Can variable pH and low oxygen moderate ocean acidification outcomes for mussel larvae?
Natural variation and changing climate in coastal oceans subject meroplanktonic organisms to broad ranges of pH and oxygen ([O₂]) levels. In controlled‐laboratory experiments we explored the interactive effects of pH, [O₂], and semidiurnal pH fluctuations on the survivorship, development, and size o...
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| Published in | Global change biology Vol. 20; no. 3; pp. 754 - 764 |
|---|---|
| Main Authors | , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Oxford
Blackwell Science
01.03.2014
Blackwell Publishing Ltd Wiley-Blackwell |
| Subjects | |
| Online Access | Get full text |
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| Abstract | Natural variation and changing climate in coastal oceans subject meroplanktonic organisms to broad ranges of pH and oxygen ([O₂]) levels. In controlled‐laboratory experiments we explored the interactive effects of pH, [O₂], and semidiurnal pH fluctuations on the survivorship, development, and size of early life stages of two mytilid mussels, Mytilus californianus and M. galloprovincialis. Survivorship of larvae was unaffected by low pH, low [O₂], or semidiurnal fluctuations for both mytilid species. Low pH (<7.6) resulted in delayed transition from the trochophore to veliger stage, but this effect of low pH was absent when incorporating semidiurnal fluctuations in both species. Also at low pH, larval shells were smaller and had greater variance; this effect was absent when semidiurnal fluctuations of 0.3 units were incorporated at low pH for M. galloprovincialis but not for M. californianus. Low [O₂] in combination with low pH had no effect on larval development and size, indicating that early life stages of mytilid mussels are largely tolerant to a broad range of [O₂] reflective of their environment (80–260 μmol kg⁻¹). The role of pH variability should be recognized as an important feature in coastal oceans that has the capacity to modulate the effects of ocean acidification on biological responses. |
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| AbstractList | Natural variation and changing climate in coastal oceans subject meroplanktonic organisms to broad ranges of
pH
and oxygen ([O
2
]) levels. In controlled‐laboratory experiments we explored the interactive effects of
pH
, [O
2
], and semidiurnal
pH
fluctuations on the survivorship, development, and size of early life stages of two mytilid mussels,
Mytilus californianus
and
M. galloprovincialis
. Survivorship of larvae was unaffected by low
pH
, low [O
2
], or semidiurnal fluctuations for both mytilid species. Low
pH
(<7.6) resulted in delayed transition from the trochophore to veliger stage, but this effect of low
pH
was absent when incorporating semidiurnal fluctuations in both species. Also at low
pH
, larval shells were smaller and had greater variance; this effect was absent when semidiurnal fluctuations of 0.3 units were incorporated at low
pH
for
M. galloprovincialis
but not for
M. californianus
. Low [O
2
] in combination with low
pH
had no effect on larval development and size, indicating that early life stages of mytilid mussels are largely tolerant to a broad range of [O
2
] reflective of their environment (80–260
μ
mol kg
−1
). The role of
pH
variability should be recognized as an important feature in coastal oceans that has the capacity to modulate the effects of ocean acidification on biological responses. Natural variation and changing climate in coastal oceans subject meroplanktonic organisms to broad ranges of pH and oxygen ([O₂]) levels. In controlled‐laboratory experiments we explored the interactive effects of pH, [O₂], and semidiurnal pH fluctuations on the survivorship, development, and size of early life stages of two mytilid mussels, Mytilus californianus and M. galloprovincialis. Survivorship of larvae was unaffected by low pH, low [O₂], or semidiurnal fluctuations for both mytilid species. Low pH (<7.6) resulted in delayed transition from the trochophore to veliger stage, but this effect of low pH was absent when incorporating semidiurnal fluctuations in both species. Also at low pH, larval shells were smaller and had greater variance; this effect was absent when semidiurnal fluctuations of 0.3 units were incorporated at low pH for M. galloprovincialis but not for M. californianus. Low [O₂] in combination with low pH had no effect on larval development and size, indicating that early life stages of mytilid mussels are largely tolerant to a broad range of [O₂] reflective of their environment (80–260 μmol kg⁻¹). The role of pH variability should be recognized as an important feature in coastal oceans that has the capacity to modulate the effects of ocean acidification on biological responses. Natural variation and changing climate in coastal oceans subject meroplanktonic organisms to broad ranges of pH and oxygen ([O2]) levels. In controlled-laboratory experiments we explored the interactive effects of pH, [O2], and semidiurnal pH fluctuations on the survivorship, development, and size of early life stages of two mytilid mussels, Mytilus californianus and M. galloprovincialis. Survivorship of larvae was unaffected by low pH, low [O2], or semidiurnal fluctuations for both mytilid species. Low pH (<7.6) resulted in delayed transition from the trochophore to veliger stage, but this effect of low pH was absent when incorporating semidiurnal fluctuations in both species. Also at low pH, larval shells were smaller and had greater variance; this effect was absent when semidiurnal fluctuations of 0.3 units were incorporated at low pH for M. galloprovincialis but not for M. californianus. Low [O2] in combination with low pH had no effect on larval development and size, indicating that early life stages of mytilid mussels are largely tolerant to a broad range of [O2] reflective of their environment (80-260 µmol kg-1). The role of pH variability should be recognized as an important feature in coastal oceans that has the capacity to modulate the effects of ocean acidification on biological responses. [PUBLICATION ABSTRACT] Natural variation and changing climate in coastal oceans subject meroplanktonic organisms to broad ranges of pH and oxygen ([O sub(2)]) levels. In controlled-laboratory experiments we explored the interactive effects of pH, [O sub(2)], and semidiurnal pH fluctuations on the survivorship, development, and size of early life stages of two mytilid mussels, Mytilus californianus and M. galloprovincialis. Survivorship of larvae was unaffected by low pH, low [O sub(2)], or semidiurnal fluctuations for both mytilid species. Low pH (<7.6) resulted in delayed transition from the trochophore to veliger stage, but this effect of low pH was absent when incorporating semidiurnal fluctuations in both species. Also at low pH, larval shells were smaller and had greater variance; this effect was absent when semidiurnal fluctuations of 0.3 units were incorporated at low pH for M. galloprovincialis but not for M. californianus. Low [O sub(2)] in combination with low pH had no effect on larval development and size, indicating that early life stages of mytilid mussels are largely tolerant to a broad range of [O sub(2)] reflective of their environment (80-260 mu mol kg super(-1)). The role of pH variability should be recognized as an important feature in coastal oceans that has the capacity to modulate the effects of ocean acidification on biological responses. Natural variation and changing climate in coastal oceans subject meroplanktonic organisms to broad ranges of pH and oxygen ([O2 ]) levels. In controlled-laboratory experiments we explored the interactive effects of pH, [O2 ], and semidiurnal pH fluctuations on the survivorship, development, and size of early life stages of two mytilid mussels, Mytilus californianus and M. galloprovincialis. Survivorship of larvae was unaffected by low pH, low [O2 ], or semidiurnal fluctuations for both mytilid species. Low pH (<7.6) resulted in delayed transition from the trochophore to veliger stage, but this effect of low pH was absent when incorporating semidiurnal fluctuations in both species. Also at low pH, larval shells were smaller and had greater variance; this effect was absent when semidiurnal fluctuations of 0.3 units were incorporated at low pH for M. galloprovincialis but not for M. californianus. Low [O2 ] in combination with low pH had no effect on larval development and size, indicating that early life stages of mytilid mussels are largely tolerant to a broad range of [O2 ] reflective of their environment (80-260 μmol kg(-1) ). The role of pH variability should be recognized as an important feature in coastal oceans that has the capacity to modulate the effects of ocean acidification on biological responses.Natural variation and changing climate in coastal oceans subject meroplanktonic organisms to broad ranges of pH and oxygen ([O2 ]) levels. In controlled-laboratory experiments we explored the interactive effects of pH, [O2 ], and semidiurnal pH fluctuations on the survivorship, development, and size of early life stages of two mytilid mussels, Mytilus californianus and M. galloprovincialis. Survivorship of larvae was unaffected by low pH, low [O2 ], or semidiurnal fluctuations for both mytilid species. Low pH (<7.6) resulted in delayed transition from the trochophore to veliger stage, but this effect of low pH was absent when incorporating semidiurnal fluctuations in both species. Also at low pH, larval shells were smaller and had greater variance; this effect was absent when semidiurnal fluctuations of 0.3 units were incorporated at low pH for M. galloprovincialis but not for M. californianus. Low [O2 ] in combination with low pH had no effect on larval development and size, indicating that early life stages of mytilid mussels are largely tolerant to a broad range of [O2 ] reflective of their environment (80-260 μmol kg(-1) ). The role of pH variability should be recognized as an important feature in coastal oceans that has the capacity to modulate the effects of ocean acidification on biological responses. Natural variation and changing climate in coastal oceans subject meroplanktonic organisms to broad ranges of pH and oxygen ([O2]) levels. In controlled‐laboratory experiments we explored the interactive effects of pH, [O2], and semidiurnal pH fluctuations on the survivorship, development, and size of early life stages of two mytilid mussels, Mytilus californianus and M. galloprovincialis. Survivorship of larvae was unaffected by low pH, low [O2], or semidiurnal fluctuations for both mytilid species. Low pH (<7.6) resulted in delayed transition from the trochophore to veliger stage, but this effect of low pH was absent when incorporating semidiurnal fluctuations in both species. Also at low pH, larval shells were smaller and had greater variance; this effect was absent when semidiurnal fluctuations of 0.3 units were incorporated at low pH for M. galloprovincialis but not for M. californianus. Low [O2] in combination with low pH had no effect on larval development and size, indicating that early life stages of mytilid mussels are largely tolerant to a broad range of [O2] reflective of their environment (80–260 μmol kg−1). The role of pH variability should be recognized as an important feature in coastal oceans that has the capacity to modulate the effects of ocean acidification on biological responses. Natural variation and changing climate in coastal oceans subject meroplanktonic organisms to broad ranges of pH and oxygen ([O2 ]) levels. In controlled-laboratory experiments we explored the interactive effects of pH, [O2 ], and semidiurnal pH fluctuations on the survivorship, development, and size of early life stages of two mytilid mussels, Mytilus californianus and M. galloprovincialis. Survivorship of larvae was unaffected by low pH, low [O2 ], or semidiurnal fluctuations for both mytilid species. Low pH (<7.6) resulted in delayed transition from the trochophore to veliger stage, but this effect of low pH was absent when incorporating semidiurnal fluctuations in both species. Also at low pH, larval shells were smaller and had greater variance; this effect was absent when semidiurnal fluctuations of 0.3 units were incorporated at low pH for M. galloprovincialis but not for M. californianus. Low [O2 ] in combination with low pH had no effect on larval development and size, indicating that early life stages of mytilid mussels are largely tolerant to a broad range of [O2 ] reflective of their environment (80-260 μmol kg(-1) ). The role of pH variability should be recognized as an important feature in coastal oceans that has the capacity to modulate the effects of ocean acidification on biological responses. |
| Author | Navarro, Michael O. Levin, Lisa A. Frieder, Christina A. Gonzalez, Jennifer P. Bockmon, Emily E. |
| Author_xml | – sequence: 1 fullname: Frieder, Christina A – sequence: 2 fullname: Gonzalez, Jennifer P – sequence: 3 fullname: Bockmon, Emily E – sequence: 4 fullname: Navarro, Michael O – sequence: 5 fullname: Levin, Lisa A |
| BackLink | http://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=28203899$$DView record in Pascal Francis https://www.ncbi.nlm.nih.gov/pubmed/24343909$$D View this record in MEDLINE/PubMed |
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| Keywords | Fluctuations Oxygen Variable multistressor Acidification mussel Larva Plankton Bivalvia coastal variability pH planktonic larvae Ocean Invertebrata Mollusca semidiurnal pH fluctuations |
| Language | English |
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| Notes | http://dx.doi.org/10.1111/gcb.12485 NOAA - No. NA10OAR4170060; No. NA08OAR4170669 istex:F2896505DB23C4CF91887263407ACF4070262F31 ArticleID:GCB12485 California Sea Grant College Program - No. R/CC-02EPD; No. R/CC-04; No. R/OPCENV-09 NSF-OCE - No. 0927445; No. 1041062 Data S1. Adult spawning and larval culturing. ark:/67375/WNG-ZFB9BQC3-J ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 14 content type line 23 |
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| References | Lucas JS, Costlow JD (1979) Effects of various temperature cycles on the larval development of the gastropod mollusc Crepidula fornicata. Marine Biology, 51, 111-117. Kurihara H, Asai T, Kato S, Ishimatsu A (2008) Effects of elevated pCO2 on early development in the mussel Mytilus galloprovincialis. Aquatic Biology, 4, 225-233. Diaz RJ, Rosenberg R (2008) Spreading dead zones and consequences for marine ecosystems. Science, 321, 926-929. Clayton TD, Byrne RH (1993) Spectrophotometric seawater pH measurements: total hydrogen ion concentration scale calibration of m-cresol purple and at-sea results. Deep-Sea Research, 40, 2115-2129. Dupont S, Lundve B, Thorndyke M (2010) Near future ocean acidification increases growth rate of the lecithotrophic larvae and juveniles of the sea star Crossaster papposus. Journal of Experimental Zoology, 314, 382-389. Pörtner HO, Langenbuch M (2005) Synergistic effects of temperature extremes, hypoxia, and increases in CO2 on marine animals: from Earth history to global change. Journal of Geophysical Research, 110, C09S10. Crawford WR, Peña MA (2013) Declining oxygen on the British Columbia continental shelf. Atmosphere-Ocean, 51, 88-103. Waldbusser GG, Brunner EL, Haley BA, Hales B, Langdon CJ, Prahl FG (2013) A developmental and energetic basis linking larval oyster shell formation to acidification sensitivity. Geophysical Research Letters, 40, 2171-2176. Rilov G, Dudas SE, Menge BA, Grantham BA, Lubchenco J, Schiel DR (2008) The surf zone: a semi-permeable barrier to onshore recruitment of invertebrate larvae? Journal of Experimental Marine Biology and Ecology, 361, 59-74. Dickson AG, Millero FJ (1987) A comparison of the equilibrium constants for the dissociation of carbonic acid in seawater media. Deep-Sea Research, 34, 1733-1743. Eerkes-Medrano D, Menge BA, Sislak C, Langdon CJ (2013) Contrasting effects of hypoxic conditions on survivorship of planktonic larvae of rocky intertidal invertebrates. Marine Ecology Progress Series, 478, 139-151. Dufault AM, Cumbo VR, Fan T-Y, Edmunds PJ (2012) Effects of diurnally oscillating pCO2 on the calcification and survival of coral recruits. Proceedings of the Royal Society B, 279, 2951-2958. Moran AL, Emlet RB (2001) Offspring size and performance in variable environments: field studies on a marine snail. Ecology, 82, 1597-1612. Sastry AN (1979) Metabolic adaptation of Cancer irroratus developmental stages to cyclic temperatures. Marine Biology, 51, 243-250. Hofmann GE, Smith JE, Johnson KS et al. (2011) High-frequency dynamics of ocean pH: a multi-ecosystem comparison. PLoS ONE, 6, e28983. Shanks AL, Shearman RK (2009) Paradigm lost? Cross-shelf distributions of intertidal invertebrate larvae are unaffected by upwelling or downwelling. Marine Ecology Progress Series, 385, 189-204. Mehrbach C, Culberson CH, Hawley JE, Pytkowicz RN (1973) Measurement of the apparent dissociation constants of carbonic acid in seawater at atmospheric pressure. Limnology and Oceanography, 18, 897-907. Hayakaze E, Tanabe K (1999) Early larval shell development in mytilid bivalve Mytilus galloprovincialis. Venus, 58, 119-127. Carson HS, López-Duarte PC, Rasmussen L, Wang D, Levin LA (2010) Reproductive timing alters population connectivity in marine metapopulations. Current Biology, 20, 1926-1931. Orlando EF, Guillette LJ (2001) A re-examination of variaiton associated with environmentally stressed organisms. Human Reproduction Update, 7, 265-272. Cai W-J, Hu X, Huang W-J et al. (2011) Acidification of subsurface coastal waters enhanced by eutrophication. Nature Geoscience, 4, 766-770. Stramma L, Schmidtko S, Levin LA, Johnson GC (2010) Ocean oxygen minima expansions and their biological impacts. Deep-Sea Research, 57.4, 587-595. Gobler CJ, Talmage SC (2013) Short- and long-term consequences of larval stage exposure to constantly and ephemerally elevated carbon dioxide for marine bivalve populations. Biogeosciences, 10, 2241-2253. Feely RA, Sabine CL, Hernandez-Ayon JM, Ianson D, Hales B (2008) Evidence for upwelling of corrosive "acidified" water onto the continental shelf. Science, 320, 1490-1492. Gaylord B, Hill TM, Sanford E et al. (2011) Functional impacts of ocean acidification in an ecologically critical foundation species. Journal of Experimental Biology, 214, 2586-2594. Pechenik JA (1999) On the advantages and disadvantages of larval stages in benthic marine invertebrate life cycles. Marine Ecology Progress Series, 177, 269-297. Hochachka PW, Somero GN (2002) Biochemical Adaptation: mechanism and Process in Physiological Evolution. Oxford University Press, New York. Hauri C, Gruber N, Vogt M et al. (2013) Spatiotemporal variability and long-term trends of ocean acidification in the California Current System. Biogeosciences, 10, 193-216. Kurihara H (2008) Effects of CO2-driven ocean acidification on the early developmental stages of invertebrates. Marine Ecology Progress Series, 373, 275-284. Dickson AG, Sabine CL, Christian JR (2007) Guide to Best Practices for Ocean CO2 Measurements. PICES Special Publication 3, Sidney, British Columbia. Thomsen J, Gutowska MA, Saphörster J et al. (2010) Calcifying invertebrates succeed in a naturally CO2-rich coastal habitat but are threatened by high levels of future acidification. Biogeosciences, 7, 3879-3891. White MM, McCorkle DC, Mullineaux LS, Cohen AL (2013) Early exposure of bay scallops (Argopecten irradians) to high CO2 causes a decrease in larval shell growth. PLoS ONE, 8, e61065. Byrne M (2012) Global change ecotoxicology: Identification of early life history bottlenecks in marine invertebrates, variable species responses and variable experimental approaches. Marine Environmental Research, 76, 3-15. Bates NR, Best MHP, Neely K, Garley R, Dickson AG, Johnson RJ (2012) Detecting anthropogenic carbon dioxide uptake and ocean acidification in the North Atlantic Ocean. Biogeosciences, 9, 2509-2522. Bockmon EE, Frieder CA, Navarro MO, White-Kershek LA, Dickson AG (2013) Technical note: controlled experimental aquarium system for multi-stressor investigation of carbonate chemistry, oxygen saturation, and temperature. Biogeosciences, 10, 5967-5975. Keeling RF, Körtzinger A, Gruber N (2010) Ocean deoxygenation in a warming world. Annual Review of Marine Science, 2, 199-229. Frieder CA, Nam SH, Martz TR, Levin LA (2012) High temporal and spatial variability of dissolved oxygen and pH in a nearshore California kelp forest. Biogeosciences, 9, 3917-3930. Van Heuven SD, Pierrot JWB, Lewis RE, Wallace DWR (2011) MATLAB Program Developed for CO2 System Calculations, ORNL/CDIAC-105b. Oak Ridge, Tennessee, Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, U.S. Department of Energy. Chan F, Barth JA, Lubchenco J, Kirincich A, Weeks H, Peterson WT, Menge BA (2008) Emergence of anoxia in the California current large marine ecosystem. Science, 319, 920. Pörtner HO (2012) Integrating climate-related stressor effects on marine organisms: unifying principles linking molecule to ecosystem-level changes. Marine Ecology Progress Series, 470, 273-290. Shanks AL, Brink L (2005) Upwelling, downwelling, and cross-shelf transport of bivalve larvae: test of a hypothesis. Marine Ecology Progress Series, 302, 1-12. Gosselin LA, Chia F-S (1996) Prey selection by inexperienced predators: do early juvenile snails maximize net energy gains on their first attack? Journal of Experimental Marine Biology and Ecology, 199, 45-58. Capone DG, Hutchins DA (2013) Microbial biogeochemistry of coastal upwelling regimes in a changing ocean. Nature Geoscience, 6, 711-717. Bograd SJ, Castro CG, Di Lorenzo E, Palacios DM, Bailey H, Gilly W, Chavez FP (2008) Oxygen declines and the shoaling of the hypoxic boundary in the California Current. Geophysical Research Letters, 35, L12607. Widdows J, Newell RIE, Mann R (1989) Effects of hypoxia and anoxia on survival, energy metabolism, and feeding of oyster larvae (Crassostrea virginica, Gmelin). Biological Bulletin, 177, 154-166. Vaquer-Sunyer R, Duarte CM (2008) Thresholds of hypoxia for marine biodiversity. Proceedings of the National Academy of Sciences, 105, 15452-15457. Wang W, Widdows J (1991) Physiological responses of mussel larvae Mytilus edulis to environmental hypoxia and anoxia. Marine Ecology Progress Series, 70, 223-236. Hettinger A, Sanford E, Hill TM et al. (2012) Persistent carry-over effects of planktonic exposure to ocean acidification in the Olympia oyster. Ecology, 93, 2758-2768. Wootton JT, Pfister CA, Forester JD (2008) Dynamic patterns and ecological impacts of declining ocean pH in a high-resolution multi-year dataset. Proceedings of the National Academy of Sciences, 105, 18848-18853. Wilt FH (2005) Development biology meets material science: morphogenesis of biomineralized structures. Developmental Biology, 280, 15-25. Booth JAT, McPhee-Shaw EE, Chua P et al. (2012) Natural intrusions of hypoxic, low pH water into nearshore marine environments on the California coast. Continental Shelf Research, 45, 108-115. Gazeau F, Gattuso J-P, Greaves M, Elderfield H, Peene J, Heip CHR, Middelburg JJ (2011) Effect of carbonate chemistry alteration on the early embryonic development of the Pacific oyster (Crassostrea gigas). PLoS ONE, 6, e23010. Whitney FA, Freeland HJ, Robert M (2007) Persistently declining oxygen levels in the interior waters of the eastern subarctic Pacific. Progress in Oceanography, 75, 179-199. 1987; 34 1976 1973; 18 2008; 35 2008; 105 1971 2008; 4 2007; 75 2013; 8 2013; 6 2010; 20 2013; 10 2010; 314 2013; 51 2013; 478 2005; 302 2008; 319 1999; 58 2010; 57.4 1999; 177 2010; 2 2010; 7 2011; 214 1993; 40 2005; 110 2011 2013; 40 1989; 177 2007 1995 2002 2011; 4 2008; 321 2008; 320 2011; 6 2012; 76 2008; 361 1979; 51 2012; 93 2012; 470 2001; 82 2005; 280 2001; 7 2009; 385 1991; 70 1996; 199 2013 2012; 279 2012; 45 2008; 373 2012; 9 e_1_2_6_51_1 e_1_2_6_53_1 e_1_2_6_19_1 Costlow JDJ (e_1_2_6_12_1) 1971 e_1_2_6_13_1 e_1_2_6_36_1 e_1_2_6_11_1 e_1_2_6_34_1 e_1_2_6_17_1 e_1_2_6_55_1 e_1_2_6_38_1 e_1_2_6_57_1 e_1_2_6_43_1 e_1_2_6_20_1 e_1_2_6_41_1 e_1_2_6_9_1 e_1_2_6_5_1 e_1_2_6_7_1 e_1_2_6_49_1 e_1_2_6_3_1 e_1_2_6_22_1 e_1_2_6_28_1 e_1_2_6_45_1 e_1_2_6_26_1 e_1_2_6_47_1 e_1_2_6_52_1 e_1_2_6_54_1 e_1_2_6_10_1 e_1_2_6_31_1 e_1_2_6_50_1 Gabbott PA (e_1_2_6_24_1) 1976 Hayakaze E (e_1_2_6_30_1) 1999; 58 Hochachka PW (e_1_2_6_32_1) 2002 e_1_2_6_14_1 e_1_2_6_35_1 e_1_2_6_33_1 e_1_2_6_18_1 e_1_2_6_39_1 e_1_2_6_56_1 Dickson AG (e_1_2_6_15_1) 1995 e_1_2_6_16_1 e_1_2_6_37_1 e_1_2_6_58_1 e_1_2_6_42_1 e_1_2_6_21_1 e_1_2_6_40_1 e_1_2_6_8_1 e_1_2_6_4_1 e_1_2_6_6_1 e_1_2_6_25_1 e_1_2_6_48_1 e_1_2_6_23_1 e_1_2_6_2_1 e_1_2_6_29_1 e_1_2_6_44_1 e_1_2_6_27_1 e_1_2_6_46_1 |
| References_xml | – reference: Hauri C, Gruber N, Vogt M et al. (2013) Spatiotemporal variability and long-term trends of ocean acidification in the California Current System. Biogeosciences, 10, 193-216. – reference: Sastry AN (1979) Metabolic adaptation of Cancer irroratus developmental stages to cyclic temperatures. Marine Biology, 51, 243-250. – reference: Thomsen J, Gutowska MA, Saphörster J et al. (2010) Calcifying invertebrates succeed in a naturally CO2-rich coastal habitat but are threatened by high levels of future acidification. Biogeosciences, 7, 3879-3891. – reference: Dickson AG, Millero FJ (1987) A comparison of the equilibrium constants for the dissociation of carbonic acid in seawater media. Deep-Sea Research, 34, 1733-1743. – reference: Hochachka PW, Somero GN (2002) Biochemical Adaptation: mechanism and Process in Physiological Evolution. Oxford University Press, New York. – reference: Lucas JS, Costlow JD (1979) Effects of various temperature cycles on the larval development of the gastropod mollusc Crepidula fornicata. Marine Biology, 51, 111-117. – reference: Byrne M (2012) Global change ecotoxicology: Identification of early life history bottlenecks in marine invertebrates, variable species responses and variable experimental approaches. Marine Environmental Research, 76, 3-15. – reference: Capone DG, Hutchins DA (2013) Microbial biogeochemistry of coastal upwelling regimes in a changing ocean. Nature Geoscience, 6, 711-717. – reference: Gazeau F, Gattuso J-P, Greaves M, Elderfield H, Peene J, Heip CHR, Middelburg JJ (2011) Effect of carbonate chemistry alteration on the early embryonic development of the Pacific oyster (Crassostrea gigas). PLoS ONE, 6, e23010. – reference: Chan F, Barth JA, Lubchenco J, Kirincich A, Weeks H, Peterson WT, Menge BA (2008) Emergence of anoxia in the California current large marine ecosystem. Science, 319, 920. – reference: Hayakaze E, Tanabe K (1999) Early larval shell development in mytilid bivalve Mytilus galloprovincialis. Venus, 58, 119-127. – reference: Bates NR, Best MHP, Neely K, Garley R, Dickson AG, Johnson RJ (2012) Detecting anthropogenic carbon dioxide uptake and ocean acidification in the North Atlantic Ocean. Biogeosciences, 9, 2509-2522. – reference: Shanks AL, Brink L (2005) Upwelling, downwelling, and cross-shelf transport of bivalve larvae: test of a hypothesis. Marine Ecology Progress Series, 302, 1-12. – reference: Gobler CJ, Talmage SC (2013) Short- and long-term consequences of larval stage exposure to constantly and ephemerally elevated carbon dioxide for marine bivalve populations. Biogeosciences, 10, 2241-2253. – reference: Waldbusser GG, Brunner EL, Haley BA, Hales B, Langdon CJ, Prahl FG (2013) A developmental and energetic basis linking larval oyster shell formation to acidification sensitivity. Geophysical Research Letters, 40, 2171-2176. – reference: Moran AL, Emlet RB (2001) Offspring size and performance in variable environments: field studies on a marine snail. Ecology, 82, 1597-1612. – reference: Dupont S, Lundve B, Thorndyke M (2010) Near future ocean acidification increases growth rate of the lecithotrophic larvae and juveniles of the sea star Crossaster papposus. Journal of Experimental Zoology, 314, 382-389. – reference: Dufault AM, Cumbo VR, Fan T-Y, Edmunds PJ (2012) Effects of diurnally oscillating pCO2 on the calcification and survival of coral recruits. Proceedings of the Royal Society B, 279, 2951-2958. – reference: Hettinger A, Sanford E, Hill TM et al. (2012) Persistent carry-over effects of planktonic exposure to ocean acidification in the Olympia oyster. Ecology, 93, 2758-2768. – reference: Cai W-J, Hu X, Huang W-J et al. (2011) Acidification of subsurface coastal waters enhanced by eutrophication. Nature Geoscience, 4, 766-770. – reference: Hofmann GE, Smith JE, Johnson KS et al. (2011) High-frequency dynamics of ocean pH: a multi-ecosystem comparison. PLoS ONE, 6, e28983. – reference: Orlando EF, Guillette LJ (2001) A re-examination of variaiton associated with environmentally stressed organisms. Human Reproduction Update, 7, 265-272. – reference: Shanks AL, Shearman RK (2009) Paradigm lost? Cross-shelf distributions of intertidal invertebrate larvae are unaffected by upwelling or downwelling. Marine Ecology Progress Series, 385, 189-204. – reference: Wang W, Widdows J (1991) Physiological responses of mussel larvae Mytilus edulis to environmental hypoxia and anoxia. Marine Ecology Progress Series, 70, 223-236. – reference: Dickson AG, Sabine CL, Christian JR (2007) Guide to Best Practices for Ocean CO2 Measurements. PICES Special Publication 3, Sidney, British Columbia. – reference: Pörtner HO (2012) Integrating climate-related stressor effects on marine organisms: unifying principles linking molecule to ecosystem-level changes. Marine Ecology Progress Series, 470, 273-290. – reference: Van Heuven SD, Pierrot JWB, Lewis RE, Wallace DWR (2011) MATLAB Program Developed for CO2 System Calculations, ORNL/CDIAC-105b. Oak Ridge, Tennessee, Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, U.S. Department of Energy. – reference: Vaquer-Sunyer R, Duarte CM (2008) Thresholds of hypoxia for marine biodiversity. Proceedings of the National Academy of Sciences, 105, 15452-15457. – reference: Gaylord B, Hill TM, Sanford E et al. (2011) Functional impacts of ocean acidification in an ecologically critical foundation species. Journal of Experimental Biology, 214, 2586-2594. – reference: Feely RA, Sabine CL, Hernandez-Ayon JM, Ianson D, Hales B (2008) Evidence for upwelling of corrosive "acidified" water onto the continental shelf. Science, 320, 1490-1492. – reference: Widdows J, Newell RIE, Mann R (1989) Effects of hypoxia and anoxia on survival, energy metabolism, and feeding of oyster larvae (Crassostrea virginica, Gmelin). Biological Bulletin, 177, 154-166. – reference: Bockmon EE, Frieder CA, Navarro MO, White-Kershek LA, Dickson AG (2013) Technical note: controlled experimental aquarium system for multi-stressor investigation of carbonate chemistry, oxygen saturation, and temperature. Biogeosciences, 10, 5967-5975. – reference: Eerkes-Medrano D, Menge BA, Sislak C, Langdon CJ (2013) Contrasting effects of hypoxic conditions on survivorship of planktonic larvae of rocky intertidal invertebrates. Marine Ecology Progress Series, 478, 139-151. – reference: Rilov G, Dudas SE, Menge BA, Grantham BA, Lubchenco J, Schiel DR (2008) The surf zone: a semi-permeable barrier to onshore recruitment of invertebrate larvae? Journal of Experimental Marine Biology and Ecology, 361, 59-74. – reference: Gosselin LA, Chia F-S (1996) Prey selection by inexperienced predators: do early juvenile snails maximize net energy gains on their first attack? Journal of Experimental Marine Biology and Ecology, 199, 45-58. – reference: White MM, McCorkle DC, Mullineaux LS, Cohen AL (2013) Early exposure of bay scallops (Argopecten irradians) to high CO2 causes a decrease in larval shell growth. PLoS ONE, 8, e61065. – reference: Wilt FH (2005) Development biology meets material science: morphogenesis of biomineralized structures. Developmental Biology, 280, 15-25. – reference: Wootton JT, Pfister CA, Forester JD (2008) Dynamic patterns and ecological impacts of declining ocean pH in a high-resolution multi-year dataset. Proceedings of the National Academy of Sciences, 105, 18848-18853. – reference: Keeling RF, Körtzinger A, Gruber N (2010) Ocean deoxygenation in a warming world. Annual Review of Marine Science, 2, 199-229. – reference: Pechenik JA (1999) On the advantages and disadvantages of larval stages in benthic marine invertebrate life cycles. Marine Ecology Progress Series, 177, 269-297. – reference: Mehrbach C, Culberson CH, Hawley JE, Pytkowicz RN (1973) Measurement of the apparent dissociation constants of carbonic acid in seawater at atmospheric pressure. Limnology and Oceanography, 18, 897-907. – reference: Booth JAT, McPhee-Shaw EE, Chua P et al. (2012) Natural intrusions of hypoxic, low pH water into nearshore marine environments on the California coast. Continental Shelf Research, 45, 108-115. – reference: Whitney FA, Freeland HJ, Robert M (2007) Persistently declining oxygen levels in the interior waters of the eastern subarctic Pacific. Progress in Oceanography, 75, 179-199. – reference: Kurihara H (2008) Effects of CO2-driven ocean acidification on the early developmental stages of invertebrates. Marine Ecology Progress Series, 373, 275-284. – reference: Kurihara H, Asai T, Kato S, Ishimatsu A (2008) Effects of elevated pCO2 on early development in the mussel Mytilus galloprovincialis. Aquatic Biology, 4, 225-233. – reference: Carson HS, López-Duarte PC, Rasmussen L, Wang D, Levin LA (2010) Reproductive timing alters population connectivity in marine metapopulations. Current Biology, 20, 1926-1931. – reference: Crawford WR, Peña MA (2013) Declining oxygen on the British Columbia continental shelf. Atmosphere-Ocean, 51, 88-103. – reference: Bograd SJ, Castro CG, Di Lorenzo E, Palacios DM, Bailey H, Gilly W, Chavez FP (2008) Oxygen declines and the shoaling of the hypoxic boundary in the California Current. Geophysical Research Letters, 35, L12607. – reference: Clayton TD, Byrne RH (1993) Spectrophotometric seawater pH measurements: total hydrogen ion concentration scale calibration of m-cresol purple and at-sea results. Deep-Sea Research, 40, 2115-2129. – reference: Diaz RJ, Rosenberg R (2008) Spreading dead zones and consequences for marine ecosystems. Science, 321, 926-929. – reference: Frieder CA, Nam SH, Martz TR, Levin LA (2012) High temporal and spatial variability of dissolved oxygen and pH in a nearshore California kelp forest. Biogeosciences, 9, 3917-3930. – reference: Pörtner HO, Langenbuch M (2005) Synergistic effects of temperature extremes, hypoxia, and increases in CO2 on marine animals: from Earth history to global change. Journal of Geophysical Research, 110, C09S10. – reference: Stramma L, Schmidtko S, Levin LA, Johnson GC (2010) Ocean oxygen minima expansions and their biological impacts. Deep-Sea Research, 57.4, 587-595. – year: 2011 – volume: 40 start-page: 2115 year: 1993 end-page: 2129 article-title: Spectrophotometric seawater pH measurements: total hydrogen ion concentration scale calibration of m‐cresol purple and at‐sea results publication-title: Deep‐Sea Research – volume: 51 start-page: 243 year: 1979 end-page: 250 article-title: Metabolic adaptation of developmental stages to cyclic temperatures publication-title: Marine Biology – volume: 177 start-page: 154 year: 1989 end-page: 166 article-title: Effects of hypoxia and anoxia on survival, energy metabolism, and feeding of oyster larvae ( , Gmelin) publication-title: Biological Bulletin – volume: 93 start-page: 2758 year: 2012 end-page: 2768 article-title: Persistent carry‐over effects of planktonic exposure to ocean acidification in the Olympia oyster publication-title: Ecology – volume: 45 start-page: 108 year: 2012 end-page: 115 article-title: Natural intrusions of hypoxic, low pH water into nearshore marine environments on the California coast publication-title: Continental Shelf Research – volume: 105 start-page: 18848 year: 2008 end-page: 18853 article-title: Dynamic patterns and ecological impacts of declining ocean pH in a high‐resolution multi‐year dataset publication-title: Proceedings of the National Academy of Sciences – volume: 4 start-page: 766 year: 2011 end-page: 770 article-title: Acidification of subsurface coastal waters enhanced by eutrophication publication-title: Nature Geoscience – volume: 7 start-page: 3879 year: 2010 end-page: 3891 article-title: Calcifying invertebrates succeed in a naturally CO ‐rich coastal habitat but are threatened by high levels of future acidification publication-title: Biogeosciences – volume: 279 start-page: 2951 year: 2012 end-page: 2958 article-title: Effects of diurnally oscillating pCO on the calcification and survival of coral recruits publication-title: Proceedings of the Royal Society B – volume: 214 start-page: 2586 year: 2011 end-page: 2594 article-title: Functional impacts of ocean acidification in an ecologically critical foundation species publication-title: Journal of Experimental Biology – start-page: 293 year: 1976 end-page: 355 – volume: 319 start-page: 920 year: 2008 article-title: Emergence of anoxia in the California current large marine ecosystem publication-title: Science – volume: 110 start-page: C09S10 year: 2005 article-title: Synergistic effects of temperature extremes, hypoxia, and increases in CO on marine animals: from Earth history to global change publication-title: Journal of Geophysical Research – volume: 51 start-page: 88 year: 2013 end-page: 103 article-title: Declining oxygen on the British Columbia continental shelf publication-title: Atmosphere‐Ocean – volume: 6 start-page: e23010 year: 2011 article-title: Effect of carbonate chemistry alteration on the early embryonic development of the Pacific oyster ( ) publication-title: PLoS ONE – volume: 8 start-page: e61065 year: 2013 article-title: Early exposure of bay scallops ( ) to high CO causes a decrease in larval shell growth publication-title: PLoS ONE – volume: 314 start-page: 382 year: 2010 end-page: 389 article-title: Near future ocean acidification increases growth rate of the lecithotrophic larvae and juveniles of the sea star publication-title: Journal of Experimental Zoology – volume: 10 start-page: 2241 year: 2013 end-page: 2253 article-title: Short‐ and long‐term consequences of larval stage exposure to constantly and ephemerally elevated carbon dioxide for marine bivalve populations publication-title: Biogeosciences – volume: 35 start-page: L12607 year: 2008 article-title: Oxygen declines and the shoaling of the hypoxic boundary in the California Current publication-title: Geophysical Research Letters – volume: 6 start-page: e28983 year: 2011 article-title: High‐frequency dynamics of ocean pH: a multi‐ecosystem comparison publication-title: PLoS ONE – volume: 478 start-page: 139 year: 2013 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| SubjectTerms | Acidification Animal and plant ecology Animal, plant and microbial ecology Animals Biological and medical sciences chemistry climate Climate change coastal variability Diurnal variations Fluctuations Fundamental and applied biological sciences. Psychology General aspects growth & development Hydrogen-Ion Concentration Invertebrates Larva Larva - growth & development Larva - metabolism Larvae Larval development Marine Marine biology metabolism Mollusca Mollusks multistressor mussel mussels Mytilus Mytilus - growth & development Mytilus - metabolism Mytilus californianus Ocean acidification Oceans Oceans and Seas oxygen Oxygen - metabolism planktonic larvae Seawater Seawater - chemistry semidiurnal pH fluctuations survival rate variance |
| Title | Can variable pH and low oxygen moderate ocean acidification outcomes for mussel larvae? |
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