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Oceanography in 2025: Proceedings of a Workshop (2009)
Ocean Studies Board (OSB)

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Glickson, Deborah. "Understanding Phytoplankton Bloom Development--Bess Ward and Mary Jane Perry." Oceanography in 2025: Proceedings of a Workshop. Washington, DC: The National Academies Press, 2009.

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Oceanography in 2025: Proceedings of a Workshop

Understanding Phytoplankton Bloom Development

Bess Ward* and Mary Jane Perry

WHAT QUESTIONS REMAIN UNANSWERED?

Historical biogeographical data sets document global and regional patterns in phytoplankton and zooplankton species distributions. Although correlations with, for example, temperature and nutrient concentrations, are strong, they remain descriptive. At a very fundamental level, we still do not know what controls the species composition of phytoplankton assemblages and what key environmental variables determine the success or failure of different groups under different conditions. Even biogeochemical models that include functional groups do so with low resolution and depend upon simple variables such as size to distinguish groups. Although size sounds like an objective variable, it’s not obvious that actual phytoplankton fall into ecologically meaningful size categories. Thus we need to link observations of phytoplankton species to measured and model outcomes to determine what factors matter to phytoplankton, and thence to predictive power in response to anthropogenic changes such as nutrient enrichment and global warming.

WHY FOCUS ON PHYTOPLANKTON BLOOMS?

Molecular ecological investigations, first of prokaryotic plankton and more recently of eukaryotic phytoplankton, have revealed a vast diversity of species in natural assemblages. The diversity at the molecular level is

*

Princeton University

School of Marine Sciences, University of Maine

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115
Front Matter (R1-R12)
Introduction and Goals--Linwood Vincent (1-2)
Integrated Oceanography in 2025--John J. Cullen (3-5)
Oceanography in 2028--Mark Abbott (6-10)
The Changing Relationship Between Humans and the Ocean--J. G. Bellingham (11-13)
Societal Implications for Ocean Research in 2025--Matthew Alford (14-16)
Oceanography in 2025: Responding to Growing Populations on a Rapidly Changing Planet--Scott Glenn (17-21)
Some Thoughts on Physical Oceanography in 2025--Ken Melville (22-25)
The Next-Generation Coupled Atmosphere-Wave-Ocean-Ice-Land Models for Ocean Research and Prediction--Shuyi S. Chen (26-27)
Science in Action, Episode 1: Exploring Boundaries--Meghan F. Cronin (28-30)
Real Time Decision Support Everywhere--Nathaniel G. Plant (31-35)
Trends in Oceanography: More Data, More People, More Relevance--J. Thomson (36-38)
Future Developments to Observational Physical Oceanography--Tom Sanford (39-42)
Prospects for Oceanography in 2025--Michael Gregg (43-45)
Oceanography in 2025--John Orcutt (46-48)
Thoughts on Oceanography in 2025--Daniel Rudnick (49-51)
The Role of Observations in the Future of Oceanography--Raffaele Ferrari (52-54)
The Future . . . One More Time--Rob Pinkel (55-57)
The Role of Acoustics in Ocean Observing Systems--Peter Worcester and Walter Munk (58-62)
Oceanography in 2025--Walter Munk (63-64)
Physical Oceanography in 2025--Chris Garrett (65-67)
A Vision of Future Physical Oceanography Research--James J. O'Brien (68-69)
Some Thoughts on Logistics, Mixing, and Power--J. N. Moum (70-72)
Ageostrophic Circulation in the Ocean--Peter Niiler (73-76)
The Future of Ocean Modeling--Sonya Legg, Alistair Adcroft, Whit Anderson, V. Balaji, John Dunne, Stephen Griffies, Robert Hallberg, Matthew Harrison, Isaac Held, Tony Rosati, Robbie Toggweiler, Geoff Vallis, and Laurent White (77-80)
Towards Nonhydrostatic Ocean Modeling with Large-eddy Simulation--Oliver B. Fringer (81-83)
Simulations of Marine Turbulence and Surface Waves: Potential Impacts of Petascale Technology--Peter P. Sullivan (84-88)
Computational Simulation and Submesoscale Variability--James C. McWilliams (89-91)
Ocean Measurements from Space in 2025--A. Freeman (92-97)
Future of Nearshore Processes Research--Rob Holman (98-100)
Future Directions in Nearshore Oceanography--H. Tuba Özkan-Haller (101-103)
Science Strategies for the Arctic Ocean--Mary-Louise Timmermans (104-106)
Submesoscale Variability of the Upper Ocean: Patchy and Episodic Fluxes Into and Through Biologically Active Layers--Daniel Rudnick, Mary Jane Perry, John J. Cullen, Bess Ward, and Kenneth S. Johnson (107-110)
Who's Blooming? Toward an Understanding of Why Certain Species Dominate Phytoplankton Blooms--Mary Jane Perry, Michael Sieracki, Bess Ward, and Alan Weidemann (111-114)
Understanding Phytoplankton Bloom Development--Bess Ward and Mary Jane Perry (115-117)
From Short Food Chains to Complex Interaction Webs: Biological Oceanography in 2025--Kelly J. Benoit-Bird (118-120)
The Interface Between Biological and Physical Processes--Mark Abbott (121-123)
Research on Higher Trophic Levels--Daniel P. Costa, Yann Tremblay, and Sean Hayes (124-129)
Marine Biogeochemistry in 2025--Kenneth S. Johnson (130-134)
Next-Generation Oceanographic Sensors for Short-Term Prediction/Verification of In-water Optical Conditions--Mark L. Wells (135-137)
Evolution of Autonomous Platform for Sustained Ocean Observations--Russ E. Davis (138-140)
Toward an Interdisciplinary Ocean Observing System in 2025--Eric D'Asaro (141-143)
Small Scale Ocean Dynamics in 2025--Jonathan Nash (144-145)
Oceanography in 2025--Dana R. Yoerger (146-149)
The Research Vessel Problem--J. N. Moum, Eric D'Asaro, Mary-Louise Timmermans, and Peter Niiler (150-152)
"Ocean Mapping" in 2025--Larry Mayer (153-156)
Seismic Oceanography: Imaging Oceanic Finestructure with Reflection Seismology--W. Steven Holbrook (157-162)
The Ocean Planet 2.0: A Vision for 2025--Justin Manley (163-165)
Force Projection Through the Littoral Zone: Optical Considerations--Kendall Carder (166-170)
Large Scale Phase-resolved Simulations of Ocean Surface Waves--Yuming Liu and Dick K.P. Yue (171-176)
Appendixes (177-178)
Appendix A: Workshop Agenda (179-180)
Appendix B: Workshop Participants (181-186)

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OCR for page 115
Oceanography in 2025: Proceedings of a Workshop Understanding Phytoplankton Bloom Development Bess Ward* and Mary Jane Perry† WHAT QUESTIONS REMAIN UNANSWERED? Historical biogeographical data sets document global and regional patterns in phytoplankton and zooplankton species distributions. Although correlations with, for example, temperature and nutrient concentrations, are strong, they remain descriptive. At a very fundamental level, we still do not know what controls the species composition of phytoplankton assemblages and what key environmental variables determine the success or failure of different groups under different conditions. Even biogeochemical models that include functional groups do so with low resolution and depend upon simple variables such as size to distinguish groups. Although size sounds like an objective variable, it’s not obvious that actual phytoplankton fall into ecologically meaningful size categories. Thus we need to link observations of phytoplankton species to measured and model outcomes to determine what factors matter to phytoplankton, and thence to predictive power in response to anthropogenic changes such as nutrient enrichment and global warming. WHY FOCUS ON PHYTOPLANKTON BLOOMS? Molecular ecological investigations, first of prokaryotic plankton and more recently of eukaryotic phytoplankton, have revealed a vast diversity of species in natural assemblages. The diversity at the molecular level is * Princeton University † School of Marine Sciences, University of Maine

OCR for page 116
Oceanography in 2025: Proceedings of a Workshop even greater than can be determined by the best microscopist, and modern methods such as DNA/RNA microarrays can evaluate diversity and abundance rapidly in relatively high throughput mode. The fact remains, however, that despite the large background diversity, only a very small number of types ever reaches really high abundance in blooms. Irigoien et al. (2004) showed that the highest biomass/production occurs mostly in high biomass blooms and these blooms are due to only four phytoplankton types: diatoms, coccolithophorids, Phaeocystis and dinoflagellates. Thus blooms, although rare and geographically small, are inordinately important to overall marine productivity and are dominated by a few types. WHAT CONTROLS THE SPECIES COMPOSITION OF PHYTOPLANKTON BLOOMS? The answer to this question depends on the factors that cause a high diversity, low abundance assemblage to develop into a low diversity, high abundance bloom. We suspect that the critical events occur long before the typical oceanographic measurement—chlorophyll or some other measure of biomass—can detect changes in the assemblage. The important responses that allow some species to win and cause others to lose must occur very soon after conditions change to allow a bloom: introduction of new nutrients by advection or upwelling, cessation of mixing due to surface warming, etc. Responses to environmental changes occur at the level of gene expression, probably often in genes that we have not yet identified or whose ecological significance we have not yet grasped. Thus fundamental molecular biological research is required to identify targets for response assay development. WHAT NEW TECHNOLOGIES COULD BE DEVELOPED AND WHAT QUESTIONS ANSWERED? In order to investigate the early development of phytoplankton blooms, it is necessary to begin sampling even before there is indication that changes are occurring. This can be done in manipulative experiments with large volume incubations at sea or on land, or by using remote observations to predict likely bloom development and then undertake in situ sampling. In order to determine the appropriate time scales for investigation of phytoplankton responses, some additional work with pure cultures is probably warranted. Then both experimental and in situ sampling can be scaled to catch, e.g., changes in gene expression that can occur on the order of minutes to hours. The development of large phytoplankton blooms depends partly on the absence or lag of grazing,

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Oceanography in 2025: Proceedings of a Workshop and overall production is thus subject to top-down control. The initial response at the genetic level that allows some species to take advantage of episodic changes in growth conditions, however, is fundamentally bottom-up. We must be able to identify and interpret such responses long before food web interactions become obvious. WHAT TECHNOLOGIES ARE REQUIRED? The two basic needs are development of technology to evaluate gene diversity and expression for many different phytoplankton species rapidly and specifically, and to deploy those methods on samples collected at appropriate time and space scales. It’s hard to imagine being able to carry out the biological measurements required to assess early bottom-up responses outside the laboratory, but some progress has been made. In situ quantitative polymerase chain reaction (Q-PCR) and hybridization methodologies are under development (John Paul, Chris Scholin). By selecting a few well-characterized genes, very specific assays can be developed to identify major phylotypes and assess gene expression among them. Functional gene microarrays offer a way to analyze the relative abundance and level of gene expression of many different kinds of genes from a multitude of different organisms simultaneously. At the very least, frequent sample collection and preservation can be done so that laboratory based analyses can be linked to remotely measured chemical and physical variables. Remote sampling and sample processing are engineering challenges beyond my insights. Clearly it’s not just technology, but communication between e.g., molecular biologists and engineers, which will make important advances possible. HOW WILL THE RESEARCH BE CONDUCTED? In the analysis of actual blooms, high frequency sampling and relatively rapid analysis is required. This probably requires a combination of remotely operated vehicles, ships and laboratory analysis. Real time analysis is not necessary for everything as long as real time sampling can be coordinated with the necessary physical and chemical measurements. In order to develop molecular assays for the key genetic responses involved in bloom development, it is also necessary to support laboratory based molecular biological research. This can go on in parallel, as genetic samples can often be reanalyzed when new tools become available. REFERENCE Irigoien, X., J. Huisman, and R.P. Harris. 2004. Global Diversity Patterns of Marine Phytoplankton and Zooplankton. Nature. 429(6994): 863-867.