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Bibliographic Details
Main Authors: Tsoy, Ira B, Prushkovskaya, Irina
Format: Dataset Open Access
Language:en
Published: PANGAEA 2019
Subjects:
A12-4; Achnanthes sp.; Actinocyclus cf. curvatulus; Actinocyclus curvatulus; Actinocyclus octonarius; Actinoptychus senarius; Amphora crassa; Amphora laevis; Amphora obtusa; Amphora proteus; Amur Bay; Arachnoidiscus ehrenbergii; Ardissonea formosa; Aulacodiscus affinis; Aulacoseira granulata; Aulacoseira islandica; Aulacoseira italica; Aulacoseira ovata; Aulacoseira praegranulata var. praeislandica; Aulacoseira praegranulata var. praeislandica forma curvata; Auliscus sculptus; Bacillariophyceae; Biddulphia biddulphiana; Calculated; Caloneis linearis; Campylodiscus angularis; Campylodiscus echeneis; Campylodiscus fastuosus; Chaetoceros debilis; Chaetoceros diadema; Chaetoceros ingolfianus; Chaetoceros lorenzianus; Chaetoceros mitra; Chaetoceros spp.; Cocconeis californica; Cocconeis costata; Cocconeis pellucida; Cocconeis placentula; Cocconeis pseudomarginata; Cocconeis scutellum; Cocconeis speciosa; Cocconeis vitrea; Coronia daemeliana; Coronia decora; Coscinodiscus asteromphalus; Coscinodiscus marginatus; Coscinodiscus oculus-iridis; Coscinodiscus radiatus; Counted; Cyclotella caspia; Cyclotella litoralis; Cymbella aspera; Cymbella australica; Cymbella spp.; Cymbella tumida; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Diatoma sp.; diatoms; Dictyocha fibula; Dictyocha messanensis forma spinosa; Didymosphenia geminata; Diploneis crabro; Diploneis interrupta; Diploneis ovalis; Diploneis smithii; Diploneis smithii var. rhombica; Diploneis spp.; Diploneis subcincta; Diploneis suborbicularis; Ditylum brightwellii; Epithemia adnata; Epithemia gibba; Eunotia praerupta; Eunotia serra; GC; Giffenia cocconeiformis; Glyphodesmis williamsonii; Gomphonema spp.; Grammatophora hamulifera; Grammatophora marina; Grammatophora oceanica; Grammatophora oceanica var. subtilissima; Gravity corer; Halamphora costata; Hantzschia amphioxys; Hyalodiscus scoticus; Japan Sea; Lyrella lyra; Lyrella lyroides; Lyrella spectabilis; Melosira moniliformis var. octogona; Meridion circulare; Navicula directa; Navicula lanceolata; Navicula pennata; Navicula spp.; Nitzschia angularis; Nitzschia insignis; Nitzschia lanceolata; Nitzschia scabra; Nitzschia spp.; Octactis octonaria; Octactis speculum; Odontella aurita; Odontidium anceps; Paralia sulcata; Petroneis glacialis; Petroneis granulata; Pinnularia borealis; Pinnularia episcopalis; Pinnularia lata; Pinnularia quadratarea; Pinnularia quadratarea var. constricta; Pinnularia viridis; Pinnularia viridis var. intermedia; Placoneis undulata; Plagiogramma staurophorum; Pleurosigma formosum; Porosira glacialis; Psammodiscus nitidus; Rhabdonema adriaticum; Rhabdonema arcuatum var. ventricosum; Rhaphoneis amphiceros; Rhizosolenia setigera; Rhoicosphenia marina; Rhopalodia musculus; Seminavis ventricosa; Shionodiscus biporus; silicoflagellates; Silicoflagellates; Skeletonema costatum; Stauroneis phoenicenteron; Staurosirella martyi; Stephanocha speculum var. minuta; Surirella fastuosa; Surirella splendida; Tabularia fasciculata; Tetracyclus rupestris; Thalassionema frauenfeldii; Thalassionema nitzschioides; Thalassiosira eccentrica; Thalassiosira spp.; Trachyneis aspera; Trigonium arcticum; Trigonium arcticum forma baleanum; Tryblionella calida; Tryblionella compressa; Tryblionella granulata; Tryblionella hungarica; Tryblionella littoralis; Ulnaria ulna
Online Access:https://doi.org/10.1594/PANGAEA.898638
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Table of Contents:
  • Diatoms and silicoflagellates from sediments in Amur Bay (Japan Sea) were analyzed with high temporal resolution to examine changes over the last 150 years. The age of sediments was estimated from unsupported 210Pb controlled by 137Cs. Siliceous microalgae examined in each cm of two sediment cores demonstrated significant changes in the ecological structure of the assemblages that reflected changes in sedimentation conditions. The obtained data suggest that the environmental changes over the last 150 years in Amur Bay are associated with the weakening of river runoff due to deforestation, sea level rise caused by global warming, and the increase of siliceous microplankton productivity that resulted in the formation of seasonal bottom hypoxia.