64
Boden TA, Marland G, Andres RJ (2011) Global, regional, and national fossil-fuel CO 2 emissions,
Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, U.S. Department
of Energy, Oak Ridge. doi:https://doi.org/10.3334/CDIAC/00001_V2011
Boschker HTS, Wielemaker A, Schaub BEM, Holmer M (2000) Limited coupling of macrophyte
production and bacterial carbon cycling in the sediment of Zostera spp. meadows. Mar Ecol
Prog Ser 203:181–189. https://doi.org/10.3354/meps203181
Bouillon S, Boschker HTS (2006) Bacterial carbon sources in coastal sediments: a cross-system
analysis based on stable isotope data of biomarkers. Biogeosciences 3:175–185. https://doi.
org/10.5194/bg-3-175-2006
Bouillon S, Borges AV, Castañeda-Moya E, Diele K, Dittmar T, Duke NC, Kristensen E, Lee
SY, Marchand C, Middelburg JJ, Rivera-Monroy VH, Smith TJ, Twilley RR (2008) Mangrove
production and carbon sinks: a revision of global budget estimates. Glob Biogeochem Cycles
22:GB2013. https://doi.org/10.1029/2007GB003052
Cabaço S, Santos R, Duarte CM (2008) The impact of sediment burial and erosion on seagrasses: a
review. Estuar Coast Shelf Sci 79:354–366. https://doi.org/10.1016/j.ecss.2008.04.021
Cai P, Huang Q-Y, Zhang X-W (2006) Interactions of DNA with clay minerals and soil colloidal
particles and protection against degradation by DNase. Environ Sci Technol 40:2971–2976.
https://doi.org/10.1021/es0522985
Chen G, Azkab MH, Chmura GL, Chen S, Sastrosuwondo P, Ma Z, Dharmawan IWE, Yin X, Chen
B (2017) Mangroves as a major source of soil carbon storage in adjacent seagrass meadows.
Sci Rep 7:42406. https://doi.org/10.1038/srep42406
Chenu C (1993) Clay- or sand-polysaccharide associations as models for the interface between
micro-organisms and soil: water related properties and microstructure. Geoderma 56:143–156.
https://doi.org/10.1016/0016-7061(93)90106-U
Ciais P, Sabine CL, Bala G, Bopp L, Brovkin V, Canadell J, Chhabra A, DeFries R, Galloway J,
Heimann M, Jones C, Le Quéré C, Myneni RB, Piao S, Thornton P (2013) 6. Carbon and other
biogeochemical cycles. In: Stocker TF, Qin D, Plattner G-K, Tignor M, Allen SK, Boschung
J, Nauels A, Xia Y, Bex V, Midgley PM (eds) Climate change 2013: the physical science basis.
Contribution of Working Group I to the fifth assessment report of the intergovernmental panel
on climate change. Cambridge University Press, Cambridge
Cyle KT, Hill N, Young K, Jenkins T, Hancock D, Schroeder PA, Thompson A (2016) Substrate
quality influences organic matter accumulation in the soil silt and clay fraction. Soil Biol
Biochem 103:138–148. https://doi.org/10.1016/j.soilbio.2016.08.014
Dauby P, Bale AJ, Bloomer N, Canon C, Ling RD, Norro A, Robertson JE, Simon A, Theate J-M,
Watson AJ, Frankignoulle M (1995) Particle fluxes over a Mediterranean seagrass bed: a one
year case study. Mar Ecol Prog Ser 126:233–246. https://doi.org/10.3354/meps126223
De Leeuw JW, Rijpstra WIC, Nienhuis PH (1995) Free and bound fatty acids and hydroxy fatty
acids in the living and decomposing eelgrass Zostera marina L. Org Geochem 23:721–728.
https://doi.org/10.1016/0146-6380(95)00062-J
Decho AW (2000) Microbial biofilms in intertidal systems: an overview. Cont Shelf Res 20:1257–
1273. https://doi.org/10.1016/S0278-4343(00)00022-4
Del Giorgio PA, Cole JJ (1998) Bacterial growth efficiency in natural aquatic systems. Annu Rev
Ecol Syst 29:503–541. https://doi.org/10.1146/annurev.ecolsys.29.1.503
Donato DC, Kauffman JB, Murdiyarso D, Kurnianto S, Stidham M, Kanninen M (2011)
Mangroves among the most carbon-rich forests in the tropics. Nat Geosci 4:293–297. https://
doi.org/10.1038/NGEO1123
Duarte CM (1991) Seagrass depth limits. Aquat Bot 40:363–377. https://doi.
org/10.1016/0304-3770(91)90081-F
Duarte CM, Cebrián J (1996) The fate of marine autotrophic production. Limnol Oceanogr
41:1758–1766. https://doi.org/10.4319/lo.1996.41.8.1758
Duarte CM, Middelburg JJ, Caraco N (2005) Major role of marine vegetation on the oceanic carbon cycle. Biogeosciences 2:1–8. https://doi.org/10.5194/bg-2-1-2005
T. Miyajima and M. Hamaguchi
Boden TA, Marland G, Andres RJ (2011) Global, regional, and national fossil-fuel CO 2 emissions,
Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, U.S. Department
of Energy, Oak Ridge. doi:https://doi.org/10.3334/CDIAC/00001_V2011
Boschker HTS, Wielemaker A, Schaub BEM, Holmer M (2000) Limited coupling of macrophyte
production and bacterial carbon cycling in the sediment of Zostera spp. meadows. Mar Ecol
Prog Ser 203:181–189. https://doi.org/10.3354/meps203181
Bouillon S, Boschker HTS (2006) Bacterial carbon sources in coastal sediments: a cross-system
analysis based on stable isotope data of biomarkers. Biogeosciences 3:175–185. https://doi.
org/10.5194/bg-3-175-2006
Bouillon S, Borges AV, Castañeda-Moya E, Diele K, Dittmar T, Duke NC, Kristensen E, Lee
SY, Marchand C, Middelburg JJ, Rivera-Monroy VH, Smith TJ, Twilley RR (2008) Mangrove
production and carbon sinks: a revision of global budget estimates. Glob Biogeochem Cycles
22:GB2013. https://doi.org/10.1029/2007GB003052
Cabaço S, Santos R, Duarte CM (2008) The impact of sediment burial and erosion on seagrasses: a
review. Estuar Coast Shelf Sci 79:354–366. https://doi.org/10.1016/j.ecss.2008.04.021
Cai P, Huang Q-Y, Zhang X-W (2006) Interactions of DNA with clay minerals and soil colloidal
particles and protection against degradation by DNase. Environ Sci Technol 40:2971–2976.
https://doi.org/10.1021/es0522985
Chen G, Azkab MH, Chmura GL, Chen S, Sastrosuwondo P, Ma Z, Dharmawan IWE, Yin X, Chen
B (2017) Mangroves as a major source of soil carbon storage in adjacent seagrass meadows.
Sci Rep 7:42406. https://doi.org/10.1038/srep42406
Chenu C (1993) Clay- or sand-polysaccharide associations as models for the interface between
micro-organisms and soil: water related properties and microstructure. Geoderma 56:143–156.
https://doi.org/10.1016/0016-7061(93)90106-U
Ciais P, Sabine CL, Bala G, Bopp L, Brovkin V, Canadell J, Chhabra A, DeFries R, Galloway J,
Heimann M, Jones C, Le Quéré C, Myneni RB, Piao S, Thornton P (2013) 6. Carbon and other
biogeochemical cycles. In: Stocker TF, Qin D, Plattner G-K, Tignor M, Allen SK, Boschung
J, Nauels A, Xia Y, Bex V, Midgley PM (eds) Climate change 2013: the physical science basis.
Contribution of Working Group I to the fifth assessment report of the intergovernmental panel
on climate change. Cambridge University Press, Cambridge
Cyle KT, Hill N, Young K, Jenkins T, Hancock D, Schroeder PA, Thompson A (2016) Substrate
quality influences organic matter accumulation in the soil silt and clay fraction. Soil Biol
Biochem 103:138–148. https://doi.org/10.1016/j.soilbio.2016.08.014
Dauby P, Bale AJ, Bloomer N, Canon C, Ling RD, Norro A, Robertson JE, Simon A, Theate J-M,
Watson AJ, Frankignoulle M (1995) Particle fluxes over a Mediterranean seagrass bed: a one
year case study. Mar Ecol Prog Ser 126:233–246. https://doi.org/10.3354/meps126223
De Leeuw JW, Rijpstra WIC, Nienhuis PH (1995) Free and bound fatty acids and hydroxy fatty
acids in the living and decomposing eelgrass Zostera marina L. Org Geochem 23:721–728.
https://doi.org/10.1016/0146-6380(95)00062-J
Decho AW (2000) Microbial biofilms in intertidal systems: an overview. Cont Shelf Res 20:1257–
1273. https://doi.org/10.1016/S0278-4343(00)00022-4
Del Giorgio PA, Cole JJ (1998) Bacterial growth efficiency in natural aquatic systems. Annu Rev
Ecol Syst 29:503–541. https://doi.org/10.1146/annurev.ecolsys.29.1.503
Donato DC, Kauffman JB, Murdiyarso D, Kurnianto S, Stidham M, Kanninen M (2011)
Mangroves among the most carbon-rich forests in the tropics. Nat Geosci 4:293–297. https://
doi.org/10.1038/NGEO1123
Duarte CM (1991) Seagrass depth limits. Aquat Bot 40:363–377. https://doi.
org/10.1016/0304-3770(91)90081-F
Duarte CM, Cebrián J (1996) The fate of marine autotrophic production. Limnol Oceanogr
41:1758–1766. https://doi.org/10.4319/lo.1996.41.8.1758
Duarte CM, Middelburg JJ, Caraco N (2005) Major role of marine vegetation on the oceanic carbon cycle. Biogeosciences 2:1–8. https://doi.org/10.5194/bg-2-1-2005
T. Miyajima and M. Hamaguchi