_自然環境と生態リスク
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2 III III II (10 12 m -2 ) (kg m -2 yr -1 ) (kg yr -1 ) (kg m -2 ) x (10 12 m -2 ) (kg m -2 yr -1 ) (kg yr -1 ) (kg m -2 ) x x x x x x x x x x x x x II nm m IV V I 0.1mm Fig A scanning electron micrograph of a centric diatom, Asteromphalus heptacles. 10 Fig. 3.9 Scanning electron micrograph of Thalassiosira, a coastal diatom, clearly showing the epitheca, hypotheca, and a connecting girdle of cell wall material. : Coscinodiscus
3 0.3mm 0.3mm Fig Scanning electron micrographs of some common marine dinoflagellates: (a) Gonyaulax polygramma, (b) Dinophysis rapa, (c) Gonyaulax sp., and (d) Ceratochoris horrida. All are microns in diameter. : Chaetoceros : Thalassiothrix 2, mm 0.3mm : Gymnodinium : Ceratium : Ceratium IX 6C H 2 C 6 H H 2 2 V II II 20µm
4 X II 2HC Ca 2+ CaC 3 + H 2 + C 2 2 V 20µm II C H 2 C 6 H H 2 0 N PSi, DNA, RNA, ATP, etc. Phytoplankton can grow explosively over a few days or weeks. This pair of satellite images shows a bloom that formed east of New Zealand between ctober 11 and ctober 25, (NASA images by Robert Simmon and Jesse Allen, based on MDIS data.) 31 Phytoplankton can grow explosively over a few days or weeks. This pair of satellite images shows a bloom that formed east of New Zealand between ctober 11 and ctober 25, (NASA images by Robert Simmon and Jesse Allen, based on MDIS data.) year averages of the surface chl-a (mg m -3 ) observed by the SeaWiFS Satellite. 11-year averages of the surface chl-a (mg m -3 ) observed by the SeaWiFS Satellite
5 Figure'14.08:'Loca2on'of'world's'major'commercial'fisheries'and'the'tonnage' (in'millions)'of'the'total'fish'catch'for'2002. IX Figure'14.08:'Loca2on'of'world's'major'commercial'fisheries'and'the'tonnage' (in'millions)'of'the'total'fish'catch'for'2002. IX II C + 12H C H H 2 II II II
6 Ventilation (upwelling) C2 2 C2 C2 2 2HC Ca 2+ CaC 3 + H 2 + C 2 II XI C2 C2 2 Fig Principal regions of coastal upwelling (blue) and down-current areas of increased primary productivity (green). Figure'06.16B:'(b)'This'model'portrays'the'exchange'of'surface'and'deep'water'across'the'ocean'basins'as'a'conveyor'belt C2 C2 2 C 2 C 2 C 2 Surface ocean Deep ocean Bacteria Large phytoplankton Small phytoplankton Bacteria Deep consumers rganic carbon Zooplankton Microzooplankton C 2 Deep water formation C2 ~ 3,700 m ~ 100 m Sea floor Chisholm (2000) Nature 407:
7 諏訪ら 2010 海の研究19(1) 55 藤井 石田 2013 海洋と生物 炭酸カルシウムの溶解度の変化予測 プランクトンだけでなく 石灰質をもつ生物が影響を受ける I Ruttimann (2006) Nature Digest, ctober 3, p16-19 産業革命以前のpHは8.17 現在は8.05程度まで低下 温度はpHに影響しないが 炭酸カルシウムは低温 高圧 で溶解度が高い 極域で強く影響でると予測 写真 Discover Blue 写真 Discover Blue 炭酸カルシウムの溶解度の変化予測 産業革命以前のpHは8.17 現在は8.05程度まで低下 温度はpHに影響しないが 炭酸カルシウムは低温 高圧 で溶解度が高い 極域で強く影響でると予測
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