wetland ecosystems. Through upstream freshwater marsh, a middle reach including the oligohaline marsh/mangrove ecotone, and downstream estuarine habitats, we observed systematic variation in soil bulk density, organic content, and pools of phosphorus (P), inorganic sulfur, and extractable iron. Consistent with observed differences in wetland productivity known to be limited by P availability, total P averaged ~200 μg g dw⁻¹ in soils from the eastern Taylor Slough/Panhandle and was on average three times higher in soils from the western Shark River Slough. Along both transects, the largest pool of phosphorus was the inorganic, carbonate-bound fraction, comprising 35–44% of total P. Greater than 90% of the total inorganic sulfur pool in these south Florida wetland soils was extracted as pyrite. Freshwater marsh sites typically were lower in pyrite sulfur (0.2–0.8 mg g dw⁻¹) relative to marsh/mangrove ecotone and downstream estuary sites (0.5–2.9 mg g dw⁻¹). Extractable iron in freshwater marsh soils was significantly higher from the Taylor Slough/Panhandle transect (3.2 mg g dw⁻¹) relative to the western Shark River Slough transect (1.1 mg g dw⁻¹), suggesting spatial variation in sources and/or depositional environments for iron. Further, these soil characteristics represent the collective, integrated signal of ecosystem structure, so any long-term changes in factors like water flow or water quality may be reflected in changes in bulk soil properties. Since the objective of current Everglades restoration initiatives is the enhancement and re-distribution of freshwater flows through the south Florida landscape, the antecedent soil conditions reported here provide a baseline against which future, post-restoration measurements can be compared.     

Mark‐resight abundance and survival estimation of Indo‐Pacific bottlenose dolphins,Tursiops aduncus,in the Swatch‐of‐No‐Ground,Bangladesh

A mark‐resight analysis under Pollock's robust design was applied to Indo‐Pacific bottlenose dolphins Tursiops aduncus in the Swatch‐of‐No‐Ground (SoNG) submarine canyon, Bangladesh, during the winter seasons of 2005–2009. Information from sightings of photo‐identified individuals (1,144) and unmarked individuals generated abundance estimates of 1,701 (95% confidence interval [CI]= 1,533–1,888), 1,927 (95% CI = 1,851–2,006), 2,150 (95% CI = 1,906–2,425), and 2,239 (95% CI = 1,985–2,524) individuals for seasons 1–4, respectively. This makes the population among the largest assessed of the species. Overall apparent survival was estimated as 0.958 (95% CI = 0.802–0.992). Interseasonal probabilities of transitioning to an unobservable state were estimated as 0.045, 0.363, and 0.300 for years 1–2, 2–3, and 3–4, respectively, and the overall probability of remaining in an unobservable state was 0.688. These probabilities, together with an apparent increase in abundance during the study period, indicate that the identified dolphins are part of a larger superpopulation moving throughout a more extensive geographic area. Of the photo‐identified dolphins, 28.2% exhibited injuries related to entanglements with fishing gear. This implies a strong potential for fatal interactions that could jeopardize the conservation status of the population, which otherwise appears favorable.     

A Report of the James Watson Lecture at Yale University

In March 2012, Nobel Prize winner James Watson gave a seminar at Yale University entitled “Driven by Ideas.” In his lecture, Watson discussed his personal vision for the future of science, specifically addressing how the scientific community should approach developing anticancer agents. He discussed the use of glycolytic inhibitors as anticancer agents due to the Warburg effect, as well as the benefits of metformin and anti-inflammatory drugs to help prevent cancer. He also compared drugs that target cell proliferation instead of targeting cell growth. Additionally, Watson commented on the mechanisms for how research should be conducted in the laboratory.     

The emergence of Cochlodinium along the California Coast (USA)

A sudden and nearly synchronous emergence of the red tide forming dinoflagellate Cochlodinium along more than 800 km of California coastline was initially observed in late summer 2004. Thereafter high cell concentrations have been detected on an annual basis. Here, we present quantitative and semi-quantitative data indicating that Cochlodinium was uncommon in the phytoplankton community in California prior to 2004 and is now persisting as a more regular component and one that seasonally can cause red tides. The quantitative portion of this study was primarily conducted in Monterey Bay, where cell densities reached at least 6 × 10⁴ cells L⁻¹ during the initial outbreak. A semi-quantitative comparison of California coastal counties by the California Department of Health Services (CDHS) was also made: of the 15 counties surveyed (most with multiple sites per county), cells were detected only from Los Angeles County in the south to San Mateo County in the central region (seven counties), but not in the northern part of the state (six counties). Two counties in the central region of the state, San Luis Obispo and Santa Cruz, displayed intense and frequent periods of elevated Cochlodinium cell abundances. Although not observed in the state-wide CDHS survey, we occasionally found cells in San Diego County with densities up to 2.7 × 10⁴ cells L⁻¹. Though these colonial dinoflagellates have been recognized in California for over 80 years, with several “blooms” recorded prior to 2004, the species’ geographic range and abundance in recent years suggest significant shifts in the nearshore phytoplankton community of this region of the eastern Pacific.     

Temporal changes in the cyst densities of Pyrodinium bahamense var. compressum and other dinoflagellates in Manila Bay, Philippines

Temporal variation in the type and abundance of dinoflagellate cysts in Manila Bay, Philippines, is established using ²¹⁰Pb-dated sediment cores. At least 17 dinoflagellate cyst species, including those of the toxic species, Pyrodinium bahamense var. compressum, were identified. P. bahamense may have been present in the area since at least the 1920s. Total cyst density has increased beginning about 1988 to 1998 coinciding with records of P. bahamense blooms in the area. Heterotrophs have always dominated the cysts assemblage. These changes in the dinoflagellate record and the P. bahamense blooms in recent years may have been induced by the interplay of warmer temperatures, high rainfall leading to higher river discharge and less turbulent waters due to passage of few tropical cyclones.     

考洲洋重金属污染水平与潜在生态危害综合评价

在等级模型的基础上,利用化学和生态学的方法,在地理信息系统(GIS)的支持下对考洲洋养殖水域表层海水及表层沉积物的重金属污染水平及潜在生态风险进行了综合评价,同时对不同的评价方法进行了分析和比较。结果表明,枯水期整个水域表层海水的重金属污染指数均低于0．5,丰水期更是低于0．2。调查期间湾内海水重金属含量较低,重金属污染不明显。枯水期绝大部分水域表层沉积物重金属的生态风险指数值变化范围为20～70,其高值区出现于湾的西部和西北部水域。表明这些水域的表层沉积物已受到重金属的轻微影响;丰水期整个水域表层沉积物重金属的潜在生态风险指数值均低于20,重金属污染不明显。在生态学方面,枯水期大部分水域的饵料生物水平均处于2～3级水平,其密集分布区位于湾西北部、湾口和吉隆河口附近水域,达4级水平,饵料生物较为丰富。丰水期饵料生物水平的密集分布区位于湾中部和望京洲沿岸水域,饵料生物最丰富,达4～5级水平;其次为湾口,为4级水平;最低则分布于湾的西部和西北部,其饵料生物较低,为1～2级水平。由于重金属污染程度较低,因此水温、盐度和营养盐等环境因子已成为影响湾内生态系统的主要因素。对各种不同评价方法所进行的分析和比较结果表明,采用多指标综合评价方法是描述污染和预测生态效应的一种有效途径。     

Causes and Consequences of Changes in Nutrient Structure in the Jiaozhou Bay

Concentrations and ratios of nutrients in Jiaozhou Bay, China, have changed much in the past decades, with trends indicating an increase in nitrogen and a decrease in silicate. Statistical analysis has shown that the long-term variations of nutrients are associated with agricultural activities, precipitation, and anthropogenic factors. Stoichiometric calculations indicate that the nutrient structure has become more and more unbalanced. There has been almost no possibility for nitrogen limitation since the 1980s, the probability of P limitation has increased, and the probability of Si limitation has also increased markedly from the 1980s to the 1990s. As a consequence of changes in nutrient structure, a decrease in the abundance of net phytoplankton was evident, whereas total chlorophyll a levels have remained roughly unchanged at around 3.55 μg/L. Thus, it is likely that smaller species have taken the niche vacated by the larger species. Changes in phytoplankton size and species composition may ultimately lead to various functional and structural changes at the system level.     

Finding of the Hydromedusa Hydractinia minima (Trinci, 1903) (Cnidaria: Hydrozoa: Hydractiniidae) in Peter the Great Bay, Sea of Japan

The first finding of the hydromedusa Hydractinia minima (Trinci, 1903) in plankton of Peter the Great Bay (Sea of Japan) is reported. The hydromedusae are 0.24–0.51 mm in bell diameter and 0.25–0.53 mm in height. The size characteristics of the nematocysts of this species (desmonemes and microbasic euryteles) are given. H. minima is present in the plankton of Peter the Great Bay from June through October at water temperatures of 16.4 to 22°C with the highest mean monthly density of 151 ind./m³. The finding of H. minima in Peter the Great Bay extends the area of this species in the North Pacific to the low-boreal subzone.Original Russian Text Copyright © 2005 by Biologiya Morya, Chaplygina, Dautova.     

Vertical distribution and germination ability of Alexandrium spp. cysts (Dinophyceae) in the sediments collected from Kure Bay of the Seto Inland Sea, Japan

The vertical distribution of Alexandrium tamarense/ catenella (hereinafter Alexandrium spp.) cysts was investigated with special attention to living cysts filled with fresh protoplasm and empty cysts. In addition, based on the incubation experiments of Alexandrium spp. cysts, the germination ability of the cysts was examined. A sediment core 63 cm in length, collected from Kure Bay of the Seto Inland Sea, West Japan, in September 2000, was provided for an analysis on the vertical distribution of Alexandrium spp. cysts. Samples from every 1 cm interval depth from the top down to 13 cm depth of the same core were taken to examine the germination ability of the cysts. Results show that Alexandrium spp. cysts were continuously observed from 59 to 60 cm depth to the top. The cyst densities in the upper parts of the core (from 9 to 10 cm depth to the top) were much more abundant those that in the lower parts (below 10–11 cm depth). The relationship between living and empty cysts in each depth did not reveal a positive correlation with the sediment depth. Based on the sedimentation rate of the core sediment (approximately 1.6 cm/year), Alexandrium spp. cysts have been produced since 1962, and a remarkable increase of these cysts was observed from ca 1993. Such a rapid increase of Alexandrium spp. cysts has probably been as a result of dense blooms of A. tamarense occurring since 1992 in Hiroshima Bay, including Kure Bay. The germination of Alexandrium spp. cysts was observed in samples collected from the top to 12–13 cm depth of the core. It suggests that the Alexandrium spp. cysts can keep the germination ability for more than 8 years.