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  • 1
    Online Resource
    Online Resource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Keywords: Marine ecology -- East China Sea. ; Electronic books.
    Description / Table of Contents: The first monograph dedicated to this topic, this book presents the latest achievements from China's national research projects on the biogenic element cycling processes in China marginal seas.
    Type of Medium: Online Resource
    Pages: 1 online resource (673 pages)
    Edition: 1st ed.
    ISBN: 9783642040603
    Series Statement: Advanced Topics in Science and Technology in China Series
    DDC: 577.1
    Language: English
    Note: Intro -- Title Page -- Copyright Page -- Preface -- Table of Contents -- 1 Introduction -- 1.1 Basic Status of China Marginal Seas -- 1.1.1 The Bohai Sea -- 1.1.1.1 Topography -- 1.1.1.2 Hydrographical and Chemical Environment -- 1.1.1.3 Tides -- 1.1.1.4 Circulation -- 1.1.1.5 Wind -- 1.1.1.6 Distribution Pattern of Sediments -- 1.1.1.7 Riverine Discharge -- 1.1.1.8 Biological Characteristics -- 1.1.2 The Yellow Sea -- 1.1.2.1 Topography -- 1.1.2.2 Hydrographical and Chemical Environment -- 1.1.2.3 Tides -- 1.1.2.4 Currents -- 1.1.2.5 Wind -- 1.1.2.6 Distribution Pattern of Sediments -- 1.1.2.7 Riverine Discharge -- 1.1.2.8 Biological Characteristics -- 1.1.3 The East China Sea -- 1.1.3.1 Topography -- 1.1.3.2 Hydrographical and Chemical Environment -- 1.1.3.3 Tides -- 1.1.3.4 Currents -- 1.1.3.5 Wind -- 1.1.3.6 Distribution Pattern of Sediments -- 1.1.3.7 Riverine Discharge -- 1.1.3.8 Biological Characteristics -- 1.1.4 The South China Sea -- 1.1.4.1 Topography -- 1.1.4.2 Hydrographical and Chemical Environment -- 1.1.4.3 Tides -- 1.1.4.4 Currents -- 1.1.4.5 Wind -- 1.1.4.6 Distribution Pattern of Sediments -- 1.1.4.7 Riverine Discharge -- 1.1.4.8 Biological Characteristics -- 1.2 Progress in Marine Biogeochemical Process Research in China -- 1.2.1 Progress in the Studies in Marine Biogeochemical Processes before 2000 in China -- 1.2.1.1 Estuaries, Coasts and Continental Shelf -- 1.2.1.2 Cycling Processes of Biogenic Elements in the Euphotic Zone -- 1.2.1.3 Marine Biogeochemical Process of Settling and Suspended Particulates -- 1.2.1.4 Biogeochemical Behavior near the Sediment-Water Interface -- 1.2.1.5 Function of Small Organisms in Marine Biogeochemical Cycling -- 1.2.2 Progress in Biogeochemical Processes of Marine Carbon Cycles since 2000 in China -- 1.2.2.1 CO2 Fluxes and Processes Between Atmospheres and Seawaters. , 1.2.2.2 Carbon and Its Biogeochemical Cycles in Seawaters -- 1.2.2.3 Carbon and Its Biogeochemistry in Marine Sediments -- 1.2.2.4 Impact of Soil from River and Marine Sediment on Carbon Cycles -- 1.2.3 Biogeochemical Cycle of Biogenic Elements -- 1.2.3.1 Biogeochemical Cycle of Nitrogen -- 1.2.3.2 Biogeochemical Cycle of Phosphorus -- 1.2.3.3 Source and Characteristics of Biogenic Silicate -- 1.2.3.4 Environment Chemical Process of the Persistent Organic Pollutants -- 1.2.3.5 Major and Minor Elements in Marine Environments -- 1.3 Functions of China Marginal Sea Sediments in Cycles of Biogenic Elements -- 1.3.1 Biogenic Elements in China Marginal Sea Sediments -- 1.3.2 Chemical Environments of China Marginal Sea Sediments and Early Diagenesis of Biogenic Elements -- 1.3.3 Contribution of Settling Particles to Biogenic Element Recycling in China Marginal Seas -- 1.3.4 Contributions of China Marginal Sea Sediments in the Recycling of Biogenic Elements -- 1.3.5 Influences of Biological Productions in China Marginal Sea Sediments on the Recycling of Biogenic Elements -- 1.3.5.1 Influences of Planktons on the Recycling of Biogenic Elements -- 1.3.5.2 Benthos Influences on the Recycling of Biogenic Elements -- References -- 2 Biogeochemical Processes of the Bohai Sea -- 2.1 Change Processes of Carbon in the Bohai Sea -- 2.1.1 Partial Pressure of CO2 in Sea Water -- 2.1.1.1 Distribution of PCO2 in Surface Waters -- 2.1.1.2 Relationship between PCO2 and Temperature, Salinity and Chl a -- 2.1.2 Riverine Sources and Estuarine Fates of Particulate Organic Carbon in Seawaters -- 2.1.2.1 Particulate Organic Carbon -- 2.1.2.2 Relationship between POC and Suspended Matter -- 2.1.2.3 Source of POC in the Estuary -- 2.1.3 Inorganic Carbon in Liaodong Bay Sediments of the Bohai Sea -- 2.1.3.1 Inorganic Carbon Forms in the Liaodong Bay Sediments. , 2.1.3.2 Relationship between Organic Carbon and Inorganic Carbon -- 2.1.3.3 Relationship Between Fe and Inorganic Carbon -- 2.1.3.4 Assessment of Influencing Factors -- 2.1.4 Biogeochemical Process of Organic Carbon in Sediments -- 2.1.4.1 Vertical Distribution of OC in Bohai Sea Sediments -- 2.1.4.2 Section Distribution in C Area -- 2.1.4.3 Correlative Factors of OC and OC Decomposition Dynamics -- 2.1.4.4 Decomposition of OC -- 2.2 Distributions and Transformations of Nitrogen in the Bohai Sea -- 2.2.1 Nitrogen in Seawaters -- 2.2.1.1 Distributions of Nitrogen -- 2.2.1.2 Vertical Variation of Dissolved Inorganic Nitrogen -- 2.2.1.3 Seasonal Differences of Nitrogen -- 2.2.1.4 Distinguishing between Transport and ConversionProcesses of Nitrogen -- 2.2.2 Evolution of Nutrients and Primary Production -- 2.2.2.1 Evolution of DIN and DIP in Bohai Sea Waters -- 2.2.2.2 Evolution of PP and Phytoplankton Community Structure -- 2.2.2.3 Influence on PP of Nitrogen and Phosphorus -- 2.2.2.4 Influence on Phytoplankton Community Structure of Nitrogen and Phosphorus -- 2.2.2.5 Indicative Function to Eco-environmental Evolution by Phytoplankton -- 2.2.3 Nitrogen Forms and the Decomposition of Organic Nitrogen in Sediments -- 2.2.3.1 Characteristics of Nitrogen Forms -- 2.2.3.2 OC Decomposition and Early Diagenesis in Core Sediments -- 2.2.3.3 Transferable Nitrogen in Core Sediments -- 2.2.4 Sediment-Water Exchange of Inorganic Nitrogen -- 2.3 Biogeochemical Processes of Phosphorus and Silicon in the Bohai Sea -- 2.3.1 Distribution of Phosphorus and Silicate in Seawaters -- 2.3.1.1 Horizontal Distribution of Phosphate and Silicate -- 2.3.1.2 Vertical Distribution of Phosphate and Silicon -- 2.3.2 Forms of Phosphorus and Silicon in Surface Sediments . -- 2.3.2.1 Forms of Phosphorus and Silicon in the Surface Sediments. , 2.3.2.2 Biogeochemical Processes of Phosphorus and Silicon of Surface Sediments in the southern Bohai Sea -- 2.3.3 Processes of Nutrients across the Sediment-Water Interface -- 2.3.3.1 Fluxes across the Sediment-Water Interface of P and Si in the Bohai Sea -- 2.3.3.2 Seasonal Variations of Phosphorus and Silicon Fluxes -- 2.3.3.3 Budgets of Phosphate and Silicate -- 2.3.3.4 Release and Adsorption of Nutrients -- 2.4 Behaviour of Heavy Metals in the Bohai Sea -- 2.4.1 Distribution of Dissolved Heavy Metals in Seawaters -- 2.4.2 Dissolved Heavy Metal Pollution in Bohai Bay -- 2.4.2.1 Distribution Characteristics of the Main Polluting Metalsin Surface Waters -- 2.4.2.2 Historical Changes of Pb and Zn in Surface Waters -- 2.4.3 Heavy Metals in Bohai Bay Sediments -- 2.4.3.1 Geochemical Characteristics of Core Sediments -- 2.4.3.2 Vertical Distribution of Heavy Metals -- 2.5 Persistent Organic Pollutants in the Coastal Areas of the Bohai Sea -- 2.5.1 Distributions of Persistent Organic Pollutants in Sediments and Mollusks -- 2.5.1.1 PAHs -- 2.5.1.2 Organic Chlorine Pesticides (OCPs -- 2.5.1.3 Dioxin-like Chemicals (PCBs, PCDDs and PCDFs) -- 2.5.1.4 Vertical Distribution of PCDD/Fs and PCBs -- 2.5.1.5 Summary for the Spatial and Temporal Distributions of POPs -- 2.5.2 Composition and Sources of Persistent Organic Pollutants -- 2.5.2.1 PAHs -- 2.5.2.2 HCHs -- 2.5.2.3 DDTs -- 2.5.2.4 PCBs -- 2.5.3 Potential Risk of Persistent Organic Pollutants -- 2.5.3.1 PAHs -- 2.5.3.2 DDTs and HCHs -- 2.5.3.3 PCDD/Fs and PCBs -- References -- 3 Biogeochemical Processes of the Yellow Sea -- 3.1 Dynamic Processes of the Yellow Sea -- 3.1.1 Yellow Sea Currents -- 3.1.1.1 Yellow Sea Warm Current -- 3.1.1.2 Coastal Currents -- 3.1.2 Water Exchange Between the Yellow Sea and the East China Sea -- 3.2 Carbon Biogeochemical Processes in the Yellow Sea. , 3.2.1 Carbon Processes across the Air-Sea Interface -- 3.2.1.1 Horizontal Distributions of Dissolved Inorganic Carbonand Alkalinity in the Surface Water -- 3.2.1.2 Horizontal Distributions of pH and PCO2 in the Surface Water -- 3.2.1.3 Relationships Between PCO2 and Temperature, Salinity,Longitude and Latitude -- 3.2.1.4 Carbon Flux across Seawater Interface of the Yellow Sea -- 3.2.2 Biological Carbon Fixation in the South Yellow Sea Seawater -- 3.2.2.1 Water Masses -- 3.2.2.2 Carbon Fixation Production -- 3.2.3 Initial Carbon Fixed Production -- 3.2.3.1 Estimation of Carbon Fixed Production of Phytoplankton -- 3.2.3.2 Estimation of Carbon Fixed Production of Zooplankton -- 3.2.3.3 Changes in Carbon Fixed Production and Ecosystem -- 3.3 Dimethylsulfide and Its Fluxes across the Sea-Air Interface of the Yellow Sea -- 3.3.1 Characteristics of Dimethylsulfide and Dimethylsulfoniopropionate -- 3.3.1.1 Horizontal Distributions -- 3.3.1.2 Biological Production and Consumption of Dimethylsulfide -- 3.3.1.3 Roles of Phytoplankton Biomass in Controlling the Distribution of Biogenic Sulfur -- 3.3.2 Sea-to-Air Flux of Dimethylsulfide -- 3.3.3 Source and Sink of Dimethylsulfide in the Microlayer . . -- 3.4 Biogeochemical Characteristics Nitrogen and Phosphorus in the Yellow Sea -- 3.4.1 Variations of Nitrogen and Phosphorus in Seawaters -- 3.4.1.1 Evolution of N and P from 1999 to 2005 -- 3.4.1.2 Reasons for the Environmental Variation -- 3.4.2 Dry and Wet Fluxes of Nutrients -- 3.4.2.1 Dry Deposition Flux of Nutrients -- 3.4.2.2 Wet Deposition Fluxes of Nutrients -- 3.4.2.3 Comparison Between the Atmospheric Fluxes and Riverine Inputs -- 3.4.3 Nutrients in the South Yellow Sea Sediments -- 3.4.3.1 Distribution Characteristics of Nitrogen -- 3.4.3.2 Relationships of Different Forms of Nitrogen -- 3.4.3.3 Predominant Factors Affecting Nitrogen Distributions. , 3.4.3.4 Release of Nitrogen.
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Journal of bioenergetics and biomembranes 28 (1996), S. 153-161 
    ISSN: 1573-6881
    Keywords: Mitochondrial outer membrane ; VDAC ; membrane folding patterns ; evolutionary conservation
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Chemistry and Pharmacology , Physics
    Notes: Abstract Previous research on the mitochondrial channel VDAC from the yeastS. cerevisiae had identified protein strands forming the wall of VDAC's aqueous pore. Here we report the results of analyzing the primary sequences of VDAC from various sources to see if the transmembrane folding pattern identified from this yeast is conserved for VDAC of different species. We analyzed the primary sequences of VDAC from higher plants, fungi, invertebrates, and vertebrates and found that all have a very similar “β-partern” profile with 12–15 peaks indicating potential sided beta strands that are candidates for protein strands forming the wall of the aqueous pore. All these VDAC sequences can be put into the 13 transmembrane strand folding pattern previously identified for yeast VDAC. These folding patterns agree with available experimental data: both electrophysiological and protease digestion data. Although the primary sequences of VDAC from very diverse organisms show low homology, sequence similarity in the proposed corresponding 13 transmembrane strands is substantial. Competing proposals utilizing 16 transmembrane β strands are in conflict with electrophysiological experimental observations and violate the constraints on such strands, such as no charged amino acids facing the phospholipid membrane and sufficient number of residues to span the membrane.
    Type of Medium: Electronic Resource
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  • 3
    Publication Date: 2016-11-23
    Description: From a large number of case studies on terrestrial deposits we know that Late Holocene climate fluctuations have an important impact on the terrestrial environments. However, it is hitherto not clear how the marine sediments can be used to shed light on the environment and climate change of the catchment. To provide such insight, we used the major element, trace element and rare earth element (REE) compositions in the southern Yellow Sea (SYS) sediments to reconstruct the changes in weathering and erosion of their source regions. The sediments originate predominantly from the upper crust of East China and are transported into the basin especially by the Yellow River (Huanghe) and to a lesser extent by the Yangtze River (Changjiang). The chemical index of alteration (CIA; 53.7–59.7) suggests low chemical weathering of the source rocks since the Middle Holocene. This is consistent with the relatively cool and arid climate in North China after the Holocene Megathermal. Comparison of element ratios, including Al/Ca, K/Ca, Al/Na, K/Na, Rb/Sr, Li/Ba and the CIA shows that we can use the latter as a robust proxy for climate change. The CIA-based mean annual precipitation and mean annual temperature show a series of climate fluctuations in the catchment. A relatively warm and humid Period I (5.3–2.9 cal. ka BP), a relatively cool and dry Period II (2.9–0.9 cal. ka BP) and an increasingly cool and dry Period III (0.9–0.3 cal. ka BP). These periods can be linked to climate intervals recognized elsewhere.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , peerRev
    Format: application/pdf
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  • 4
    Publication Date: 2024-02-07
    Description: Bacterial metabolism largely drives the sequestration of refractory organic matter in the ocean. However, a lack of understanding exists regarding the abundance and reactivity of bacterial particulate organic matter (POM). Here we report the bacterial contributions to suspended POM collected in the oligotrophic Western Pacific Warm Pool (WPWP). Around 27% of particulate organic carbon (POC) and ∼39% of particulate nitrogen (PN) in the surface ocean were derived from bacteria. Most of the bacterial POM (∼87%) was labile or semi-labile, and ∼85% of bacterial POM was removed between depths of ∼100–300 m. Bacterial POM constituted only ∼8% and ∼13% of refractory POC and PN, respectively. The rapid cycling of bacterial POM in upper waters was likely related to oligotrophic conditions and facilitated by higher temperatures in the WPWP. Taken together, these observations indicate that bacterial POM plays a crucial role in supplying energy for bacterial respiration. Key Points We assess bacterial contributions to suspended particulate organic matter (POM) in the Western Pacific Warm Pool on the basis of D-amino acid biomarkers Bacterial organics constitute 27% of surface ocean particulate organic carbon (POC) and 39% of particulate nitrogen (PN), but majority (∼87%) is labile or semi-labile Rapid cycling of bacterial POM in the upper ocean results in a contribution of only ∼8% to refractory POC and ∼13% to PN
    Type: Article , PeerReviewed
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  • 5
    Publication Date: 2024-02-07
    Description: Viruses carrying phoH genes are an important functional group that may boost phosphate metabolism of their prokaryote hosts and affect phosphorus cycle in the ocean. However, at present, very little is known about the phoH-carrying viruses' community structure and diversity in marine sediments, as well as their correlation network with prokaryotes and environment. Here, via a large spatial scale investigation along the Bohai Sea, Yellow Sea, and East China Sea, for the first time, diverse unknown benthic phoH-carrying viruses were uncovered, which were mainly affiliated to three clusters. Interestingly, these viruses presented a very distinct community structure compared to those in seawaters. Correlation network analysis implied that these viruses might mainly infect the prokaryotes of Gamm-/Delta-proteobacteria, Thaumarchaeota, and Cyanobacteria in sediments. Distinct virus-prokaryote correlation network modules were shown in different sea areas. These modules' highly nested feature implied their coevolution with prokaryotes during long-term arms race. Their distribution in sediments was influenced by multiple factors including geographic separation and the key environmental variables of total organic carbon and total phosphorus, and responded to terrestrial inputs and coastal aquaculture activities. The results of this study provide novel insights into the benthic virus communities potentially participating in phosphorus cycling in the ocean.
    Type: Article , PeerReviewed
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  • 6
    Publication Date: 2024-02-07
    Description: Concentrations of particulate organic carbon (POC) and total hydrolyzable amino sugars (THAS) were measured along a transect of the dynamic South Yellow Sea (SYS) to investigate the bioreactivity and bacterial reworking of particulate organic matter (POM). Results showed that POM bioavailability was linked with primary production, as revealed by the significant correlation between chlorophyll-a concentrations and the diagenetic indicator glucosamine/galactosamine (GlcN/GalN). Production of bioavailable POM could rapidly stimulate microbial activity, generating hot spots of heterotrophic alteration. Lower GlcN/GalN ratios (〈3) observed in the entire SYS indicate that POM underwent extensive microbial alteration. In particular, extremely low GlcN/GalN ratios (∼0.7) were found in the Yellow Sea Cold Water Mass, reflecting high bacterial alteration of POM. Estimates based on the bacterial biomarker muramic acid showed that on average ∼13% of POM in the SYS was of bacterial origin. Elevated bacterial contributions were found in both nearshore and offshore areas. Strong mixing in the nearshore and the presence of cyclonic eddies in offshore waters may increase the residence time of POM in the water column and thus promote bacterial transformation of POM. Overall, our findings indicate that bacterial reworking of POM varies with productivity and that the extensive bacterial transformation of the remaining POM observed in the water column probably enhances long-term carbon sequestration.
    Type: Article , PeerReviewed
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  • 7
    Publication Date: 2024-02-07
    Description: Compound‐specific isotope analysis has opened up a new realm for resolving the sources and transformation processes of marine organic matter. However, the stable carbon isotope patterns of amino sugars remain unknown. We examined δ 13 C of amino sugars in marine phytoplankton and heterotrophic bacteria, and the variations in amino sugar δ 13 C during 66‐d planktonic organic matter degradation experiments, to investigate the metabolic sources and transformations of amino sugars by bacterial reworking. The δ 13 C values of glucosamine (GlcN) and galactosamine (GalN) were comparable in heterotrophic bacteria (difference Δδ 13 C GlcN–GalN = 0.4–4.0‰) but pronouncedly different in phytoplankton (Δδ 13 C GlcN–GalN = 4.3–16.6‰), suggesting similar synthesis pathways of GlcN and GalN in bacteria that differed from phytoplankton. Compared to GlcN and GalN, bacteria preferentially use isotopically light organic compounds for muramic acid (MurA) synthesis. During simulated microbial degradation of organic matter, the δ 13 C difference between GlcN and GalN decreased from 5.8‰ on the initial day to 1‰ at a late stage in the experiment, but the difference between GlcN and MurA remained at 5.3‰. This difference is consistent with the pattern in cultured phytoplankton (average Δδ 13 C GlcN–GalN = 5.9‰ ± 1.4‰) and heterotrophic bacteria (average Δδ 13 C GlcN–MurA = 4.6‰ ± 3.4‰), indicating enhanced bacterial resynthesis as degradation proceeded. Based on the difference in δ 13 C among GlcN, GalN, and MurA, we propose a novel index of variation in amino sugar δ 13 C, representing amino sugar resynthesis, to describe the diagenetic state of organic matter. Together, these findings suggest that amino sugar δ 13 C can be used as a new tool to track heterotrophic processes of marine organic matter.
    Type: Article , PeerReviewed
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  • 8
    Publication Date: 2024-02-23
    Description: Marginal seas influenced by large rivers are characterized by complex hydrodynamic and organic matter cycling processes. However, the impacts of hydrodynamics on the composition and reactivity of particulate organic matter (POM) remain unclear. Here we conducted a comprehensive study on the bulk, molecular and biological properties of suspended POM in the Changjiang Estuary and adjacent area subjected to strong currents, eddies as well as typhoons during spring and autumn. D/L‐enantiomers of particulate amino acids (PAA) were analyzed to evaluate the bioreactivity of POM and quantify bacterial‐derived organic carbon. We found that POM bioavailability as indicated by carbon‐normalized yields of PAA (PAA‐C%) reflected the ecosystem productivity. Relatively high PAA‐C% values (20−35%) were observed in productive areas influenced by Changjiang River plume, cyclonic eddies and typhoons, likely related to the enhanced nutrient availability arising from hydrodynamic processes. In contrast, the oligotrophic Taiwan Warm Current‐influenced regions featured relatively low POM bioavailability (PAA‐C% 〈 10%) despite typhoons facilitating water mixing. The PAA‐C% values showed a significant positive correlation with extracellular enzyme activity, indicating that bioavailable POM can rapidly stimulate heterotrophic transformation. Hot spots of elevated bioavailable POM showed high contributions of bacterial organic carbon. A large portion (∼2/3) of bacterial organic carbon was present in the form of bacterial detritus, suggesting that patches of these biological hot spots represent important sites of carbon sequestration. Together, our findings indicate that fresh POM production is largely controlled by nutrient supply driven by hydrodynamic processes, with important implications for carbon sequestration in the dynamic ocean margins. Plain Language Summary Marginal seas are subject to complex hydrodynamic processes and play an important role in carbon sequestration. Disentangling the linkages between hydrodynamics and organic carbon reactivity and composition is crucial to understanding the regional carbon cycle. Here we collected suspended particulate organic matter (POM) in the Changjiang Estuary and adjacent coastal areas. Based on the biomarker D/L‐amino acids, we assessed the bioavailability of POM and quantified the organic carbon originating from bacteria. We found that high bioactivity of POM occurred in productive Changjiang River plume, cyclonic eddy, and typhoon influenced areas. These hydrodynamic processes appear to increase nutrient availability, therefore promoting phytoplankton growth. Bioavailable POM can rapidly stimulate heterotrophic activity and facilitate the transformation of algal‐derived organic carbon to bacterial detritus, thus contributing to carbon sequestration. Our findings suggest that the production of bioavailable POM is largely controlled by hydrodynamically driven nutrient supply. Key Points We use D/L‐amino acids to assess the bioreactivity and bacterial origins of particulate organic matter (POM) in the dynamic Changjiang Estuary and adjacent area High bioavailability of POM occurs in productive regions affected by Changjiang River plume, cyclonic eddies and typhoons Hot spots of bioavailable POM represent important sites for carbon sequestration
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  • 9
    Publication Date: 2024-03-25
    Description: The TetraEther indeX of 86 carbon atoms (TEX86) is widely used as a proxy to reconstruct past sea surface temperatures. Most current applications of TEX86 are primarily based on analyzing the composition of isoprenoid glycerol dialkyl glycerol tetraethers (isoGDGTs) that comprise TEX86 in sediments, with the assumption that the sedimentary isoGDGTs are mainly derived from the surface mixed layer. Here we report on the variations in the isoGDGT distribution, archaeal abundance and community through the water column of the Western Pacific Ocean, directly testing the export depth of isoGDGTs and constraining the temperature records of TEX86. Our data show that maximum isoGDGT concentrations occurred in subsurface waters (150–200 m) with maximum archaeal abundances. The ratio between isoGDGTs bearing 2 vs. 3 cyclopentane moieties, i.e. [2/3] ratio, increased with depth, which is likely related to the shift of the archaeal community from Ca. Nitrosopelagicus-dominance to norank_f__Nitrosopumilaceae-dominance. Models based on the [2/3] ratios in the water column predicted an average export depth of isoGDGTs to sediments of around 150–200 m, consistent with the robust relationship between the compiled sedimentary TEX86 and the annual mean subsurface temperature. Taken together, our findings support that TEX86 records subsurface rather than surface temperatures in the open ocean.
    Type: Article , PeerReviewed
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  • 10
    Publication Date: 2017-06-27
    Description: The prognostic significance of PD-L1 expression in patients with glioma: A meta-analysis Scientific Reports, Published online: 26 June 2017; doi:10.1038/s41598-017-04023-x
    Electronic ISSN: 2045-2322
    Topics: Natural Sciences in General
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