Whole Transcriptome Analysis of the Coral <i>Acropora millepora</i> Reveals Complex Responses to CO<sub>2</sub>‐driven Acidification during the Initiation of Calcification

Molecular Ecology - Tập 21 Số 10 - Trang 2440-2454 - 2012
Aurélie Moya1,2,3,4, L. Huisman1,5,3, Eldon E. Ball6, David C. Hayward6, Lauretta C. Grasso1,6, Chia Miin Chua1, Hin-Koon Woo7, Jean‐Pierre Gattuso2,4, Sylvian Foret1, David J. Miller1,8
1ARC Centre of Excellence for Coral Reef Studies, James Cook University, Townsville, Queensland 4811, Australia
2INSU-CNRS, Laboratoire d’Océanographie de Villefranche, B.P. 28, 06234, Villefranche-sur-mer, Cedex, France
3these authors contributed equally to this work
4UPMC University of Paris 06, Observatoire Océanologique de Villefranche, 06230 Villefranche-sur-mer, France
5Section of Computational Science, Universiteit van Amsterdam, Science Park 904, 1098 XH, Amsterdam, The Netherlands
6Evolution, Ecology and Genetics, Research School of Biology, Bldg. 46 Australian National University, Canberra, A.C.T. 0200, Australia
7Macrogen Inc., 10F World Meridian Center, 60-24 Gasan-dong, Gumchun-gu, Seoul 153-781, South Korea
8School of Pharmacy and Molecular Sciences, James Cook University, Townsville, Queensland 4811, Australia

Tóm tắt

AbstractThe impact of ocean acidification (OA) on coral calcification, a subject of intense current interest, is poorly understood in part because of the presence of symbionts in adult corals. Early life history stages of Acropora spp. provide an opportunity to study the effects of elevated CO2 on coral calcification without the complication of symbiont metabolism. Therefore, we used the Illumina RNAseq approach to study the effects of acute exposure to elevated CO2 on gene expression in primary polyps of Acropora millepora, using as reference a novel comprehensive transcriptome assembly developed for this study. Gene ontology analysis of this whole transcriptome data set indicated that CO2‐driven acidification strongly suppressed metabolism but enhanced extracellular organic matrix synthesis, whereas targeted analyses revealed complex effects on genes implicated in calcification. Unexpectedly, expression of most ion transport proteins was unaffected, while many membrane‐associated or secreted carbonic anhydrases were expressed at lower levels. The most dramatic effect of CO2‐driven acidification, however, was on genes encoding candidate and known components of the skeletal organic matrix that controls CaCO3 deposition. The skeletal organic matrix effects included elevated expression of adult‐type galaxins and some secreted acidic proteins, but down‐regulation of other galaxins, secreted acidic proteins, SCRiPs and other coral‐specific genes, suggesting specialized roles for the members of these protein families and complex impacts of OA on mineral deposition. This study is the first exhaustive exploration of the transcriptomic response of a scleractinian coral to acidification and provides an unbiased perspective on its effects during the early stages of calcification.

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Tài liệu tham khảo

10.1007/s00338-008-0392-5

10.1073/pnas.1007273107

10.1007/978-94-007-0114-4_9

10.1016/j.jembe.2010.11.009

10.1038/75556

10.1016/S0022-0981(96)02622-6

10.1152/ajpcell.00403.2005

10.3354/meps296291

10.1093/icb/37.6.633

10.1038/425365a

10.1016/0003-2697(87)90021-2

10.1029/2009GC002411

10.1054/ceca.1998.0018

10.1007/s005310050286

10.1126/science.1165283

10.1111/j.1365-294X.2008.03879.x

10.3354/meps08346

10.1016/j.tig.2010.01.003

10.1016/S0006-291X(03)00527-8

10.1242/jeb.203.22.3445

10.1371/journal.pgen.1002187

10.1007/s00227-009-1171-8

10.1242/jeb.200.5.883

10.2307/1539156

10.1186/1471-2164-9-540

10.1016/j.ydbio.2011.02.010

10.1093/sysbio/syq010

10.1111/j.1469-185X.1999.tb00180.x

10.1007/s00424-011-0922-9

10.1007/978-94-007-0114-4_6

Harrison PL, 1990, Ecosystems of the World Coral Reefs., 133

10.1371/journal.pone.0026411

10.1073/pnas.0710604105

10.1111/j.1749-6632.1984.tb12385.x

10.1016/j.gca.2009.04.015

10.5194/bgd-8-8485-2011

IPCC, 2007, Climate Change 2007: The physical science basis: contribution of working group I to the fourth assessment report of the Intergovernmental Panel on Climate Change

10.1126/science.1141560

10.1021/bm9012106

10.5670/oceanog.2009.101

10.3354/meps07802

10.1074/jbc.271.13.7313

10.1029/2004JC002576

10.1186/gb-2009-10-3-r25

Lewis E, 1998, ORNL/CDIAC‐105

10.1016/S0070-2153(07)80006-8

10.1016/S1095-6433(03)00201-0

10.1007/s00338-004-0369-y

10.1111/j.1365-294X.2011.05205.x

Mitterer RM, 1978, Amino acid composition and metal binding capability of the skeleton protein of corals, Bulletin of Marine Science, 28, 173

10.2108/zsj.22.311

10.1074/jbc.M804726200

10.1073/pnas.0809996106

10.1371/journal.pone.0014521

Ohde S, 1999, Carbon dioxide flux and metabolic processes of a coral reef, Okinawa, Bulletin of Marine Science, 65, 559

Orr JC, 2011, Ocean Acidification

10.1038/nature04095

10.1126/science.1204794

10.1080/14756360410001689540

10.1093/nar/30.9.e36

10.1007/s00338-010-0697-z

10.1186/1471-2148-9-178

10.1093/bioinformatics/btp616

Rozen S, 2000, Primer3 on the WWW for general users and for biologist programmers, Methods in Molecular Biology, 132, 365

Sambrook J, 2001, Molecular Cloning: A Laboratory Manual

10.1186/1471-2164-8-337

10.2517/prpsj.10.311

10.1242/jeb.00141

10.1002/dvdy.20517

10.1038/nature10249

10.1371/journal.pone.0004865

10.2174/138161208783877884

10.1007/s12562-009-0189-7

Tambutté S, 1996, Inorganic carbon supply to symbiont photosynthesis of the sea anemone, Anemonia viridis: role of the oral epithelial layers, Symbiosis, 20, 199

10.1242/jeb.032540

10.1016/j.cbpb.2006.06.011

10.1186/gb-2002-3-7-research0034

Wilkinson C, 2008, Status of Coral Reefs of the World: 2008

10.1186/gb-2010-11-2-r14

10.3354/meps221125