Chemical consequences of oxygenation in a shallow eutrophic lake studied with mesocosms

To assess the effects of oxygenation in a shallow, highly eutrophic lake, an experiment with large enclosures was carried out. From the results two main effects can be expected from the oxygenation of the whole lake: (a) fish mortality and the resulting putrefactive processes would be avoided; (b) an increase in nitrogen and phosphorus concentration and, consequently, in the trophic level of the lake would probably occur.     

铁施肥促进海洋浮游植物和生物碳泵的不确定性

铁作为浮游植物所必需的微量元素,限制了全球超过三分之一海域的初级生产力,尤其是在高营养盐、低叶绿素海域(high nutrient low chlorophyll,HNLC)。长期以来海洋铁施肥被认为是一项可以降低大气二氧化碳含量的地球工程策略。然而通过13次海洋人工铁施肥(artificial ocean iron fertilization,aOIF)实验发现,铁的额外添加对海洋深层碳输出量的促进作用要显著低于预期。本文简要地总结了碳在海洋和大气中的循环过程,回顾了人工铁施肥实验对生物碳泵和碳通量等的影响,分析了从海洋铁施肥到海洋碳汇关键生物地球化学过程的影响因素。综上分析发现,科学界对生物碳泵过程及其调控机制的认识仍十分浅薄,考虑到海洋铁施肥还会对海洋生态系统带来一定的负面作用,铁施肥能否作为降低大气中CO₂的有效手段,以达到碳中和并缓解温室效应仍需进一步研究。     

Bacterial utilization of algal extracellular products in a southwestern reservoir

Rates of carbon flow from phytoplankton to bacteria were estimated for Lake Arlington, Texas. The lake is a warm (annual temperature range 7 to 35 °C), shallow, monomictic reservoir with limited macrophyte development in the littoral zone. Samples were collected from 6 depths within the photic zone from a site located over the deepest portion of the lake. Primary production and exudate production were calculated from NaH¹⁴CO₃ incorporation. Bacterial production was calculated from [methyl-³H]-thymidine incorporation. Depth averaged primary production ranged from a seasonal low of 9.0 μg C l⁻¹ h⁻¹ in January to a seasonal maximum of 153 μg C l⁻¹ h⁻¹ during holomixis in September. Annual depth-averaged production was 67.8 ± 7.3 μg C l⁻¹ h⁻¹. Exudate production ranged between 21.9 and 54.2% of primary production and annually averaged 30.8%. Bacterial production ranged between 1.7 and 46.0 μg C l⁻¹ h⁻¹ and annually averaged 16.0 ± 1.9 μg C l⁻¹ h⁻¹. Bacteria processed approximately 70% of exudate and incorporated 35% into biomass. Bacterial production was positively correlated with total primary production (r = 0.38, p < 0.003, n = 6), particulate primary production (r = 0.34, p < 0.004, n = 70) and bacterial uptake of exudate (r = 0.43, p < 0.001, n = 68). While exudate was readily utilized by bacteria it dit not appear to be produced in sufficient quantity or at a sufficient rate to serve as the sole or a major source of carbon supporting bacterial growth.     

Evidence for Permo-Triassic colonization of the deep sea by isopods

The deep sea is one of the largest ecosystems on Earth and is home to a highly diverse fauna, with polychaetes, molluscs and peracarid crustaceans as dominant groups. A number of studies have proposed that this fauna did not survive the anoxic events that occurred during the Mesozoic Era. Accordingly, the modern fauna is thought to be relatively young, perhaps having colonized the deep sea after the Eocene/Oligocene boundary. To test this hypothesis, we performed phylogenetic analyses of nuclear ribosomal 18S and 28S and mitochondrial cytochrome oxidase I and 16S sequences from isopod crustaceans. Using a molecular clock calibrated with multiple isopod fossils, we estimated the timing of deep-sea colonization events by isopods. Our results show that some groups have an ancient origin in the deep sea, with the earliest estimated dates spanning 232–314 Myr ago. Therefore, anoxic events at the Permian–Triassic boundary and during the Mesozoic did not cause the extinction of all the deep-sea fauna; some species may have gone extinct while others survived and proliferated. The monophyly of the ‘munnopsid radiation’ within the isopods suggests that the ancestors of this group evolved in the deep sea and did not move to shallow-water refugia during anoxic events.     

城市系统碳循环:特征、机理与理论框架

城市是地表受人类活动影响最深刻的区域,城市系统碳循环在全球和区域碳过程中具有重要的地位和作用.提出了城市“自然-社会”二元碳循环的概念,探讨了城市系统碳循环的一般特征;分析了城市系统碳循环的内部机理,主要包括:城市系统碳储量和碳输入/输出通量的主要过程和途径、城市系统碳储量、碳通量和碳流通的生命周期分析、城市系统碳输入和碳输出的类型划分等;提出了基于系统层次划分和碳流通过程的城市系统碳循环的研究框架,分析了城市自然系统和城市经济系统的主要碳流通过程和环节,构建了城市系统碳循环研究的思路和理论框架;最后提出了城市系统碳循环领域未来的研究重点.     

Vertical and seasonal variations of inorganic carbon allocation into macromolecules by phytoplankton population in a brown-colored and a clear-water lake

The aim of this study was to asses vertical and seasonal variations of inorganic carbon allocation into macromolecules by phytoplankton population in an humic and acidic lake (Lake Vassivière) and in a clearwater lake (Lake Pavin). Biochemical fractionation was done by consecutive differential extractions in order to separate proteins, polysaccharides, lipids and low molecular weight compounds (LMW) by virtue of their relative solubilities in different extraction solvents.Independent of depth and season, the principal photosynthetic end products were polysaccharides followed by proteins, LMW and lipids. However, inorganic carbon allocation into macromolecules varied, in these two lakes, with depth and with the taxonomic composition of phytoplankton. Carbon allocation into polysaccharides decreased with increasing depth, especially in the brown-colored humic lake, and Diatoms, showed high C incorporation into polysaccharides.     

Carbon isotope ratio and photosynthetic activity of phytoplankton in the eutrophic Mikawa Bay,Japan

Primary production by phytoplankton in the eutrophic Mikawa Bay, Japan, was studied by simultaneous measurements of natural carbon isotope ratio (δ ¹³C) and short-term carbon uptake rates (¹³C tracer study) of size-fractionated nannoplankton (<10 μm) and net plankton (>10 μm) samples. Short-term photosynthetic rates, which represent the physiological state of algae, were variable regardless of standing stock sizes. Theδ ¹³C values of particulate organic carbon (POC) in June and July displayed horizontal variations for both the net plankton fraction (−19.8 to −12.7‰) and the nannoplankton fraction (−22.0 to −12.8‰). For both fractions, low concentrations of POC had more negativeδ ¹³C values (−22 to −18‰). Highδ ¹³C values for the net plankton were found when POC concentrations were much higher, due to red tide. This suggests that the increase in algal standing crop for the net plankton fraction resulted from accelerated photosynthetic activity. However the nannoplankton fractions with higher POC values have relatively lowδ ¹³C values.     

棕囊藻属(Phaeocystis)的分类与生活史(综述)

棕囊藻属Phaeocystis（定鞭藻纲Prymnesiophyceae)的分类问题目前还有争论。其种的分类标准是以初始的群体形态、地理分布、细胞特征等以及分子生物学特征,如染色体倍性,基因组大小等为依据。基于以上各种分类特征,目前比较确定的棕囊藻属藻类有四种：一种是只观察到单细胞形态的凹孔棕囊藻（P.scrobiculata),另外三种是能够形成群体的波切棕囊藻（P.pouchetii)、球形棕囊藻（P.globosa)和南极棕囊藻（P.antarctica)。棕囊藻具有一个复杂的异形生活史,介于几种游离的单细胞（不动的细胞,具有鞭毛的动细胞,小游动孢子以及可能存在的大游动孢子）和群体之间的形态交替。但其生活史中仍有许多不确定的问题。     

The regional record of Albian oceanic anoxic events at the Apulian Platform Margin (Gargano Promontory, southern Italy)

The Gargano Promontory, located on the eastern margin of the Apulia Platform, represents a distinctive Tethyan area where the transition from carbonate platform to adjacent basin is exposed on land. The Albian stratigraphic record, represented by shallow-water, slope and deep-water deposits, provides a good opportunity to investigate the regional response to oceanic anoxic events (OAEs) in different depositional settings by using an integrated, high-resolution micropalaeontological (planktonic foraminifers and calcareous nannofossils) approach. Results show that organic matter preservation is confined to the more distal areas (Marne a Fucoidi Formation), and consists of black shale intervals from the middle and late Albian (Ticinella primula/Prediscosphaera columnata Zones; upper Ticinella praeticinensis Subzone/R. achlyostaurion Zone, respectively). Integrated biostratigraphic data correlate the intervals of black shale deposition to the Urbino and Amadeus levels, previously identified and named in the Umbria-Marche Basin. These black shales record the effects of OAEs 1b and 1c. The biotic changes in the pelagic Albian succession of the Apulian Platform Margin provide evidence for episodes of eutrophication that correlate to the deposition of these black shales. Genetic models for the two episodes of organic matter preservation are proposed, taking into account both global and local controlling factors.     

Species-specific growth rate of phytoplankton in the West Pacific sector of the Southern Ocean. I.Prorocentrum scuttellum schröder

Phytoplankton samples were collected from the West Pacific Sector of the Southern Ocean to measure the growth rate from November 30 to December 1, 1995.Prorocentrum scuttellum was selected for growth rate measurement using the method of cell cycle analysis. During the 24 hr sampling cycle, cells ofP. scuttellum changed from 2,500 to 5,000 cells/L. The highest abundance was observed at 8:40 AM, December 1, and lowest at 11:40 PM, November 30. Cellular division seemed to occur sometime between 11:40 PM, November 30 and 2:40 AM, December 1. After cell division, DNA fluorescence shifted slowly towards the right, representing the S phase, and the majority of the cells were in S+G2 phases at 8:40 AM, December 1. Between the next six hours, a sharp drop in DNA fluorescence occurred, representing mitosis, and the majority of the cells returned to the G1 phase by 2:40 PM, December 1. We can not determine the duration time of the terminal event from this result However, the growth rate ofP. scuttellum was calculated as 0.43 d^-1 with the help of curve fitting methods. This unexpected result seems to have resulted due to background noise, unsynchronous cell division, unequal sampling, water column unstability, and migrating behavior ofP. scuttellum.     

CELL AND GROWTH CHARACTERISTICS OF TYPES A AND B OF EMILIANIA HUXLEYI (PRYMNESIOPHYCEAE) AS DETERMINED BY FLOW CYTOMETRY AND CHEMICAL ANALYSES1

Two morphotypes of Emiliania huxleyi (Lohmann 1902) Hay et al. 1967, types A and B, known to be unequally distributed in the oceans, were grown in dilution cultures at a range of photon flux densities (PFDs) (1.5–155 μmol photons·m^?2·s^?1) and two temperatures (10° and 15° C). Calcite carbon and organic carbon content of the cells as well as instantaneous growth rate, cell size, chlorophyll fluorescence, and light-scatter properties clearly depended on growth conditions and differed considerably for the two morphotypes. The ratio between calcite carbon and organic carbon production showed an optimum of 0.65 in E. huxleyi type A cells at PFD = 17.5. The ratio increased slightly with a temperature increase from 10° to 15°C but remained < 1.0 at both temperatures in light-limited cells. In contrast, calcite carbon production exceeded organic carbon production (ratio: 1.4–2.2) in phosphate-deprived cultures. Emiliania huxleyi type B generally showed a higher calcite carbon/organic carbon ratio than E. huxleyi type A, but the relation with PFD was similar. The content of calcite carbon and organic carbon as well as the instantaneous growth rate, cell size, chlorophyll fluorescence, and light-scatter properties showed large diel variations that were closely related to the division cycle. Our results show the importance of mapping the structure of any sampled cell population with respect to the phase in the cell division cycle, as this largely determines the outcome of not only “per cell” measurements but also short time (less than 24 h) flux measurements. For instance, dark production of calcite by E. huxleyi was negatively affected by cell division. Slowly growing (phosphate-stressed) cultures produced calcite in the light and in the dark. In contrast, rapidly growing cultures at 10°C produced calcite only in the light, whereas in the dark there was a significant loss of calcite due to dissolution.     

Relationships between phytoplankton periodicity and the concentrations of total and unionized ammonia in channel catfish ponds

Phytoplankton abundance fluctuated throughout a 9 month study period in two 1.62 ha channel catfish (Ictalurus punctatus) production ponds. Summer phytoplankton communities in both ponds were dominated by blue-green algae (Cyanophyta). During periods of rapidly decreasing phytoplankton abundance, total ammonia-nitrogen concentrations increased but a decrease in pH during these same periods moderated the concentrations of unionized ammonia-nitrogen. Although unionized ammonia-nitrogen concentrations did not reach levels considered acutely toxic to fish, extended periods of moderately high unionized ammonia-nitrogen concentrations (>O.15 mg/1) occurred in the late fall months and may have serious implications for fish health.