ScholarWorks@Hanyang University ERICA Campus: Shin, Kyung Hoon

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Shin, Kyung Hoon (신경훈)

ERICA 공학대학 (ERICA 해양융합공학과)

Research Area: 동위원소생태환경과학, 해양유기생지화학, Isotope Ecology and Environmental Science, Marine Organic Biogeochemistry

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stable isotope:11||primary productivity:9||Copepod:9||phytoplankton:9||Dissolved organic matter:8||Trophic position:8||Yellow Sea:8||Polychaete:7||surface sediment:7||Lake Shihwa:7||clay mineral:6||trophic position:6||IBP:6||nalkanes:6||amino acid:6||Sediment:5||zooplankton:5||Oxidative stress:5||biomarker:5||HPLC:5||Organic matter:5||Perinereis nuntia:5||Glutathione Stransferase:5||Estuary:5||Stable isotope:5||food web:4||Carbon isotopes:4||nAlkanes:4||Kongsfjorden:4||pigment:4||Phytoplankton:4||Fatty acids:4||EEMPARAFAC:4||Tigriopus japonicus:4||Source tracking:4||Carbon stable isotope:4||Fluorescence:4||POM:4||Bioaccumulation:4||Stable carbon isotope:4||Temperature:4||Microcystis aeruginosa:4||Food web:4||점토광물:4||Amino acids:4||stable isotope tracer:3||Elovl:3||Nalkanes:3||표층 퇴적물:3||Zostera marina:3||Sediment organic matter:3||Lipid biomarker:3||compoundspecific isotope analysis:3||Carbon isotope:3||Fluorescence spectroscopy:3||Stable isotope ratio:3||Compoundspecific isotope analysis:3||Holocene:3||Stable isotopes:3||Asan Bay:3||nitrogen isotope:3||황해:3||sea ice:3||Tributyltin:3||bioaccumulation:3||Alkenone:3||Brachionus koreanus:3||FTICRMS:3||illite:3||DDVP:3||fish:3||PAHs:3||Estuary dam:3||Fatty acid profile:3||DOM:3||Fatty acid:3||Metallothioneinlike proteins:3||biomarkers:3||Sediments:3||Source discrimination:3||provenance:3||mycosporinelike amino acids:3||Biomarker:3||13C tracer method:3||Nitrogen isotope:3||delta C13:3||Paracyclopina nana:3||Arctic Ocean:3||delta N15:3||Biodegradation:3||Trophic transfer:3||trace metals:2||PARAFAC:2||Dongdae Bay:2||CARBON:2||trophic level:2||Hucksan Mudbelt Deposit:2||compoundspecific isotope analysis (CSIA):2||Copper:2||Manila clam:2||Source identification:2||Source tracing:2||근원지:2||South Sea of Korea Mudbelt Deposit:2||dinosterol:2||Alkylphenols:2||CHEMTAX:2||Stable isotope analysis:2||Stable isotope ratios:2||Cytochrome P450:2||ISOTOPIC COMPOSITION:2||Catalase:2||Mercury:2||estuary:2||fatty acid:2||fatty acids:2||아산만:2||아이비피:2||Metal:2||일라이트:2||Metallothionein:2||Stratification:2||Styrene oligomers:2||정량X선회절분석법:2||Arctic:2||Paleovegetation:2||Interlaboratory comparison:2||Bayesian mixing model:2||Svalbard:2||Particulate organic carbon:2||Beaufort sea:2||Methylmercury:2||glutathione Stransferases:2||Irgarol 1051:2||Microalgae:2||Microcystins:2||Alternative biocides:2||East Sea (Japan Sea):2||COLD SEEPS:2||Tetraselmis suecica:2||Amino acid:2||Jeju Mudbelt Deposit:2||Benthos ecosystem:2||lake:2||AhR agonists:2||linear discriminant analysis:2||Primary production:2||Primary productivity:2||Gas hydrate:2||Mycosporinelike amino acids:2||Anaerobic oxidation of methane:2||mercury:2||Quantitative Xray diffraction analysis:2||Endmember mixing:2||Geum estuary:2||RIVER:2||LDI:2||Endmember mixing analysis:2||UV radiation:2||UVB:2||CSIA of amino acids:2||Lake Sihwa:2||Remediation:2||nalkane:2||Lake sihwa:2||Landuse types:2||Reproduction:2||CSIAAAs:2||River impoundment:2||nitrogen isotopes:2||Neanthes succinea:2||nitrogen stable isotope:2||Water quality:2||Diazinon:2||Cadmium:2||Rotifer:2||Ruditapes philippinarum:2||Youngsan River:2||organophosphorous pesticides:2||Nitrogen stable isotope:2||BISPHENOLA:2||Lipid:2||SIAR:2||Lipid biomarkers:2||Lipid metabolism:2||Eutrophication:2||Nutrient diol index:2||Lipid peroxidation:2||ORGANICMATTER:2||polychaete:2||Biodegradability:2||amino acids:2||STABLE CARBON:2||Extracellular polymeric substances:2||quantitative Xray diffraction analysis:2||quartz:2||Compoundspecific isotope analysis (CSIA):2||FOODWEB:2||authentication:2||SURFACE SEDIMENTS:2||benthic microalgae:2||Salinity:2||biocontrol:2||seasonal variation:2||sediment:2||MARINE:2||MARINESEDIMENTS:2||Organic pollutants:2||Fad:2||Organophosphorous pesticides:2||Sediment management:2||stable isotope analysis:2||stable isotope analysis (SIA):2||Organophosphorous pesticides (OPs):2||Sedimentary organic carbon:2||stable isotopes:2||Diuron:2||Seomjin estuary:2||Seomjin river estuary:2||Sequencing batch reactor:2||MICROBIAL COMMUNITIES:2||Shingu Reservoir:2||Shingu reservoir:2||GCQTOFMS:1||GC/C/IRMS:1||GENE:1||GENOME:1||GHB:1||GSFLX:1||GST:1||Gamma (gamma)hydroxybutyric acid:1||Gamma radiation:1||Gas chromatography&#8211:1||Gas chromatographycombustionisotope ratio mass spectrometry (GCC/IRMS):1||Geographical authentication:1||Geum Estuary:1||Geum River:1||Glacial retreat:1||Global monsoon (GM):1||Glycerol dialkyl glycerol tetraethers:1||Glycerol dialkyl glycerol tetraethers (GDGTs):1||Glycerophospholipid:1||Glyoxylate:1||Gohyeon Bay:1||Green tide:1||Greenling:1||Growth:1||Gymnosperm:1||H4IIEluc bioassay:1||HABITAT:1||HAENAM SAGUMI:1||HBIs:1||HEXAPLEXTRUNCULUS:1||HIGHLY BRANCHED ISOPRENOIDS:1||HONGKONG:1||HPLCMS/MS:1||HYDROCARBONS:1||Halocynthia roretzi:1||Han river:1||Hanon paleomaar:1||Heat shock protein:1||Heat shock protein (Hsp):1||Heat shock proteins:1||Heavy metals:1||Herbicide:1||Human health risk assessment:1||Human risk assessment:1||Hydrological modeling:1||Hydrology:1||Hydrophobic organic contaminants (HOCs):1||Hydroxylated isoprenoid glycerol dialkyl glycerol tetraethers (OHGDGTs):1||INDUSTRIAL:1||INGESTION:1||IP25:1||IRMS):1||Impose:1||Indian monsoon:1||Industrial area:1||Ingenuity pathway analysis:1||Intertidal sediments:1||Intertropical convergence zone (ITCZ):1||Iris pseudoacorus:1||Isotope ecology:1||Isotope physiology:1||Isotopic baseline:1||Isotopic niche:1||Isotopic niche space:1||Japan Sea:1||Jeju Island:1||Jeongokri:1||KMnO4 oxidation:1||KOBrKOH treatment:1||Kdparticle:1||King George island:1||Kjedahl method:1||Kongsfjorden Bay:1||Kuroshio Extension:1||LANDFAST ICE:1||LIPID BIOMARKER:1||Lake Hwaong:1||Larus crassirostris:1||Last deglaciation:1||Last glacial period:1||Lead:1||Life cycle:1||Life history traits:1||Life parameter:1||Life span:1||Lignin phenols:1||Lipid molecular:1||Lipogenesis:1||London Convention:1||London Protocol:1||Long chain alkyl diols:1||Long chain diol index:1||Long chain diols:1||Longchain diols:1||Longline sea squirt and oyster aquaculture:1||M. aeruginosa:1||MANJAVACAS ROTIFERA:1||MATTER:1||MAXIMUMLIKELIHOOD:1||MCMURDO SOUND:1||METHANE OXIDATION:1||MIDI:1||MOLECULAR CHARACTERIZATION:1||MS:1||Mackenzie Shelf:1||Mackenzie trough:1||Macroinvertebrate:1||Magnification:1||Malathion:1||Manganese superoxide dismutase:1||Manila clam (Ruditapes philippinarum):1||Marian cove (62 degrees 13 ' S 58 degrees 47 ' W):1||Marine aerosol:1||Marine benthic diatoms:1||Marine bivalves:1||Marine invertebrate:1||Marine mammal:1||Mechanism:1||Mekong River Delta:1||Membrane fouling:1||Mesocosms:1||Metal response element:1||Metals:1||Metazoan and protistan diets:1||Methane:1||Methane (CH4):1||Microphytoplankton:1||MicrocystinLR:1||Microphytobenthos:1||Millet:1||MixSIR:1||Mokpo Coastal areas:1||Molecular biomarker:1||Molecular biomarkers:1||Monogonont rotifer:1||Morphological characteristics:1||Motility:1||Movement:1||Mud volcano:1||Multiple endpoints:1||Multiple sources:1||Mumun period:1||Mycobacterium gilvum PYRGCK:1||Mycosporinelike amino acids (MAAs):1||NANOPARTICLES:1||NASSARIUSNITIDUS:1||NEWPARTICLE FORMATION:1||NITROGEN:1||NITROGEN ISOTOPES:1||NITROGEN ISOTOPIC COMPOSITION:1||NONYLPHENOL ETHOXYLATES:1||NRF2:1||NUCLEATION:1||NYALESUND:1||Nakdong River:1||Niche competition:1||Nitrate:1||Nitrate flux:1||Nitrate isotope:1||Nitrate source:1||Nitrogen budget:1||Nitrous oxide (N2O):1||Nonbiodegradable organic matter:1||Nonpoint sources:1||Nonylphenol:1||Northwest pacific ocean:1||Nuisance bloom:1||OCEAN:1||ORGANICMATTER SOURCES:1||ORGANOTIN CONTAMINATION:1||OXYGEN:1||Ocean acidification:1||Ocean dumping:1||Ojiri의 건중량당 흡수 효율이 더 높지만 (Short and McRoy1984) 질소 이용율은 일반적으로 수층보다 퇴적물에서높다(Boon 1986:1||Oligobrachia haakonmosbiensis:1||Olive flounder:1||Open estuary:1||Organic carbon:1||Organic carbonnormalized binding coefficient:1||Organic matter sources:1||Organochlorine pesticides:1||Origin:1||Oversummering:1||Oxic condition:1||Oyster:1||Pglycoprotein:1||PATCH SIZE:1||PCB:1||PCDD/Fs:1||PERSISTENT ORGANIC POLLUTANTS:1||PHENANTHRENE:1||PHYTOPLANKTON:1||PIP25 index:1||PLASTIC DEBRIS:1||PLATELET ICE:1||PMF model:1||POC:1||POLYCYCLIC AROMATICHYDROCARBONS:1||POLYETHOXYLATES:1||POPs:1||PRESERVATION METHODS:1||PROTEIN:1||PUFA:1||Pacific Arctic:1||Pacific Arctic Ocean:1||Paldang:1||Paleo SST:1||Paleotemperature:1||Paleoceanography:1||Paleoclimate:1||Paleoclimatology:1||Paleonutrient proxy:1||Paralia sp.:1||Parallel factor analysis (PARAFAC):1||Passive sampling:1||Periphytic algae:1||Persistent organic pollutants (POPS):1||Persistent organic pollutants (POPs):1||Petroleum:1||Phaeocystis:1||Phaeocystis sp.:1||Photoprotective pigment:1||Photosynthesis:1||Pigment:1||Pleistocene:1||Pohang Basin:1||Pollution:1||Polychlorinated biphenyl:1||Polycyclic aromatic hydrocarbons:1||Polycyclic aromatic hydrocarbons (PAHs):1||Pore water:1||Porosira glacialis:1||Principal component regression:1||Proboscia diatoms:1||Proteomics:1||Pseudobagrus fulvidraco:1||Pulse amplitude modulated (PAM) fluorometry:1||QUANTIFICATION:1||QUANTITATIVE PCR:1||REPRODUCTION:1||RESONANCE MASSSPECTROMETRY:1||RIVER ESTUARY:1||RNA sequencing:1||Radon:1||Reactive oxygen species:1||Red mud:1||Remote sensing:1||Removal rate:1||Repair:1||Risk assessment:1||Rivertype reservoir:1||Riverine organic carbon:1||Rock Shell:1||Ross Sea:1||S. arcaeformis:1||S. woodiana:1||SECOCD:1||SEDIMENT:1||SEDIMENTS:1||SEWAGESLUDGE:1||SHELF:1||SIBER:1||SIR2:1||SMEGMATIS:1||SOUTH CHINA SEA:1||SOUTHERNCALIFORNIA:1||SOUTHERNOCEAN:1||SPATIAL VARIABILITY:1||SPE extraction:1||SPECTRA:1||STABLEISOTOPES:1||SULFATE:1||SULFATEREDUCING BACTERIA:1||SULFURICACID:1||SURFACE WATERS:1||SURVIVAL:1||SVALBARD ISLANDS:1||Sea surface temperature (SST):1||Seabird eggs:1||Season:1||Seawater:1||Seawater exchange:1||Sediment core:1||Sediment exposure:1||Sediment oxygen consumption:1||Sediment quality:1||Sediment resuspension:1||Sedimentary organic matter:1||Seomjin River:1||Sequential extraction:1||Sherlock microbial identification system:1||Shikimate:1||Shipyard:1||Siboglinid tubeworm:1||Siloxanes:1||Simultaneous extraction:1||Singil Stream:1||Sinking particle:1||Size exclusion chromatography:1||Soil organic carbon:1||Soluble microbial products:1||Source fingerprinting:1||Source tracking tools:1||Sources:1||Southeastern Yellow Sea Mud:1||Southern East Sea:1||Spectrophotometry:1||Spectroscopic indices:1||Stable carbon isotope (δ13C):1||Stable isotope labeling:1||Stable isotope tracer:1||Stable isotopic compositions:1||Stable nitrogen isotope (δ15N):1||Stable organic carbon isotope:1||Stephanodiscus sp.:1||Sterols:1||Stockholm Convention:1||Storm event:1||Submarine groundwater discharge:1||Sulfate reduction bacteria:1||Superoxide dismutase:1||Surface nutrient proxy:1||Surface sediment:1||Suspended particulate matter:1||Synchronous fluorescence spectra:1||Synthetic musk compounds:1||TBT:1||TEMPORAL TRENDS:1||TEQs:1||THAISCLAVIGERA:1||TIGRIOPUSJAPONICUS:1||TMF:1||TRIBUTYLTIN POLLUTION:1||Tandem duplication:1||Temporal change:1||Temporal trend:1||Terrestrial input:1||Terrestrial organic carbon:1||Tetraslemis suecica:1||Thalassiosira sp.:1||The Yellow Sea:1||Tidal flat:1||Tidal power plant:1||Tidewater glacier:1||Tigriopus kingsejongensis:1||Toxic metal:1||Trace metal pollution:1||Traceability:1||Transcriptome analysis:1||Triacylglycerol:1||Trophic levels:1||Trophic magnification factor:1||Trophic magnification factor (TMF):1||Trophic magnification factors:1||Trophic state:1||Two source mixing model:1||Twodimensional correlation spectroscopy (2DCOS):1||U37(K '):1||U. douglasiae:1||UK′37:1||UV irradiation:1||UVB radiation:1||UVabsorbing compounds:1||UVradiation:1||Unsaturation index:1||VANBAALENII PYR1:1||WATER TREATMENT PLANTS:1||WEDDELL SEA:1||Wastewater:1||Wastewater treatment:1||Water accommodated fraction:1||Water accommodated fraction WAF:1||Western Arctic Ocean:1||Wetland food web:1||XRF core scanning:1||YELLOW SEA:1||Yellow Sea Cold Water Mass:1||Yeongheung Island:1||Youngsan river estuary:1||Z. marina:1||ZOSTERANOLTII:1||Zooplankton:1||^13C tracer method:1||absolute mineral composition:1||agricultural application:1||agricultural reservoir:1||agrochemicals:1||alkenones:1||alkylphenols:1||allelopathy:1||allochthonous:1||allochthonous inputs:1||amino acidspecific isotope analysis:1||anadromous fish:1||anthropogenic landuse:1||antioxidant defense:1||antioxidants:1||aquaculture:1||aryl hydrocarbon receptor:1||autochthonous:1||bacteria:1||benthic environment:1||benthic macroinvertebrates:1||benthicpelagic coupling:1||bioactive peptides:1||bioactivity:1||bioassay:1||biodiversity:1||biological activities:1||biopolymeric carbon (BPC):1||body size:1||brassicasterol:1||byproduct:1||cHABs:1||carbon:1||carbon and nitrogen isotope:1||carbon and nitrogen stable isotope ratios:1||carbon and nitrogen stable isotopes:1||carbon isotopes:1||carbon stable isotope:1||carbon stable isotope ratio:1||carbon transport:1||carbonisotope:1||chemosynthesis:1||chitooligosaccharides:1||chlorophylla size fraction:1||chlorophyllα:1||chlrophyll (chl) a:1||classification:1||combustion&#8211:1||community index:1||community wide metrics:1||complete mitochondrial genome:1||compound specific isotopes analysis (CSIA):1||compoundspecific amino acid analysis:1||compoundspecific isotope:1||compoundspecific stable isotope analysis:1||continuous weir:1||copper:1||cosmeceutical:1||cyanobacteria:1||d(13)C:1||dam impact:1||delta C13 values:1||diet estimate:1||diet source:1||dimethylsulphoniumpropionate (DMSP):1||discards:1||disinfectants:1||dissolved organic matter (DOM):1||dissolved organic matter component:1||dsrAB gene:1||dualisotopes:1||ecosystem linkage:1||empirical model:1||environmental assessment:1||environmental factors:1||environmental forensic:1||enzyme:1||epibrassicasterol:1||epilithon:1||epiphyte:1||excitationemission matrix:1||feeding behavior:1||feeding ecology:1||fish community:1||fish muscle:1||fish proteins:1||fishery byproduct:1||food source:1||food webs:1||foodweb:1||forensic:1||gas hydrate:1||gelatinous zooplankton:1||generalists:1||geographic origin:1||geomorphic characteristics:1||growth:1||habitat condition:1||heavy metals:1||helical grain:1||heterotrophic source:1||highly branched isoprenoid:1||household chemical product:1||human health:1||hybrid rocket:1||ice proxy:1||indicator species:1||intraextracellular:1||invasive species:1||isotope differentiation:1||isotope ratio mass spectrometry:1||isotope ratio mass spectrometry (GC&#8211:1||kelp beds:1||krill:1||lab on a chip:1||lagoon:1||lakes:1||land use:1||lipid biomarkers:1||machine learning:1||macrotidal estuary:1||malachite green:1||manila clam:1||marine:1||marine environment:1||mcrA gene:1||meiofauna:1||melt pond:1||metal wire:1||metallothioneinlike proteins:1||metallothioneins:1||methane:1||methane oxidation:1||microbial degradation:1||microfluidic sensor:1||microplastic:1||minke whale:1||mixing model:1||monsoon period:1||mud flat:1||mud volcano:1||mycosporinelike amino acids (MAAs):1||nanoplastic:1||neanthes succinea:1||nitrogen:1||nitrogen and carbon composition:1||nitrogen content:1||nitrogen isotope analysis:1||nitrogen source trace:1||nitrogen stable isotope ratio:1||nonbiodegradable organic matter:1||nonoxidized organic matter:1||nutrient:1||ocean dumping:1||organic carbon:1||organic matter:1||organic matters:1||organomineral interactions:1||organochlorine:1||organophosphate:1||origin of organic matter:1||oxidative stress:1||p38 MAPK:1||p53:1||paleoceanography:1||parallel factor analysis:1||particulate organic matter:1||periphyton:1||pesticide:1||pesticide residues:1||photoprotective compounds:1||pigment production rate:1||pollutant:1||pollutant tracking:1||polychaetes:1||precautionary principle:1||primary production:1||production:1||protein hydrolysate:1||radiocarbon:1||rainy season:1||regression rate:1||regulated river:1||relative mineral composition:1||resource competition:1||restoration:1||river:1||river continuum:1||river food web:1||saponification:1||sea surface temperature:1||sediment pollution:1||shrimp:1||sinking particle:1||siphonophore:1||size fraction:1||skin health:1||soil:1||source amino acids:1||specialists:1||species identification:1||stable carbon isotope:1||stable carbon isotopes:1||stable isotope composition:1||stable isotope probing technique:1||stable isotope ratio:1||stable isotope ratios:1||stable nitrogen isotope:1||styrene oligomers:1||succession:1||sulfatemethane transition zone:1||summer monsoon:1||surfaceenhanced Raman spectroscopy:1||taxonomic composition:1||terrestrial input:1||total organic carbon:1||toxic cyanobacteria:1||toxic microcystin:1||trace analysis:1||traceability:1||trophic amino acids:1||trophic dynamics:1||trophic enrichment:1||trophic interaction:1||trophic niche:1||trophic structure:1||ultrafiltration membrane reactor:1||ultraviolet radiation (UVR):1||unintended pollution:1||vertical differences:1||water management:1||weir impacts:1||xanthophyll compound:1||xanthophyll pigment:1||갯지렁이:1||과거 해수면온도:1||군집지수:1||글루타치온 S전이효소:1||금속결합 단백질:1||깔따구류:1||다이아지논:1||다환방향족탄화수소:1||동위원소생리학:1||동위원소생태학:1||동해:1||디디브이피:1||먹이질:1||미량금속:1||보의 영향:1||복원:1||부유 입자에의 흡착계수:1||산지 판별:1||상대광물조성:1||생물검정:1||생물농축:1||생체지표:1||서북극해:1||석영:1||스티렌올리고머:1||시화호:1||아릴탄화수소수용체:1||알킬페놀:1||유기인계 농약:1||유기인계농약:1||장족형 다이올:1||저서생태계:1||절대광물조성:1||정량X선회절분석:1||제주니질대:1||탄소·질소 안정동위원소비:1||퇴적물:1||퇴적토:1||퇴적토 관리:1||표층퇴적물:1||한국남해니질대:1||화합물 안정동위원소:1||황해 남동 니질대:1||황해 중앙 니질대:1||13C labeled diet uptake:1||흑산니질대:1||16S rRNA:1||18:1 omega 7:1||18:3 omega 6:1||8.2ka cooling event:1||?C14:1||ACE inhibitory activity:1||ACID TREATMENT:1||ACIDS:1||ALEUTIAN LOW:1||ALKENONES:1||ALKYLPHENOLS:1||AMINOACIDS:1||ANAEROBIC OXIDATION:1||ANOMALOUS CONDITIONS:1||AOM:1||AQUATIC FOODWEB:1||AQUATIC ORGANIC MATERIALS:1||ARCHAEAL LIPID BIOMARKERS:1||ARCTICOCEAN:1||ARNT:1||ATLANTICOCEAN:1||ATMOSPHERIC DIMETHYL SULFIDE:1||Adelie Penguin:1||Adenosine5' triphosphate (ATP):1||Adsorption:1||Adverse Biological Effect:1||Ag+impregnated silica column:1||Aged carbon export:1||Aging:1||Agricultural reservoir:1||Agricultural watershed:1||AhR:1||AhR activity:1||Algae:1||Algae Chlorophyll a fluorescence:1||Algal bloom water:1||Alkaline extractable organic matter:1||Alkenone unsaturation index:1||Amino acid isotope:1||Antarctic:1||Antarctic Peninsula:1||Antarctic copepod:1||Antarctic seabirds:1||Antarctica:1||Antifouling paint:1||Antimicrobials:1||Antioxidant:1||Antioxidant enzyme:1||Antioxidant genes:1||Aquatic invertebrate:1||Artificial barrier:1||Asan bay:1||Assimilation:1||BEHTBP:1||BIOGEOCHEMISTRY:1||BIOTRANSFORMATION:1||BSAF:1||Bay of Bengal:1||Bayesian isotope mixing model:1||Bengal Fan:1||Benthic community:1||Benthic nutrient flux:1||Benthicpelagic coupling:1||Benzo[a]pyrene:1||Benzo[alpha]pyrene:1||Bioaccumulation:1||Biocides:1||Biocontrol:1||Biodegradable dissolved organic carbon:1||Biodilution:1||Biological effects:1||Biological factors:1||Biomagnification:1||Biomagnification factor:1||Biomanipulation:1||Bioremediation:1||Biotransformation:1||Blacktailed gull:1||Blubber:1||Butyltin:1||C and N stable isotopes:1||C&#8211:1||C13):1||C. ELEGANS:1||CANCER:1||CARBONATE REMOVAL:1||CASCADIA MARGIN:1||CELL:1||CHUKCHISEA:1||CLOUD CONDENSATION NUCLEI:1||CLUSTER:1||CO 2 emissions:1||COASTAL WATERS:1||COI sequencing:1||CONSUMPTION:1||CONTINENTALSHELF:1||CONTINENTALSLOPE:1||CONVERGENT MARGIN:1||COST:1||CRUDEOIL:1||CSIA:1||CYP:1||Cambridge Bay:1||Carbon and nitrogen isotope:1||Carbon dioxide (CO2):1||Carbon isotopic composition:1||Carbon isotopic composition (&#948:1||Carbon stable isotope ratios:1||Caribbean:1||Caridina denticulata:1||Central Yellow Sea Mud:1||Cetacean:1||Chironomids:1||Chla (chlorophyll a):1||Chlorophyll a:1||Chlorpyrifos:1||Cholinesterase:1||Chromium:1||Chukchi Sea:1||Clam Ruditapes philippinarum:1||Closed estuary:1||Coastal food web:1||Coastal lake:1||Coastal organisms:1||Coastal sea:1||Coastal sediment:1||Complex river catchment:1||Compound specific isotope:1||Compound specific isotope analysis:1||Compound specific isotopes:1||Compoundspecific carbon isotopes:1||Controlling factors:1||Copepod Paracyclopina nana:1||Copepod Tigriopus japonicus:1||Copper and zinc superoxide dismutase:1||Crassostrea gigas:1||Crude oil dispersed sediments:1||Culture:1||Cyanobacterial toxin:1||DBDPE:1||DEGRADATIONPRODUCTS:1||DEGRADING BACTERIA:1||DELTAC13:1||DELTAN15 VALUES:1||DEPOSITION:1||DIAGRAM:1||DIATOM ASSEMBLAGES:1||DNA repair:1||DOGWHELK NUCELLALAPILLUS:1||Daphnia magna:1||Dechlorane:1||Degradation:1||Denitrification:1||Dennison et al. 1987). 그러므로 퇴적물은 뿌리를 내리고 사는 해초에게 중요한 영양염 공급처이다. 그러나 잎과 뿌리가 해초의 성장에 기여하는 정도를 추정해보면 잎과 뿌리 모:1||Desaturase:1||Diaphanosoma celebensis:1||Diet contribution:1||Diet source:1||Digital Vernier Caliper:1||Dike construction:1||Discrimination:1||Dissolved inorganic carbon:1||Dissolved organic carbon:1||Dissolved organic matter (DOM) fluorescence:1||Dissolved organic nitrogen:1||Distribution coefficient:1||EAST ANTARCTICA:1||EEMPARAFAC modeling:1||ELECTROSPRAY:1||EMILIANIAHUXLEYI PRYMNESIOPHYCEAE:1||ENVIRONMENT:1||EST:1||ESTUARY:1||ETHOXYLATES:1||EVOLUTION:1||EXPRESSION:1||EXTENDS LIFESPAN:1||East Asian Monsoon:1||East Asian monsoon:1||East Asian summer monsoon (EASM):1||East Sea:1||East Sea of Korea:1||Eastern South Sea:1||Eastern tropical pacific:1||Ecological risk assessment:1||Ecotoxicology:1||Effectdirected analysis:1||Elongase:1||Emperor Penguin:1||End member mixing:1||End member mixing analysis:1||Endangered amphibian species:1||Endogenous:1||Environmental stressors:1||Enzymatic activity:1||Estuarine DOC:1||Estuarine rotifer:1||Euphausia pacifica:1||Excitationemission matrix (EEM):1||Exogenous:1||Extracellular polymeric substances (EPS):1||Extreme event:1||FRACTIONATION:1||FTICR MS:1||Fall phytoplankton bloom:1||Fatty acid composition:1||Fatty acid synthesis:1||Fecundity:1||Filter feeders:1||Finespotted flounder:1||Fish:1||Fjords:1||Flame retardant:1||Fluorescence indices:1||Fluorescence property:1||Fluorometry:1||Food quality:1||Fossil organic carbon:1||Fouriertransform ion cyclotron resonance mass spectrometry (FTICRMS):1||GAS:1||GAS HYDRATE:1||GC:1||

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