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海洋生物の生成する炭酸カルシウムのX線回折測定: 沖縄地域学リポジトリ

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(1)

Citation

沖縄工業高等専門学校紀要 = Bulletin of Okinawa National

College of Technology(9): 1-12

Issue Date

2015-03

URL

http://hdl.handle.net/20.500.12001/18711

(2)

ᾏὒ⏕≀ࡢ⏕ᡂࡍࡿⅣ㓟࢝ࣝࢩ࣒࢘ࡢ ; ⥺ᅇᢡ ᐃ

ᨻᮌΎᏕ㸪☾ᮧᑦᏊ㸪ᒣᮏᗈ⨾㸱 㸯Ἀ⦖ᕤᴗ㧗➼ᑓ㛛Ꮫᰯ ᶵᲔࢩࢫࢸ࣒ᕤᏛ⛉㸪Ἀ⦖ᕤᴗ㧗➼ᑓ㛛Ꮫᰯ ⏕≀㈨※ᕤᏛ⛉㸪 Ἀ⦖⨾ࡽᓥ㈈ᅋ   せ᪨ Ⅳ㓟࢝ࣝࢩ࣒࢘ࢆ୺ᡂศ࡜ࡍࡿࢺࢤࢫࢠ࣑ࢻࣜ࢖ࢩࡢ㦵᱁࡜࣍ࢱࢸ㈅ࡢ㈅Ẇ࡟ᑐࡋ࡚ࠊX ⥺ᅇᢡ ᐃ ࢆ⾜ࡗࡓࠋࡑࡢ⤖ᯝࠊ௨ୗࡢࡇ࡜ࡀ᫂ࡽ࠿࡜࡞ࡗࡓࠋ(1)ࢺࢤࢫࢠ࣑ࢻࣜ࢖ࢩࡢ㦵᱁ࡣࠊ‽Ᏻᐃࡢ࢔ࣛࢦ ࢼ࢖ࢺᵓ㐀࡛࠶ࡿࡀࠊඛ➃㒊ศ࡟㏆࠸࡯࡝≉ᐃࡢ⤖ᬗ᪉఩࡟㓄ྥࡍࡿࠋ(2)࣍ࢱࢸ㈅ࡢ㈅Ẇࡣ୺࡜ࡋ࡚࢝ ࣝࢧ࢖ࢺᵓ㐀࡜࢔ࣛࢦࢼ࢖ࢺᵓ㐀ࡢΰྜ࡜࡞ࡗ࡚࠸ࡿࠋࡓࡔࡋ㈅ᰕࡢ௜╔ࡍࡿ㡿ᇦࡣࠊ୺࡜ࡋ࡚࢔ࣛࢦ ࢼ࢖ࢺᵓ㐀࡜࡞ࡗ࡚࠸ࡿࠋ(3)ࢧࣥࢦ㦵᱁ࡢඛ➃㏆ഐ࠾ࡼࡧ࣍ࢱࢸ㈅Ẇࡢ⼖ࡘࡀ࠸㏆ഐ࡛ࡣࠊ≉ᐃࡢ࢔ࣛ ࢦࢼ࢖ࢺ⤖ᬗ᱁Ꮚ㠃࠿ࡽࡢᅇᢡࣆ࣮ࢡࡀపゅᗘഃ࡬ࢃࡎ࠿࡟ࢩࣇࢺࡍࡿࠋࡇࡢ⌮⏤ࡣࠊࢫࢺࣟࣥࢳ࣒࢘ ࡢᙳ㡪࡜᥎ ࡉࢀࡿࠋ ࣮࣮࢟࣡ࢻ㸸Ⅳ㓟࢝ࣝࢩ࣒࢘ࠊX ⥺ᅇᢡ ᐃࠊ࢔ࣛࢦࢼ࢖ࢺࠊ࢝ࣝࢧ࢖ࢺࠊࢺࢤࢫࢠ࣑ࢻࣜ࢖ࢩ࣍ࢱࢸ  㸯㸬⥴ゝ  㐀♋ࢧࣥࢦࡣ࢖ࢯࢠࣥࢳࣕࢡࡸࢡࣛࢤ࡞࡝ࡢ่⬊ື≀࡟ᒓࡍࡿࢧࣥࢦ⹸㸦࣏ࣜࣉ㸧ࡢ㞟ྜయ㸦⩌య㸧 ࡛࠶ࡿࡀࠊᾏỈࡢᰤ㣴ሷࢆ▼⅊໬ࡋ࡚ࢸ࣮ࣈࣝ≧ࠊⴥ≧ࠊᯞ≧ࠊሢ≧࡞࡝ᵝࠎ࡞ᙧ≧ࡢ㦵᱁ࢆᙧᡂࡋ࡚ ᡂ㛗ࡍࡿࠋ▼⅊໬ࡣయෆ࡟ඹ⏕ࡉࡏ࡚࠸ࡿ〓⹸⸴࡜࿧ࡤࢀࡿ᳜≀ࣉࣛࣥࢡࢺࣥࡀගྜᡂ࡟ࡼࡾ⏕⏘ࡍࡿ ᰤ㣴㸦ⅣỈ໬≀㸧ࢆࡶ࡜࡟ࠊ㐀㦵⣽⬊ࡢാࡁ࡟ࡼࡗ࡚▼⅊໬ẕᾮ࡜࢝ࣝࢩ࣒࢘࢖࢜ࣥࠊ࠾ࡼࡧⅣ㓟Ỉ⣲ ࢖࢜ࣥࡢࡼ࠺࡞⁐Ꮡ↓ᶵⅣ⣲ࡢ▼⅊໬཯ᛂ࡟ࡼࡗ࡚⏕ࡌࡿ࡜ࡉࢀ࡚࠸ࡿ㸯㸧ࠋࢧࣥࢦࡢ㦵᱁ࡣࠊᩳ᪉ᬗࡢ Ⅳ㓟࢝ࣝࢩ࣒࢘⤖ᬗ࡛࠶ࡿࠕAragonite㸸࢔ࣛࢦࢼ࢖ࢺ㸦࢔ࣛࣞ▼⤖ᬗ㸧࡛ࠖࠊ㦵᱁ࡢᚤ⣽ᵓ㐀ࡣ㔪≧࢔ ࣛࢦࢼ࢖ࢺ⤖ᬗࡢ㞟ྜ⤌⧊࡜࡞ࡗ࡚࠸ࡿࡇ࡜ࡀྂࡃ࠿ࡽ▱ࡽࢀ࡚࠸ࡿ㸰㸧ࠋࡋ࠿ࡋࡇࡢ࢔ࣛࢦࢼ࢖ࢺ⤖ᬗ ᵓ㐀ࡣⅣ㓟࢝ࣝࢩ࣒࢘ࡢ࡞࠿࡛ࡶ‽Ᏻᐃ⤌⧊࡛࠶ࡾࠊ470Υ௨ୖࡢ㧗 ⎔ቃୗ࡟ࡉࡽࡍ࡜ᖖ ᖖᅽ࡛Ᏻ ᐃ࡞⳻㠃య᱁ᏊࡢࠕCalcite㸸࢝ࣝࢧ࢖ࢺ㸦᪉ゎ▼⤖ᬗ㸧ࠖ࡟ኚ໬ࡍࡿࠋ⏕≀⏤᮶ࡢⅣ㓟࢝ࣝࢩ࣒࢘⤖ᬗࡣ ࢔ࣛࢦࢼ࢖ࢺࡀ୺࡛࠶ࡿࡀࠊ୍㒊ࡢ஧ᯛ㈅࡛ࡣ࢝ࣝࢧ࢖ࢺ࡜࢔ࣛࢦࢼ࢖ࢺࡀΰᅾࡋ࡚࠸ࡿࡶࡢࡀ࠶ࡿࠋ ஧┦ࡀΰᅾࡍࡿ⌮⏤ࡣࡼࡃศ࠿ࡗ࡚࠸࡞࠸ࡀࠊ஧ᯛ㈅ࡢ㈅ᰕࡀ௜╔ࡍࡿ㒊ศ࡛ࡣ㧗ᐦᗘࡢ࢔ࣛࢦࢼ࢖ࢺ ᵓ㐀࡛ࠊࡑࡢ௚ࡢ㒊ศ࡛ࡣపᐦᗘࡢ࢝ࣝࢧ࢖ࢺᵓ㐀࡜࡞ࡗ࡚࠾ࡾࠊࡇࡢ⌮⏤࡟㛵ࡋ࡚ࡣ 200 ᖺ᮶ࡢ㞴ၥ ࡜ゝࢃࢀ࡚࠸ࡿࠕ࢔ࣛࢦࢼ࢖ࢺ㸫࢝ࣝࢧ࢖ࢺၥ㢟ࠖ࡜ࡋ࡚▱ࡽࢀ࡚࠸ࡿ㸱㸧ࠋࡲࡔ᫂☜࡞⤖ㄽࡀฟ࡚࠸࡞ ࠸ࡀࠊᙉᗘࢆᚲせ࡜ࡍࡿሙᡤࡀ㧗ᐦᗘࡢ࢔ࣛࢦࢼ࢖ࢺ࡛࠶ࡿࡇ࡜࠿ࡽࠊᙉᗘ࡜ࡢ㛵㐃ࡀண᝿ࡉࢀࡿࠋ

(3)

ⴭ⪅ࡽࡣ୍㐃ࡢ◊✲࡛ᮌࡢᯞࡢࡼ࠺࡟୕ḟඖࡢ」㞧࡞㦵᱁ࢆᙧᡂࡍࡿᯞࢧࣥࢦ࡟╔┠ࡋࠊࡑࡢᯞࢧࣥ ࢦࡢ㦵᱁ᙧ≧ࡸ㦵᱁ᙉᗘ࡜⏕⫱⎔ቃ࡟㛵ࡍࡿ◊✲ࢆ⾜ࡗ࡚࠸ࡿ㸲㸧㸫㸴㸧ࠋᯞࢧࣥࢦࡣሢ≧ࢧࣥࢦ࡜ẚ࡭࡚ ᡂ㛗ࡀ᪩ࡃࠊᡂ㛗ࡍࡿ࡟ᚑࡗ࡚኱ࡁࡃᯞࢆᗈࡆࡿ≉ᚩࢆᣢࡘࡀࠊἼ࠶ࡓࡾ࡞࡝࡟ࡼࡗ࡚ᢡᦆࡋ࡚ࡋࡲ࠺ࠋ Ⅳ㓟࢝ࣝࢩ࣒࢘ࡢ⤖ᬗᵓ㐀࡜ᙉᗘ࡜ࡢ㛵ಀࢆ⪃࠼ࡓሙྜࠊᯞࢧࣥࢦ㦵᱁࡟࠾࠸࡚ࡶ࣍ࢱࢸ㈅ࡢࡼ࠺࡟ᙉ ᗘࡀᚲせ࡞㒊ศ࡜ࡑ࠺࡛࡞࠸㒊ศ࡜࡛⤖ᬗᵓ㐀ࡀ␗࡞ࡗ࡚࠸࡚ࡶ୙ᛮ㆟࡛ࡣ࡞࠸ࠋࡋ࠿ࡋࠊࡇࢀࡲ࡛ᯞ ࢧࣥࢦࡢ㦵᱁ࡢ⤖ᬗᵓ㐀ࢆヲ⣽࡟ㄪᰝࡋࡓ౛ࡣࡳ࠶ࡓࡽ࡞࠸ࠋࡲࡓࠊࢧࣥࢦࡢ▼⅊໬ࡢ㝿࡟ࡣᾏỈ୰࡟ ྵࡲࢀࡿᵝࠎ࡞໬Ꮫᡂศࡶ㦵᱁୰࡟ྲྀࡾ㎸ࢇ࡛࠸ࡿ࡜ࡉࢀࠊẚ㍑ⓗᡂ㛗ࡢ㐜࠸ࣁ࣐ࢧࣥࢦ࡞࡝ࡢሢ≧ࢧ ࣥࢦࢆᑐ㇟࡜ࡋ࡚໬Ꮫᡂศࢆᢳฟࡋࠊ㐣ཤࡢᆅ⌫つᶍࡢẼೃኚືࡢ᚟ඖ࡞࡝ࡀヨࡳࡽࢀ࡚࠸ࡿ㸴㸧ࠋ㐀♋ ࢧࣥࢦࡢ㦵᱁ᙧᡂ࣓࢝ࢽࢬ࣒࡟௚ࡢ໬Ꮫᡂศࡀᐤ୚ࡋ࡚࠸ࡿ࡜ࡍࢀࡤࠊᯞ≧ࢧࣥࢦࡣሢ≧ࢧࣥࢦ࡟ẚ࡭ ࡚ᡂ㛗ࡀ᪩࠸ࡓࡵࠊඛ➃ഃ࡜᰿ᮏഃ࡜࡛ࡣ⤖ᬗᵓ㐀࡟ఱࡽ࠿ࡢ㐪࠸ࡀㄆࡵࡽࢀࡿྍ⬟ᛶࡶ࠶ࡿࠋࡑࡇ࡛ ᮏ◊✲࡛ࡣࠊ㔠ᒓᮦᩱࡢ⤖ᬗᵓ㐀ࡢྠᐃ࡞࡝࡟ከ⏝ࡉࢀࡿ㹖⥺ᅇᢡ ᐃἲ㸦X-Ray diffraction method㸸 XRD㸧ࢆ฼⏝ࡋ࡚ࠊᯞࢧࣥࢦ㦵᱁ࡢ⤖ᬗᵓ㐀࡟ࡘ࠸࡚ㄪᰝࡍࡿࡇ࡜࡜ࡋࡓࠋࡲࡓẚ㍑ࡢࡓࡵ࡟༑ศᡂ㛗 ࡋࡓ࣍ࢱࢸ㈅ࡢ㈅Ẇ࡟ࡘ࠸࡚ࡶ㹖⥺ᅇᢡ ᐃࢆᐇ᪋ࡋࠊ࢔ࣛࢦࢼ࢖ࢺ㸫࢝ࣝࢧ࢖ࢺၥ㢟ࡢ☜ㄆࡶ⾜ࡗࡓࠋ   ౪ヨᮦ࠾ࡼࡧᐇ㦂᪉ἲ  ᯞࢧࣥࢦ㦵᱁   ౪ヨᮦࡢᯞࢧࣥࢦ㦵᱁ࡣࠊᅗ 1 ࡟♧ࡍࡼ࠺࡞඲㛗ࡀ⣙ 400mm ࡢࢺࢤࢫࢠ࣑ࢻࣜ࢖ࢩ㸦Acropora intermedia㸧ࡢ㦵᱁࡛࠶ࡿࠋࡇࡢࢺࢤࢫࢠ࣑ࢻࣜ࢖ࢩࡣἈ⦖⨾ࡽᾏỈ᪘㤋࡛㣫⫱ࡉࢀ࡚࠸ࡓࡶࡢ࡛ࠊ㣫⫱ ࡟࠶ࡓࡗ࡚ࡣỈ᪘㤋ࡢᒇୖ࡟タ⨨ࡉࢀࡓỈᵴ࡛⾜ࢃࢀࠊ㏆ᾏ࠿ࡽỮࡳୖࡆࡓᾏỈࢆỈ㉁ㄪᩚ࠾ࡼࡧ ᗘ ㄪᩚࡋ࡞࠸ࡲࡲࠊ᥃ࡅὶࡋࡢ≧ែ࡜ࡋࡓࠋ࡞࠾ࠊ᰿ᮏ㒊ศ࠿ࡽඛ➃㒊ศ࡟࠸ࡓࡿࡲ࡛࡟せࡍࡿᡂ㛗ᮇ㛫 ࡣࠊ࠾࠾ࡴࡡ 1 ᖺ࡛࠶ࡿࠋࡇࡢ㦵᱁࡟࠾࠸࡚ࠊᅗ 2㸦a㸧࡟♧ࡍࡼ࠺࡟ 5 ⟠ᡤࡢ ᐃ⟠ᡤࢆỴᐃࡋࠊᑠᆺ ୓⬟ษ᩿ᶵ㸦࣐ࣝࢺ࣮ MC110 ᨵ㸧ࢆ⏝࠸࡚ࠊ஝ᘧ᮲௳ࡢࡶ࡜ᅗ 2㸦b㸧࡟♧ࡍࡼ࠺࡟㦵᱁ࡢ୰ᚰ௜㏆ ࠿ࡽ 2~3mm ࡢⷧ∦ࢆษࡾฟࡋࡓࠋࡑࡢ㝿ࠊࢧࣥࢦ㦵᱁ࡢඛ➃᪉ྥࡀศ࠿ࡿࡼ࠺࡟༳ࢆ௜ࡅࡓࠋ  ࣍ࢱࢸ㈅Ẇ ẚ㍑ᑐ㇟࡜ࡋ࡚ࠊᅗ 3 ࡟♧ࡍ࣍ࢱࢸ㈅㸦Mizuhopecten yessoensis㸧ࡢ㈅Ẇࡶ⏝ពࡋࡓࠋࡇࡢ࣍ࢱࢸ㈅ࡣ

(a) Sampling position  (b)Shape of sample Fig.1 The skeleton of Acropora intermedia   Fig.2 Detail of XRD measurement sample

㸯 㸰 㸱 㸲 㸳 2~3mm 15mm

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໭ᾏ㐨㔝௜㒆ᑿᓃ἟ἢᓊࡢ᰿ᐊᾏᓙ࡛᱆⥙⁺࡟ࡼࡗ࡚⁺⋓ࡉࢀࡓࡶࡢ࡛࠶ࡾࠊ㈅Ẇࡢᶍᵝ࠿ࡽᖺ㱋 5 ᖺ ࡢᡂ㈅࡜᥎ ࡉࢀࡿࠋࡩࡃࡽࡳࡢᙅ࠸ẆࡀࠕᕥẆ㸦ࡉ࠿ࡃ㸧ࠖࠊࡩࡃࡽࡳࡢᙉ࠸ẆࡀࠕྑẆ㸦࠺࠿ࡃ㸧ࠖ ࡛࠶ࡿࠋࡇࡢ஧ᯛࡢ㈅Ẇ࠿ࡽᅗ 4㸦a㸧࡟♧ࡍࡼ࠺࡟⼖ࡘࡀ࠸㒊ศ࠿ࡽ஧ᮏࡢ┤⥺㸦୍ᮏࡣ㈅ᰕ㒊ศࢆ㏻ ࡾࠊࡶ࠺୍ᮏࡣ㈅ᰕ௜╔㒊ศࢆ㏻ࡽ࡞࠸㸧ࢆỴᐃࡋࠊࡑࡇ࠿ࡽ➼㛫㝸࡟ࢧࣥࣉࣜࣥࢢ᥇ྲྀ఩⨨ࢆỴᐃࡋ ࡓࠋ⼖ࡘࡀ࠸࠿ࡽ 15mm ࡢ఩⨨ࢆ No.1 ࡜ࡋ࡚ࠊࡑࡇ࠿ࡽ 10mm 㛫㝸ࡈ࡜࡟ࢧ࢖ࢬࡀ 5mm×5mm ࡢࢧࣥ ࣉࣝࢆࠊࢧࣥࢦ࡜ྠᵝ࡟ᑠᆺ୓⬟ษ᩿ᶵ࡟࡚ษࡾฟࡋࡓࠋ㈅ᰕࡀ௜╔ࡋ࡚࠸ࡓ㡿ᇦࡣࠊA-2ࠊA-3 ࠾ࡼࡧ C-2ࠊC-3 ࡢ㸲⟠ᡤ࡛࠶ࡿࠋ࡞࠾ ᐃࡣ㈅Ẇࡢෆ㠃ഃ࡜ࡋࡓࠋ  ; ⥺ᅇᢡ ᐃ  X ⥺ᅇᢡ ᐃ࡟ࡣᅗ 5 ࡟♧ࡍᓥὠ〇సᡤ〇ࡢ X ⥺ᅇᢡ⿦⨨㸦XRD-6100㸧ࢆ౑⏝ࡋࡓࠋ ᐃ࡟ࡣ Cu ⟶⌫ࢆ౑⏝ࡋࠊ⟶㟁ᅽ 50kVࠊ⟶㟁ὶ 35mA ࡢ X ⥺Ⓨ⏕᮲௳࡜ࡋࡓࠋࡲࡓࠊ ᐃ࡟㝿ࡋࠊNi ࣇ࢕ࣝࢱ࣮ ࠾ࡼࡧ 2mm ࡢࢫࣜࢵࢺࢆ౑⏝ࡋࡓࠋࢦࢽ࣓࣮࢜ࢱ㸦2ȟ㸧ࡢᅇ㌿ࡣࢫࢸࢵࣉゅ 0.02 degࠊ⛣ື㏿ᗘ 1.0 deg/min ࡜ࡋࠊ10㹼80 deg ࡢ⠊ᅖ࡟ࡘ࠸࡚ᅇᢡࣉࣟࣇ࢓࢖ࣝࢆ ᐃࡋࡓࠋࢧࣥࣉࣝࡢタ⨨ࡣࠊᅗ 6 ࡟♧ ࡍ࡜࠾ࡾ࡟タ⨨ࡋࡓࠋᅗ୰ࡢᯟ࡛ᅖࡲࢀࡓ㡿ᇦࡀᴫࡡ ᐃ⠊ᅖ࡜࡞ࡿࠋ࡞࠾ࠊ ᐃ࡟ࡼࡾᚓࡽࢀࡓ X ⥺ ᅇᢡࣉࣟࣇ࢓࢖ࣝࡣࠊࣇ࣮ࣜࢯࣇࢺ㸦PatView㸵㸧㸧ࢆ౑⏝ࡋ࡚ࠊࣂࢵࢡࢢࣛ࢘ࣥࢻࡢ㝖ཤࠊKȘ 2㝖ཤࠊ ࣆ࣮ࢡࢧ࣮ࢳࢆ⾜ࡗࡓࠋᚓࡽࢀࡓࣆ࣮ࢡࡣ American Mineralogist Crystal Structure Database㸸AMCSD 㸶㸧

࡟཰㘓ࡉࢀࡓⅣ㓟࢝ࣝࢩ࣒࢘ࡢ࢔ࣛࢦࢼ࢖ࢺ࡞ࡽࡧ࡟࢝ࣝࢧ࢖ࢺࡢࣆ࣮ࢡ࡜ẚ㍑᳨ウࢆ⾜ࡗࡓࠋ

(a) Left shell (b) Right shell Fig.3 The Shells of Mizuhopecten yessoensis

(a) Left shell    (b) Right shell Fig.4 Sampling position and shape of sample

Inside Inside

Outside Outside

(5)

Fig.5 XRD measurement equipment.  Fig.6 Example of sample setting 㸬 ᐃ⤖ᯝ  ᯞࢧࣥࢦ㦵᱁   ᯞࢧࣥࢦࡢ X ⥺ᅇᢡࣉࣟࣇ࢓࢖ࣝࢆᅗ 7 ࡟♧ࡍࠋࡲࡓᅗ࡟ࡣࠊࢹ࣮ࢱ࣮࣋ࢫ AMCSD ࡟࠶ࡿ⢊ᮎ࢔ࣛ ࢦࢼ࢖ࢺࡢࢹ࣮ࢱ࡟ࡘ࠸࡚ࠊྛ ᐃሙᡤࡢ㸦㸯㸯㸯㸧ᅇᢡࣆ࣮ࢡࢆ 100%࡜ᇶ‽໬ࡋࡓࣆ࣮ࢡᙉᗘẚࡶ ♧ࡋࡓ㸷㸧ࠋ ᐃࡉࢀࡓᅇᢡࣉࣟࣇ࢓࢖ࣝࡀࡇࡢࣆ࣮ࢡᙉᗘẚ࡜࡯ࡰ୍⮴ࡋ࡚࠸ࢀࡤࠊ ᐃヨᩱࡣ࢔ࣛࢦ ࢼ࢖ࢺࡢ⤖ᬗᵓ㐀࡛࠶ࡾࠊࡲࡓ⤖ᬗ᪉఩ࡀࣛࣥࢲ࣒࡟㓄ྥࡋ࡚࠸ࡿࡇ࡜ࢆព࿡ࡋ࡚࠸ࡿࠋᅗ 7 ࡟࠾࠸࡚ࠊ ᰿ᮏഃࡢ Position 1 ࡜ᯞࡀศᯞࡍࡿ๓ࡢ Position 2 ࡢࣉࣟࣇ࢓࢖ࣝࢆẚ㍑ࡍࡿ࡜ࠊ୧⪅ࡣ࡯ࡰ➼ࡋࡃ࠿ࡘ ࢹ࣮ࢱ࣮࣋ࢫ࡟グ㍕ࡉࢀࡓ⢊ᮎヨᩱࡢᙉᗘẚ࡜ࡶᴫࡡ୍⮴ࡋ࡚࠸ࡿࠋࡓࡔࡋࠊᅇᢡゅ 42.94 deg ࡟࠾ࡅ ࡿ㸦㸰㸰㸮㸧㠃࠿ࡽࡢᅇᢡࣆ࣮ࢡ࡜ࠊᅇᢡゅ 45.90 deg ࡟࠾ࡅࡿ㸦㸰㸰㸯㸧㠃࠿ࡽࡢᅇᢡࣆ࣮ࢡࡀࠊ⢊ ᮎヨᩱࡢࡶࡢࡼࡾࡸࡸ㧗ࡵࡢ್࡜࡞ࡗ࡚࠸ࡿࠋࡇࡢࡇ࡜ࡣࠊX ⥺ᅇᢡ ᐃ⟠ᡤ࡟ࡣ㸦㸰㸰㸮㸧ࡲࡓࡣ㸦㸰 㸰㸯㸧ࡢ᪉఩ࢆᣢࡗࡓ⤖ᬗࡀࠊ㏻ᖖࡼࡾከࡃᏑᅾࡋ࡚࠸ࡿࡇ࡜ࢆព࿡ࡋ࡚࠸ࡿࠋ࡞࠾ࠊ48 deg ௜㏆ࡢࣆ ࣮ࢡࡶ⢊ᮎヨᩱࡢࣆ࣮ࢡࡼࡾ㧗ࡵ࡜࡞ࡗ࡚࠸ࡿࡀࠊ㏆᥋ࡍࡿ஧ࡘࡢࣆ࣮ࢡ㸦㸮㸲㸯㸧㸸48.35 degࠊ㸦㸰㸮 㸰㸧㸸48.51 degࠊࡀ㔜࡞ࡾྜࡗࡓࡶࡢ࡛࠶ࡾࠊ㓄ྥࡢᙳ㡪࡛ࡣ࡞࠸ࠋ⥆࠸࡚ࠊPosition 1 ࠾ࡼࡧ Position 2 ࡢᘏ㛗࡛࠶ࡾࠊศᯞᚋࡢ Position 3 ࡟╔┠ࡍࡿ࡜ࠊ඲యⓗ࡞ഴྥࡣ Position 2 ࡜㢮ఝࡋ࡚࠸ࡿࡀࠊᅇᢡࣉ ࣟࣇ࢓࢖ࣝࡢ 42.06 degࠊ62.70 deg ࠾ࡼࡧ 75.16 deg ࡟ࠊᅗ୰[A]࡛♧ࡍࡼ࠺࡟᪂ࡓ࡞ࣆ࣮ࢡࢆ⏕ࡌ࡚࠸ࡿࠋ ࡓࡔࡋࡇࡢࣆ࣮ࢡࡣࠊ࢔ࣛࢦࢼ࢖ࢺࡢᅇᢡࣆ࣮ࢡ࡜ࡣ୍⮴ࡋ࡞࠸ࠋࡇࢀࡽࡢᅇᢡࣆ࣮ࢡࡣࠊPosition 2 ࡛ࡶࢃࡎ࠿࡟⏕ࡌ࡚࠸ࡿࡀࠊࡉࡽ࡟ศᯞࡋࡓᚋࡢඛ➃ഃࡢ Position 5 ࡟࠾࠸࡚ࡑࡢᙉᗘࡀ୍ẁ࡜㧗ࡃ࡞ ࡗ࡚࠸ࡿࠋࡍ࡞ࢃࡕࠊࡇࡢᯞࢧࣥࢦࡢඛ➃௜㏆࡟ࡣࠊୖ㏙ࡢ 3 ࡘࡢᅇᢡࣆ࣮ࢡࢆᣢࡘ⤖ᬗࡢ≀㉁ࡀᏑᅾ ࡋ࡚࠸ࡿࡇ࡜࡟࡞ࡿࠋ୍᪉࡛ࠊศᯞࡋࡓṧࡾࡢඛ➃ഃ㸦Position 4㸧࡛ࡣࠊᅗ୰[B]࡛♧ࡋࡓࣆ࣮ࢡࡀㄆࡵ ࡽࢀࡿࠋࡇࡢࣆ࣮ࢡࡣ୍ぢࡍࡿ࡜ඛࡢࣆ࣮ࢡ[A]࡜ྠ఩⨨ࡢࡼ࠺࡛࠶ࡿࡀࠊࡑࢀࡒࢀ࢔ࣛࢦࢼ࢖ࢺࡢᅇᢡ 㠃㸦㸰㸰㸮㸧㸸42.94 degࠊ㸦㸯㸳㸯㸧㸸63.39 degࠊ㸦㸲㸮㸮㸧㸸76.85 deg ࡜୍⮴ࡋ࡚࠸ࡿࠋࡘࡲࡾࠊࡇࡢ᪂ ࡓ࡟⏕ࡌࡓࣆ࣮ࢡ[A]ࡣࠊ࢔ࣛࢦࢼ࢖ࢺࡢᅇᢡ㠃㸦㸰㸰㸮㸧ࠊ㸦㸯㸳㸯㸧ࠊ㸦㸲㸮㸮㸧ࡢ୕ࡘࡢࣆ࣮ࢡࡀపゅ ᗘഃ࡬ࢩࣇࢺࡋࡓࡶࡢ࡜᥎ ࡉࢀࡿࠋ

Coral

(6)

Fig.7 XRD profiles of Acropora intermedia as shown in Fig.2(a).

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[ A ] [ A ] [ A ] [ A ] [ A ] [ A ] [ B ] [ B ] [ B ] (1 1 1) (2 2 0) (2 2 1) (0 4 1) (2 0 2) (1 5 1) (2 2 0) (2 0 4) (4 0 0)

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(7)

 ࣍ࢱࢸ㈅Ẇ  ࣍ࢱࢸ㈅Ẇ㸦ᕥẆ㸧 ᕥẆࡢ X ⥺ᅇᢡ ᐃ⤖ᯝࢆᅗ 8 ࡟♧ࡍࠋ࡞࠾ࠊᚤᑠ࡞ࣆ࣮ࢡ࡟ࡘ࠸᳨࡚ウࡍࡿࡓࡵࠊᅇᢡᙉᗘࡀ 0~10000cps ࡲ࡛ࢆᣑ኱ࡋ࡚♧ࡋ࡚࠸ࡿࠋᅇᢡࣉࣟࣇ࢓࢖ࣝ࡟ࡣ AMCSD ࡟࠾ࡅࡿ࢔ࣛࢦࢼ࢖ࢺࡢᅇᢡ ゅ㸷㸧ࠊ࢝ࣝࢧ࢖ࢺࡢᅇᢡゅ㸯㸮㸧࡟ࡘ࠸࡚♧ࡋࡓࠋᕥẆ࡛ࡣ ᐃ఩⨨ A-2 ࠾ࡼࡧ A-3 ࡟㈅ᰕࡀ௜╔ࡋ࡚࠸ ࡿࠋ⼖ࡘࡀ࠸㒊ศ࡟᭱ࡶ㏆࠸ ᐃ఩⨨ࠕA-1ࠖ࡟࠾࠸࡚ࡣࠊ࢝ࣝࢧ࢖ࢺࡢ⤖ᬗ᱁Ꮚ㸦㸯㸮㸲㸧㸸29.42 deg ࡢࣆ࣮ࢡࡀ௚ࡢᅇᢡ㠃࡟ẚ࡭࡚㢧ⴭ࡟ᙉࡃࠊ⥆࠸࡚㸦㸮㸯㸶㸧㸸47.54 deg ࡢࣆ࣮ࢡࡀ☜ㄆ࡛ࡁࡿࠋ㸦㸮㸯 㸶㸧ࡢࣆ࣮ࢡࡣࢹ࣮ࢱ࣮࣋ࢫ࡟ẚ࡭࡚㢧ⴭ࡟㧗࠸ࡇ࡜࠿ࡽࠊ㈅Ẇෆ㒊ࡢ⼖ࡘࡀ࠸㏆ࡃࡣࡇࡢ᪉ྥ࡟⤖ᬗ ࡀ㓄ྥࡋ࡚࠸ࡿ࡜ᛮࢃࢀࡿࠋࡲࡓࠊ77 deg ௜㏆࡟ࡶᅇᢡࣆ࣮ࢡࡀ☜ㄆ࡛ࡁࡿࡀࠊࡇࡢ఩⨨࡛ࡣ࢝ࣝࢧ࢖ ࢺ㸦㸯㸰㸶㸧㸸72.95 deg ࡜」ᩘࡢ࢔ࣛࢦࢼ࢖ࢺᅇᢡ㠃ࡀ㞄᥋ࡋ࡚࠾ࡾࠊ࢝ࣝࢧ࢖ࢺ㸦㸯㸰㸶㸧ࡢࣆ࣮ࢡ ᙉᗘẚࡀ㠀ᖖ࡟ᑠࡉ࠸ࡇ࡜ࢆ⪃៖ࡍࢀࡤࠊ࠾ࡑࡽࡃ࢔ࣛࢦࢼ࢖ࢺࡢࣆ࣮ࢡࡔ࡜ᛮࢃࢀࡿࠋࡲࡓࠊ58deg ௜㏆࡟ࡣࠊAMCSD ࡟グ㍕ࡉࢀࡓ࢔ࣛࢦࢼ࢖ࢺ࡞ࡽࡧ࡟࢝ࣝࢧ࢖ࢺࡢᅇᢡゅ࡜ࡣ୍⮴ࡋ࡞࠸ࣆ࣮ࢡࡀᏑ ᅾࡋ࡚࠸ࡿࠋࡇࡢ఩⨨࠿ࡽ㈅ᰕࡢ௜╔㒊ศ㸦 ᐃ఩⨨ A-2 ࠾ࡼࡧ A-3㸧࡟⛣⾜ࡍࡿ࡜ࠊᅇᢡࣉࣟࣇ࢓࢖ ࣝࡣ኱ࡁࡃኚ໬ࡍࡿࠋ࢝ࣝࢧ࢖ࢺ㸦㸯㸮㸲㸧ࠊ㸦㸮㸯㸶㸧ࡢᅇᢡࣆ࣮ࢡࡣᅗ୰ࡢᯟෆ࡛♧ࡋࡓࡼ࠺࡟㢧ⴭ ࡟ῶᑡࡋࠊࡑࡢ௦ࢃࡾ࡟࢔ࣛࢦࢼ࢖ࢺ㸦㸮㸮㸰㸧㸸31.17 deg ࡢࣆ࣮ࢡࡀ㢧ⴭ࡟㧗ࡃ࡞ࡿࠋࡲࡓࠊࡉࡁࡢ 58deg ௜㏆ࡢࣆ࣮ࢡࡶᾘ⁛ࡋࡓࠋ ᐃ఩⨨ࡀඛ➃ഃࡢ A-4 ࡟࡞ࡿ࡜࢝ࣝࢧ࢖ࢺ࡜࢔ࣛࢦࢼ࢖ࢺࡢࣆ࣮ࢡ ࡀΰᅾࡍࡿࡼ࠺࡟࡞ࡿࡀࠊ ᐃ఩⨨ A-5 ࡟࡞ࡿ࡜࢔ࣛࢦࢼ࢖ࢺࡢᅇᢡࣆ࣮ࢡࡣ 37 deg ࡜ 77 deg ௜㏆ࡢ ࡶࡢࢆ㝖ࡁぢࡽࢀ࡞ࡃ࡞ࡿࠋ୍᪉࡛ࠊ㈅ᰕࡢ௜╔ࡋ࡚࠸࡞࠸ ᐃ఩⨨ B ࢆࡳࡿ࡜ࠊ ᐃ఩⨨࡟ࡼࡽࡎ㢮 ఝࡢᅇᢡࣉࣟࣇ࢓࢖ࣝ࡜࡞ࡗ࡚࠸ࡿࠋࡲࡓࠊࡉࡁࡢ 58 deg ࡢࣆ࣮ࢡࡶ☜ㄆ࡛ࡁࡿࠋ࢝ࣝࢧ࢖ࢺࡢࣆ࣮ࢡ ࡢ୰࡛≉࡟ὀ┠ࡋࡓ࠸ࡢࡣࠊ47 deg ௜㏆ࡢ㸦㸮㸯㸶㸧࠾ࡼࡧ㸦㸯㸯㸴㸧ࡢࣆ࣮ࢡ࡛࠶ࡿࠋࡇࡢࣆ࣮ࢡࡣ ඛ➃࡟㏆࡙ࡃ࡟ᚑ࠸ῶᑡࡍࡿഴྥ࡟࠶ࡿࠋࡲࡓ ᐃ఩⨨ AࠊB ࡜ࡶ࡟ 77 deg ௜㏆ࡢᅇᢡࣆ࣮ࢡࡣ࢔ࣛࢦ ࢼ࢖ࢺࡢᅇᢡࣆ࣮ࢡ࡜ᛮࢃࢀࡿࡀࠊA-1 ࠾ࡼࡧ B-1 ࡛ࡣࠊపゅᗘഃ࡟͆Unknown peak͇࡛♧ࡋࡓࣆ࣮ࢡ ࡀ⏕ࡌ࡚࠸ࡿࠋ  ࣍ࢱࢸ㈅Ẇ㸦ྑẆ㸧 ⥆࠸࡚ྑẆࡢ X ⥺ᅇᢡ ᐃ⤖ᯝࢆᅗ 9 ࡟♧ࡍࠋ㈅ᰕࡢ௜╔఩⨨ࡣ ᐃ఩⨨ C-2 ࠾ࡼࡧ C-3 ࡛࠶ࡿࠋྑ Ẇ࡟࠾࠸࡚ࡶᕥẆࡢ ᐃ఩⨨ A-2ࠊA-3 ࡜ྠᵝ࡟㈅ᰕ௜╔㒊ศࡢ࢝ࣝࢧ࢖ࢺ㸦㸯㸮㸲㸧ࠊ㸦㸮㸯㸶㸧ࡢᅇ ᢡࣆ࣮ࢡࡀ㢧ⴭ࡟ῶᑡࡋࠊࡑࡢ௦ࢃࡾ࡟࢔ࣛࢦࢼ࢖ࢺ㸦㸮㸮㸰㸧㸸31.17 deg ࡢࣆ࣮ࢡࡀ㢧ⴭ࡟㧗ࡃ࡞ࡿ ഴྥࡀㄆࡵࡽࢀࡿࠋࡓࡔࡋࠊྑẆࡢ࡯࠺ࡀ࢔ࣛࢦࢼ࢖ࢺࡢᅇᢡࣆ࣮ࢡࡀከ࠸ഴྥ࡟࠶ࡿࠋ㈅ᰕࡢ௜╔ࡋ ࡚࠸࡞࠸ ᐃ఩⨨ D ࡟࠾࠸࡚ࡶࠊᇶᮏⓗ࡞ഴྥࡣᕥẆࡢ ᐃ఩⨨ B ࡜ྠࡌ࡛ࠊ࡯࡜ࢇ࡝࢝ࣝࢧ࢖ࢺ⤖ᬗ ࡢᅇᢡ㠃࠿ࡽࡢᅇᢡ࡛࠶ࡿࠋࡲࡓࠊ ᐃ఩⨨࡟ࡼࡿ 47 deg ௜㏆ࡢ㸦㸮㸯㸶㸧࠾ࡼࡧ㸦㸯㸯㸴㸧ࡢࣆ࣮ࢡ ࡢኚ໬ࡶ㢮ఝࡋ࡚࠸ࡿࠋྑẆ࡟࠾࠸࡚ࡶ ᐃ఩⨨ CࠊD ࡟ࡼࡽࡎ࢔ࣛࢦࢼ࢖ࢺࡢᅇᢡࣆ࣮ࢡ࡜ᛮࢃࢀࡿ 77 deg ௜㏆ࡢࣆ࣮ࢡ࡟╔┠ࡍࡿ࡜ࠊC-1 ࠾ࡼࡧ D-1 ࡛ࡣపゅᗘഃ࡟ࡶ࠺ࡦ࡜ࡘࣆ࣮ࢡࡀ⌧ࢀࡿࠋࡉࡽ࡟ࠊ ࡼࡃぢࡿ࡜ 42 deg ௜㏆࡟࠶ࡿᅇᢡࣆ࣮ࢡࡣࠊ⼖ࡘࡀ࠸㏆ഐࡢ C-1 ࠾ࡼࡧ D-1 ࡟࠾࠸࡚ࠊ͆Unknown peak͇ ࡛♧ࡋࡓࡼ࠺࡟ⱝᖸపゅᗘഃ࡬ࢩࣇࢺࡋ࡚࠸ࡿࠋ

(8)

Fig.8 XRD profiles of Mizuhopecten yessoensis (Left shell) 20 30 40 50 60 70 80 0 5000 10000 In te n sit y / cp s B-2 20 30 40 50 60 70 80 0 5000 10000 In te n si ty / c p s B-3 20 30 40 0 60 0 80 0 5000 10000 In te ns it y / c p s B-4 20 30 40 50 60 70 80 0 5000 10000 In te n si ty / c p s B-5 20 30 40 50 60 70 80 0 0 0 A-2 0 0 0 A-3 0 0 0 A-4 20 30 40 50 60 70 80 0 0 0 A-5 20 30 40 50 60 70 80 0 5000 10000 2 / deg In te n sity / c p s A-1 20 30 40 50 60 70 80 0 5000 10000 2 / deg In te n si ty / cp s B-1 Aragonite Calcite Aragonite Calcite C(104) C(018) A(002) C C C A A A C C A C A A C A C C C(018) C(116) C(116) Unknown peak Unknown peak A

(9)

Fig.9 XRD profiles of Mizuhopecten yessoensis (Right shell) 0 0 0 D-2 0 0 0 D-3 0 0 D-4 20 30 40 0 60 0 80 0 0 0 D-5 20 30 40 50 60 70 80 0 5000 10000 2 / deg In te n sity / c p s D-1 0 5000 10000 In te n si ty / c p s C-5 20 30 40 0 60 0 80 0 5000 10000 In te nsi ty / cps C-4 20 30 40 0 60 0 80 0 5000 10000 In te n sity / c p s C-3 0 5000 10000 In te n sity / c p s C-2 20 30 40 50 60 70 80 0 5000 10000 2 / deg In te n si ty / c p s C-1 Aragonite Calcite Aragonite Calcite C(104) C(018) A(002) A A C C(018) C(116) C(116) Unknown peak Unknown peak C(104)

(10)

㸬⪃ᐹ   ᯞࢧࣥࢦࡢ㦵᱁࡞ࡽࡧ࡟࣍ࢱࢸࡢ㈅Ẇࢆ X ⥺ᅇᢡࡋࡓ⤖ᯝࠊ࣍ࢱࢸ㈅Ẇࡣ ᐃ⟠ᡤ࡟ࡼࡗ࡚࢝ࣝࢧ ࢖ࢺ⤖ᬗ࡜࢔ࣛࢦࢼ࢖ࢺ⤖ᬗࡢΰྜ࡜࡞ࡗ࡚࠾ࡾࠊᯞࢧࣥࢦࡣ ᐃ⟠ᡤ࡟ࡼࡽࡎ࢔ࣛࢦࢼ࢖ࢺ⤖ᬗ࡛࠶ ࡿࡇ࡜ࡀศ࠿ࡗࡓࠋࡋ࠿ࡋᯞࢧࣥࢦࡢ⤖ᬗᵓ㐀ࢆㄪᰝࡋࡓ⤖ᯝࠊᅗ 7 ࡢ[A]࡛♧ࡋࡓࣆ࣮ࢡࡢࡼ࠺࡟࢔ࣛ ࢦࢼ࢖ࢺࡢᅇᢡ㠃࡟ᒓࡉ࡞࠸ゅᗘ࠿ࡽࡢᅇᢡࣆ࣮ࢡࡀほᐹࡉࢀࡓࠋࡇࡢࣆ࣮ࢡࡣᮏ᮶ࠊᅗ୰[B]࡛♧ࡋࡓ ࢔ࣛࢦࢼ࢖ࢺ⤖ᬗࡢ㸦㸰㸰㸮㸧ࠊ㸦㸯㸳㸯㸧ࠊ㸦㸲㸮㸮㸧࠿ࡽࡢᅇᢡࡔ࡜ᛮࢃࢀࡿࡀࠊఱࡽ࠿ࡢᙳ㡪࡟ࡼࡾ ୍㒊ࡢ⤖ᬗࡢᅇᢡゅࡀపゅᗘഃ࡬ࢩࣇࢺࡋࡓࡶࡢ࡜⪃࠼ࡽࢀࡿࠋᯞࢧࣥࢦࡢඛ➃㏆ഐ࡛⌧㇟ࡀほᐹࡉࢀ ࡓ࡜࠸࠺ࡇ࡜ࡣࠊ࢔ࣛࢦࢼ࢖ࢺ⤖ᬗࡀᙧᡂࡉࢀ࡚࠿ࡽᮇ㛫ࡀ⤒ࡗ࡚࠸࡞࠸࡜࠸࠺ࡇ࡜࡛࠶ࡾࠊࢧࣥࢦࡢ 㦵᱁ᙧᡂ࡟㛵㐃ࡋ࡚࠸ࡿྍ⬟ᛶࡀ㧗࠸ࠋࡉࡽ࡟ࠊ࢔ࣛࢦࢼ࢖ࢺ⤖ᬗࡢᅇᢡゅࡢపゅᗘഃ࡬ࡢኚ໬ࡣࠊ࣍ ࢱࢸ㈅Ẇࡢ⼖ࡘࡀ࠸௜㏆ࡢᅇᢡࣉࣟࣇ࢓࢖ࣝ࡟࠾࠸࡚ࡶ͆Unknown peak͇࡛♧ࡋࡓࡼ࠺࡟ほᐹࡉࢀ࡚࠸ ࡿࠋ࣍ࢱࢸ㈅ࡢ㈅Ẇᡂ㛗ࡀࠊ௒ᅇࡢ ᐃ఩⨨ A-1ࠊB-1ࠊC-1ࠊD-1 ௜㏆࠿ࡽⅣ㓟࢝ࣝࢩ࣒࢘ࡢ⤖ᬗࢆᙧ ᡂࡍࡿ࡜ࡍࢀࡤࠊᯞࢧࣥࢦ࡜ྠᵝ࡟ࠊᅇᢡゅࡢపゅᗘഃ࡬ࡢࢩࣇࢺࡣ㈅Ẇᙧᡂ࡜㛵㐃ࡀ࠶ࡿ࡜⪃࠼ࡽࢀ ࡿࠋ 㹖⥺ᅇᢡ ᐃ࡛ࡣࠊᅇᢡゅࡀୗグࡢࣈࣛࢵࢢࡢᅇᢡ᮲௳࡟ᚑ࠺ࡇ࡜ࡀ▱ࡽࢀ࡚࠸ࡿ㸯㸯㸧

O

T

n

sin

d

2

  or

T

O

sin

n

d

2

   (1) ࡇࡇ࡛ d㸸᱁Ꮚ㠃㛫㝸ࠊȟ㸸ࣈࣛࢵࢢゅ㸦㸻ධᑕゅ㸻཯ᑕゅ㸧ࠊȢ㸸X ⥺Ἴ㛗ࠊn㸸཯ᑕḟᩘ࡛࠶ࡿࠋ ゅᗘȟࡀపゅഃ࡟ࢩࣇࢺࡍࡿࡓࡵ࡟ࡣࠊ⤖ᬗ᱁Ꮚ㛫㝸 d ࡀ኱ࡁࡃ࡞ࡽ࡞ࡅࢀࡤ࡞ࡽ࡞࠸ࠋࡍ࡞ࢃࡕࠊⅣ 㓟࢝ࣝࢩ࣒࢘ CaCO3ࢆᵓᡂࡍࡿཎᏊࡢ࡝ࢀ࠿ࡀ௚ࡢཎᏊ࡟⨨᥮ࡉࢀࡓ࠿ࠊࡶࡋࡃࡣ௚ࡢཎᏊࡀཎᏊ㛫࡟ ධࡾ㎸ࢇ࡛⤖ᬗ᱁Ꮚ㛫㝸ࡀᗈࡀࡗࡓ࠿ࡢ࡝ࡕࡽ࠿࡛࠶ࡿࠋ௚ࡢᩥ⊩࡟ࡼࡿ࡜ࠊᾏỈ୰࡟ྵࡲࢀࡿ Ca ௨ እࡢཎᏊࡀࠊCa ཎᏊ࡜⨨᥮ࡍࡿࡇ࡜࡛Ⅳ㓟࢝ࣝࢩ࣒࢘ࡢᙧᡂ࡟ᙳ㡪ࡍࡿ࡜ሗ࿌ࡉࢀ࡚࠸ࡿ㸯㸰㸧ࠋ౛࠼ࡤࠊ Mg ཎᏊ࡟㛵ࡋ࡚ࡣࠊCa ࡜ Mg ࡢ mol ẚࡀࢧࣥࢦ㦵᱁ࡢᙧᡂ࡟ᙳ㡪ࢆ࠾ࡼࡰࡋࠊMg ࡢ๭ྜࡀᑡ࡞ࡃ࡞ ࡿ࡜࢔ࣛࢦࢼ࢖ࢺ࡛ࡣ࡞ࡃ࢝ࣝࢧ࢖ࢺࢆඃඛⓗ࡟ᙧᡂࡍࡿࡼ࠺࡟࡞ࡿ㸯㸱㸧ࠋ࢝ࣝࢧ࢖ࢺࡢᙧᡂ࡟㛵ࡋ࡚ ࡣࠊ࢝ࣝࢧ࢖ࢺࡢ୺ᅇᢡ㠃࡛࠶ࡿ㸦㸯㸮㸲㸧㸸29.42 deg ࡟ὀ┠ࡍࢀࡤࡼ࠸ࠋᅗ 7 ࡟♧ࡋࡓࢧࣥࢦ㦵᱁ࡢ ᅇᢡࣉࣟࣇ࢓࢖࡛ࣝࡑࡢᅇᢡࣆ࣮ࢡࢆ☜ㄆࡍࡿ࡜ࠊ ᐃ఩⨨࡟ࡼࡽࡎ㠀ᖖ࡟ࢃࡎ࠿࡛ࡣ࠶ࡿࡀ 30 deg ௜ ㏆࡟ᅇᢡࣆ࣮ࢡࡀㄆࡵࡽࢀࡿࠋ☜࠿࡟ Mg ࡟ࡼࡿᙳ㡪ࡀ࠶ࡿ࡜ᛮࢃࢀࡿࡀࠊࡑࡢ㔞ࡣࡈࡃࢃࡎ࠿࡜⪃࠼ ࡽࢀࡿࠋࡲࡓࠊMg ࡢཎᏊ␒ྕࡣ 12 ࡛࠶ࡾࠊ࢝ࣝࢩ࣒࢘ Ca ࡢ 20 ࡼࡾᑠࡉ࠸ࡓࡵཎᏊ༙ᚄࡀᑠࡉ࠸ࠋࡍ ࡞ࢃࡕࠊCa ࡢ Mg ࡬ࡢ⨨᥮ࡣࣆ࣮ࢡࢆ㧗ゅᗘഃ࡬ࢩࣇࢺࡉࡏࡿࡇ࡜࡜࡞ࡾࠊపゅᗘഃ࡬ࢩࣇࢺࡉࡏࡿࡇ ࡜ࡣ࡞࠸ࠋ ᾏỈ୰࡟ྵࡲࢀࡿཎᏊࡢ୰࡛ࡶࠊ⏕≀ࡀⅣ㓟࢝ࣝࢩ࣒࢘ࢆ⏕ᡂࡍࡿ㝿࡟኱ࡁࡃ㛵୚ࡋ࡚࠸ࡿ࡜ࡋ࡚ὀ ┠ࡉࢀ࡚࠸ࡿࡢࡀࢫࢺࣟࣥࢳ࣒࢘ Sr ࡛࠶ࡿ㸯㸲㸧㹼㸯㸴㸧ࠋSr ࡣ Ca ࡼࡾཎᏊ༙ᚄࡀ኱ࡁ࠸࡟ࡶ࠿࠿ࢃࡽࡎࠊ Ca ࡜ᐜ᫆࡟⨨᥮ࡍࡿࡇ࡜ࡀ࡛ࡁࠊࡲࡓ⨨᥮㔞ࡀỈ ࡟ᙳ㡪ࡍࡿࡇ࡜ࡀ▱ࡽࢀ࡚࠸ࡿ㸯㸳㸧ࠋࡑࡢࡓࡵࠊࢧ ࣥࢦ㦵᱁ෆ࡟ྵࡲࢀࡿ Sr ࡢྠ఩యࢆㄪᰝࡍࡿࡇ࡜࡛ࠊࢧࣥࢦ㦵᱁ᙧᡂ᫬ࡢỈ ࡸ஧㓟໬Ⅳ⣲㔞ࢆ᥎ᐃࡍ

(11)

ࡿࡇ࡜ࡀྍ⬟࡛࠶ࡾࠊ㐣ཤࡢᆅ⌫⎔ቃࢆ᥎ ࡍࡿࡓࡵࡢᣦᶆ࡜࡞ࡗ࡚࠸ࡿࠋAMCSD ࡟࠾ࡅࡿ Sr ࢆྵ ࡴ࢔ࣛࢦࢼ࢖ࢺࡢᅇᢡࣆ࣮ࢡࢆㄪᰝࡍࡿ࡜㸯㸵㸧㸦㸰㸰㸮㸧ᅇᢡ㠃࡟ᑐࡋ࡚ 42.97 deg ࡛࠶ࡾࠊ⣧⢋࡞࢔

ࣛࢦࢼ࢖ࢺࡢ 42.94 deg ࡟ẚ࡭࡚࡯࡜ࢇ࡝ᕪࡀ࡞࠸ࠋ୍᪉࡛ࠊAMCSD ࡟ྵࡲࢀࡿ Strontianite (SrCO3)ࡢ 㸦㸰㸰㸮㸧ᅇᢡ㠃࡟ᑐࡍࡿᅇᢡࣆ࣮ࢡࡣ 41.55 deg ࡛࠶ࡾ㸯㸶㸧ࠊ࢔ࣛࢦࢼ࢖ࢺ࡟ẚ࡭࡚ࢃࡎ࠿࡟పゅᗘഃ ࡟ࢩࣇࢺࡋ࡚࠸ࡿࠋ ࡇࡢࢫࢺࣟࣥࢳ࣒࢘ࡢᙳ㡪࡟ࡼࡿᅇᢡࣆ࣮ࢡࡢኚ໬ࢆ㚷ࡳࢀࡤࠊᮏ◊✲⤖ᯝࡣ௨ୗࡢࡼ࠺࡟⪃࠼ࡽࢀ ࡿࠋ࣍ࢱࢸ㈅Ẇࡢ⼖ࡘࡀ࠸௜㏆࠾ࡼࡧᯞࢧࣥࢦࡢඛ➃㏆ഐ㸦Position 5㸧࡛ࡢ XRD  ᐃ⤖ᯝ࡟࠾࠸࡚ࠊ ࠸ࡎࢀࡶ 42 deg ௜㏆࡟࠶ࡿᅇᢡࣆ࣮ࢡࡀపゅᗘഃ࡬⛣ືࡋࡓ⌮⏤ࠊࡑࡋ࡚ 77 deg ௜㏆࡛ࡣపゅᗘഃ࡬ࡢ ⛣ືࠊࡶࡋࡃࡣ᪂ࡓ࡞ࣆ࣮ࢡࡀ⏕ࡌࡓ⌮⏤࡜ࡋ࡚ࠊᾏỈ୰࡛⏕≀ࡀⅣ㓟࢝ࣝࢩ࣒࢘ࢆᙧᡂࡍࡿ㝿࡟ Sr ࢆྲྀࡾ㎸ࢇ࡛ Strontianite (SrCO3)ࢆᙧᡂࡋࡓࡓࡵ࡜⪃࠼ࡽࢀࡿࠋ≉࡟ᯞࢧࣥࢦࡀ⏕ᡂࡍࡿ࢔ࣛࢦࢼ࢖ࢺ ࡣ⧄⥔≧㸦ࡶࡋࡃࡣ㔪≧㸧࡛࠶ࡿࡇ࡜ࡀ▱ࡽࢀ࡚࠾ࡾ㸯㸴㸧ࠊ≉ᐃࡢᅇᢡࣆ࣮ࢡࡀ㧗ࡃ࡞ࡗࡓ⌮⏤ࡣ⏕ᡂ ึᮇ࡟≉ᐃࡢ᪉ྥ࡬㓄ྥࡋࡓࡓࡵ࡜⪃࠼ࡽࢀࡿࠋࡋ࠿ࡋࡇࡢᅇᢡࣆ࣮ࢡࡣᯞࢧࣥࢦࡢඛ➃࠿ࡽ㐲ࡊ࠿ࡿ ࡟ᚑࡗ࡚ᑠࡉࡃ࡞ࡗ࡚࠸ࡿࡇ࡜࠿ࡽࠊᡂ㛗ࡍࡿ࡟ᚑࡗ࡚ࡇࡢึᮇࡢ⧄⥔≧⤖ᬗ㛫ࡢ✵㝽ࢆᇙࡵࡿࡼ࠺࡟ ࢔ࣛࢦࢼ࢖ࢺ⤖ᬗࢆ⏕ᡂࡍࡿ࡜࡜ࡶ࡟ࠊ⤖ᬗࡢᅇ㌿ࡀ⏕ࡌࡿࡶࡢ࡜⪃࠼ࡽࢀࡿࠋᯞࢧࣥࢦࡢඛ➃௜㏆࡛ ࠶ࡗ࡚ࡶࠊPosition 4 ࡛ࡣ≉ᐃࡢᅇᢡ㠃࠿ࡽࡢࣆ࣮ࢡᙉᗘࡀቑຍࡋࡓࡶࡢࡢࠊపゅᗘഃ࡬ࡢࣆ࣮ࢡࡢࢩࣇ ࢺࢆ⏕ࡌ࡞࠿ࡗࡓࠋࡇࡢᯞඛ➃࡛ࡣ Strontianite (SrCO3)࡛ࡣ࡞ࡃࠊCa ࡜ Sr ࡢΰᅾࡋࡓ Aragonite ࢆᙧᡂ ࡋࡓ࡜⪃࠼ࡽࢀࡿࠋ௒ᚋࠊࢧࣥࢦ㦵᱁ࡢࢧࣥࣉࣝᩘࢆቑࡸࡍ࡜࡜ࡶ࡟ࠊ࢚ࢿࣝࢠ࣮ศᩓᆺ X ⥺ศᯒ㸦Energy dispersive X-ray spectrometry㸸EDX㸧࡞࡝ࢆ⏝࠸࡚᭦࡞ࡿ᳨ウࢆヨࡳࡿࠋ

 ⤖  ゝ ᯞࢧࣥࢦ㦵᱁ࡢ⤖ᬗᵓ㐀ㄪᰝࡢ୍⎔࡜ࡋ࡚ࠊⅣ㓟࢝ࣝࢩ࣒࢘ࢆ୺ᡂศ࡜ࡍࡿ㦵᱁ࢆᙧᡂࡍࡿࢺࢤࢫࢠ ࣑ࢻࣜ࢖ࢩ㸦Acropora intermedia㸧ࢆᑐ㇟࡜ࡋ࡚ࠊࡑࡢ㦵᱁ࡢ X ⥺ᅇᢡ ᐃࢆ⾜ࡗࡓࠋࡲࡓẚ㍑ࡢࡓࡵࠊ Ⅳ㓟࢝ࣝࢩ࣒࢘ࢆ୺ᡂศ࡜ࡍࡿ࣍ࢱࢸ㈅㸦Mizuhopecten yessoensis㸧ࡢ㈅Ẇ࡟ᑐࡋ࡚ࡶྠᵝࡢ X ⥺ᅇᢡ  ᐃࢆ⾜ࡗࡓࠋࡑࡢ⤖ᯝࠊ௨ୗࡢࡇ࡜ࡀ᫂ࡽ࠿࡜࡞ࡗࡓࠋ 1㸬ࢺࢤࢫࢠ࣑ࢻࣜ࢖ࢩࡢ㦵᱁ࡣࠊ‽Ᏻᐃࡢ࢔ࣛࢦࢼ࢖ࢺᵓ㐀࡜ࡼࡤࢀࡿⅣ㓟࢝ࣝࢩ࣒࡛࢘࠶ࡾࠊᏳ ᐃࡢ࢝ࣝࢧ࢖ࢺᵓ㐀࡛ࡣ࡞࠸ࠋඛ➃㒊ศ࡟㏆࠸࡯࡝≉ᐃࡢ⤖ᬗ᪉఩࡟㓄ྥࡍࡿഴྥࡀ࠶ࡿࠋ 2㸬࣍ࢱࢸ㈅ࡢ㈅Ẇࡣ୺࡜ࡋ࡚࢝ࣝࢧ࢖ࢺᵓ㐀ࡢ⤖ᬗ࡛࠶ࡿࡀࠊ࢔ࣛࢦࢼ࢖ࢺᵓ㐀ࡢ⤖ᬗ࡜ࡢΰྜ࡛ ࠶ࡿࠋ㈅ᰕࡢ௜╔ࡍࡿ㡿ᇦࡣࠊ୺࡜ࡋ࡚࢔ࣛࢦࢼ࢖ࢺᵓ㐀࡛࠶ࡾࠊ௚ࡢ㡿ᇦ࡜ࡣ᫂ࡽ࠿࡟␗࡞ࡿࠋ 3㸬ࢧࣥࢦ㦵᱁ࡢඛ➃㏆ഐࠊ࣍ࢱࢸ㈅Ẇࡢ⼖ࡘࡀ࠸㏆ഐ࡛ࡣࠊ≉ᐃࡢ࢔ࣛࢦࢼ࢖ࢺ⤖ᬗ᪉఩࠿ࡽࡢᅇ ᢡࣆ࣮ࢡࡀࠊపゅᗘഃ࡬ࢃࡎ࠿࡟ࢩࣇࢺࡍࡿࠋࡇࡢ⌮⏤ࡣࠊᩥ⊩࡞࡝࠿ࡽࢫࢺࣟࣥࢳ࣒࢘ࡢᙳ㡪 ࡜᥎ ࡉࢀࡿࠋ ᘬ⏝ᩥ⊩ 㸯㸧㕥ᮌ῟ࠊ஭ୖ㯞ኤ㔛ࠊ㐀♋ࢧࣥࢦ㢮ࡢ▼⅊໬ᶵᵓ࡜ᆅ⌫⎔ቃኚື࡟ᑐࡍࡿᛂ⟅ࠊᾏࡢ◊✲ࠊ21㸦5㸧ࠊ 177㸫188ࠊ㸦2012㸧

(12)

㸰㸧బ⸨ᩄᙪࠊࢧࣥࢦ(Scleractinia)ࡢ㦵᱁ࡢᚤ⣽ᵓ㐀 : ࡑࡢ 1. 㟁Ꮚ㢧ᚤ㙾࡟ࡼࡿほᐹࠊᆅ⌫⛉Ꮫࠊ66ࠊ 8C㸫14ࠊ㸦1963㸧 㸱㸧㐲⸨୍ెࠊ࢝ࣝࢧ࢖ࢺ㸫࢔ࣛࢦࢼ࢖ࢺၥ㢟ࠖ࡟ᣮࡴ㹼ศᏊ⏕≀Ꮫ࡛㏕ࡿ⏕య㖔≀Ꮫ᭱኱ࡢ㞴ၥ㹼ࠊ JGLࠊ4㸦4㸧ࠊ6㸫7ࠊ㸦2008㸧 㸲㸧ୖ㔛ඃ㈗ࠊᨻᮌΎᏕࠊ☾ᮧᑦᏊࠊᒣᮏᗈ⨾ࠊᯞࢧࣥࢦ㦵᱁ࡢ᭤ࡆ≉ᛶ࡜ෆ㒊ᵓ㐀ࡢ┦㛵ᛶࡢㄪᰝࠊ ᪥ᮏᶵᲔᏛ఍ ᮦᩱຊᏛ㒊㛛࢝ࣥࣇ࢓ࣞࣥࢫ㸦M&M'14㸧ㅮ₇ㄽᩥ㞟㸪CD-ROMࠊNo.GS23, 1㸫4㸦2014㸧. 㸳㸧ୖ㔛ඃ㈗ࠊᨻᮌΎᏕࠊ☾ᮧᑦᏊࠊᒣᮏᗈ⨾ࠊᯞࢧࣥࢦࡢᅄⅬ᭤ࡆᙉᗘ≉ᛶࠊ᪥ᮏᮦᩱᏛ఍ ಙ㢗ᛶ࣭ ◚ቯྜྠࢩ࣏ࣥࢪ࣒࢘ㅮ₇ㄽᩥ㞟ࠊ114㸫117ࠊ㸦2013㸧 㸴㸧஭ୖ㯞ኤ㔛ࠊ⎔ቃᣦᶆ࡜ࡋ࡚ࡢࢧࣥࢦ㦵᱁୰ࡢᚤ㔞ඖ⣲࡜ࡑࡢኚື࣓࢝ࢽࢬ࣒ࡢゎ᫂࡟ྥࡅ࡚ࠊᾏ ࡢ◊✲ࠊ21㸦5㸧ࠊ159㸫175ࠊ㸦2012㸧 㸵㸧http://mukiken.eng.niigata-u.ac.jp/chemsoft/x-raysoft/PatViewHelp.html 㸶㸧http://rruff.geo.arizona.edu/AMS/amcsd.php

㸷㸧http://rruff.geo.arizona.edu/AMS/amcsd.php (Dal Negro A, Ungaretti L, American Mineralogist 56,768-772 (1971))

㸯㸮㸧http://rruff.geo.arizona.edu/AMS/amcsd.php (Graf D L, American Mineralogist 46, 1283-1316 (1961)) 㸯㸯㸧W.D.࢟ࣕࣜࢫࢱ࣮ࠊᮦᩱࡢ⛉Ꮫ࡜ᕤᏛ [1] ᮦᩱࡢᚤ⣽ᵓ㐀ࠊᇵ㢼㤋ࠊ62㸫67ࠊ㸦2002㸧

㸯㸰㸧໭ᮧගᏕࠊⅣ㓟࢝ࣝࢩ࣒࢘⤖ᬗከᙧࡢᯒฟᣲື࡟ཬࡰࡍῧຍ≀ຠᯝࠊ᪥ᮏᾏỈᏛ఍ㄅࠊ53㸦3㸧ࠊ 162㸫165ࠊ(1999)

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X-Ray diffraction measurement of marine-derived calcium carbonate



Kiyotaka Masaki㸯, Naoko Isomura㸰, Hiromi Yamamoto㸱 

Department of Mechanical Systems Engineering, Department of Bioresources Engineering㸪 Okinawa Churashima Foundation㸪



X-ray diffraction measurements (XRD) were obtained for the skeleton of an Acropora intermedia specimen and the shell of a Mizuhopecten yessoensis specimen in order to investigate the crystal structure of marine-derived calcium carbonate. The results implied the following conclusions. (1)The skeleton of Acropora intermedia is composed of aragonite, which is a metastable crystal. It is also oriented along a specific direction located at or near the tip. (2) The shell of Mizuhopecten yessoensis is composed of both calcite, which is stable crystal, and aragonite crystal. The region containing the scallop adductor is primarily composed of a structure formed of aragonite crystal. (3) The diffraction angles of certain aragonite crystal planes were shifted toward lower angles near the tip of the skeleton or the hinge of the shell. This result suggests the influence of strontium present in the specimens.

Key word: Calcium carbonate, X-Ray diffraction method, Aragonite, Calcite, Acropora intermedia,

Mizuhopecten yessoensis

 

参照

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