The DOI matches its Crossref record; 6 of the 6 references it cites were found in a registry or an index.
Effects of increased pCO2 and temperature on the North Atlantic spring bloom. I. The phytoplankton community and biogeochemical response
Open accessAbstract
The North Atlantic spring bloom is one of the largest annual biological events in the ocean, and is characterized by dominance transitions from siliceous (diatoms) to calcareous (coccolithophores) algal groups.To study the effects of future global change on these phytoplankton and the biogeochemical cycles they mediate, a shipboard continuous culture experiment (Ecostat) was conducted in June 2005 during this transition period.Four treatments were examined: (1) 12°C and 390 ppm CO 2 (ambient control), (2) 12°C and 690 ppm CO 2 (high pCO 2 ), (3) 16°C and 390 ppm CO 2 (high temperature), and (4) 16°C and 690 ppm CO 2 ('greenhouse').Nutrient availability in all treatments was designed to reproduce the low silicate conditions typical of this late stage of the bloom.Both elevated pCO 2 and temperature resulted in changes in phytoplankton community structure.Increased temperature promoted whole community photosynthesis and particulate organic carbon (POC) production rates per unit chlorophyll a.Despite much higher coccolithophore abundance in the greenhouse treatment, particulate inorganic carbon production (calcification) was significantly decreased by the combination of increased pCO 2 and temperature.Our experiments suggest that future trends during the bloom could include greatly reduced export of calcium carbonate relative to POC, thus providing a potential negative feedback to atmospheric CO 2 concentration.Other trends with potential climate feedback effects include decreased community biogenic silica to POC ratios at higher temperature.These shipboard experiments suggest the need to examine whether future pCO 2 and temperature increases on longer decadal timescales will similarly alter the biological and biogeochemical dynamics of the North Atlantic spring bloom.
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Cites
Orr, J. C., Fabry, V. J., Aumont, O., Bopp, L., Doney, S. C., Feely, R. A., Gnanadesikan, A., Gruber, N., Ishida, A., Joos, F., et al. (2005) · Nature · doi:10.1038/nature04095 · Cited by 4,590
Oceanic phytoplankton, atmospheric sulphur, cloud albedo and climate
Charlson, R. J., Lovelock, J. E., Andreae, M. O., & Warren, S. G. (1987) · Nature · doi:10.1038/326655a0 · Cited by 4,305
Simulated response of the ocean carbon cycle to anthropogenic climate warming
Sarmiento, J. L., Hughes, T. M. C., Stouffer, R. J., & Manabe, S. (1998) · Nature · doi:10.1038/30455 · Cited by 899 · cited 1×
“One of the Ecostats was maintained using this system at ambient SST (12°C) and the other was 4°C above ambient temperature, as has been predicted for high latitude ocean regimes by the year 2100 (Sarmiento et al. 1998, 2004).”
MethodPotential impact of climate change on marine export production
Bopp, L., Monfray, P., Aumont, O., Dufresne, J., Le Treut, H., Madec, G., Terray, L., & Orr, J. C. (2001) · Global Biogeochemical Cycles · doi:10.1029/1999gb001256 · Cited by 514 · cited 1×
“At the same time, warming associated with the release of greenhouse gases into the atmosphere has been predicted to raise sea surface temperature (SST) by 1 to 4°C over the next 100 yr (Bopp et al. 2001, Alley et al. 2007).”
BackgroundCarbon acquisition of bloom‐forming marine phytoplankton
Rost, B., Riebesell, U., Burkhardt, S., & Sültemeyer, D. (2003) · Limnology and Oceanography · doi:10.4319/lo.2003.48.1.0055 · Cited by 486
Ziveri, P., de Bernardi, B., Baumann, K.-H., Stoll, H. M., & Mortyn, P. G. (2007) · Deep Sea Research Part II: Topical Studies in Oceanography · doi:10.1016/j.dsr2.2007.01.006 · Cited by 202
Cited by
Climate change and ocean acidification effects on seagrasses and marine macroalgae
Koch, M., Bowes, G., Ross, C., & Zhang, X. (2013) · Global Change Biology · doi:10.1111/j.1365-2486.2012.02791.x · Cited by 869
Harmful algal blooms and climate change: learning from the past and present to forecast the future
Wells, M. L., Trainer, V. L., Smayda, T. J., Karlson, B. S. O., Trick, C. G., Kudela, R. M., Ishikawa, A., Bernard, S., Wulff, A., Anderson, D. M., et al. (2015) · Harmful Algae · doi:10.1016/j.hal.2015.07.009 · Cited by 828
Constable, A. J., Melbourne‐Thomas, J., Corney, S. P., Arrigo, K. R., Barbraud, C., Barnes, D. K. A., Bindoff, N. L., Boyd, P. W., Brandt, A., Costa, D. P., et al. (2014) · Global Change Biology · doi:10.1111/gcb.12623 · Cited by 623
Hofmann, G. E., Barry, J. P., Edmunds, P. J., Gates, R. D., Hutchins, D. A., Klinger, T., & Sewell, M. A. (2010) · Annual Review of Ecology, Evolution, and Systematics · doi:10.1146/annurev.ecolsys.110308.120227 · Cited by 533
Self-citationMicroorganisms and ocean global change
Hutchins, D. A., & Fu, F. (2017) · Nature Microbiology · doi:10.1038/nmicrobiol.2017.58 · Cited by 499
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Metadata
- Authors
- Feng, Y., Hare, C., Leblanc, K., Rose, J., Zhang, Y., DiTullio, G., Lee, P., Wilhelm, S., Rowe, J., Sun, J., Nemcek, N., Gueguen, C., Passow, U., Benner, I., Brown, C., & Hutchins, D.
- Venue
- Marine Ecology Progress Series
- Publisher
- Inter-Research Science Center
- Published
- 2009-08-19
- Volume
- 388
- Pages
- 13-25
- ISSN
- 0171-8630 (ISSN-L)
- 1616-1599
- OpenAlex
- W2143402417
- Cited by
- 248
- References
- 6
- FWCI
- 13.03
- Type
- journal article
- Language
- en
- Open access
- bronze
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- Feng, Y., Hare, C., Leblanc, K., Rose, J., Zhang, Y., DiTullio, G., Lee, P., Wilhelm, S., Rowe, J., Sun, J., Nemcek, N., Gueguen, C., Passow, U., Benner, I., Brown, C., & Hutchins, D. (2009). Effects of increased pCO2 and temperature on the North Atlantic spring bloom. I. The phytoplankton community and biogeochemical response. Marine Ecology Progress Series. https://doi.org/10.3354/meps08133
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