Project: Bermuda Atlantic Time-series Study
Ocean Carbon & Biogeochemistry [OCB]
U.S. Joint Global Ocean Flux Study [U.S. JGOFS]
URL: Project Web Site
Start date: 1988-10
End date: 2013-08
Geolocation: Northwest Sargasso Sea at 32 deg 10' N 64 deg 30' W
A full description of the BATS research program (including links to the processed BATS data) is available from the BATS Web site (see http://www.bios.edu/research/bats.html. Any data from contributed from selected ancillary projects will appear below in the datasets listing.
The Bermuda Atlantic Time-Series Study
Contributed by Mike Lomas (updated 30 September 2010 by cchandler)
Introduction and Scientific Background
The Bermuda Atlantic Time-series Study (BATS, 32° 10'N, 64° 30'W) was established in 1988 to study the ocean carbon cycle by analyzing important hydrographic and biological parameters throughout the water column. BATS complements the other Sargasso Sea time-series, the Ocean Flux Program (OFP) a deep sediment trap mooring in place since 1978, and Hydrostation "S" a hydrographic time-series sampled approximately biweekly since 1954. Currently, BATS makes monthly measurements of important hydrographic, biological and chemical parameters throughout the water column at different sites within the Sargasso Sea.
Long-term time series are a powerful tool for investigating ocean biogeochemistry and its effects on the global carbon cycle. The seasonal, interannual and longer-scale dynamics of carbon and nutrient cycles in the upper ocean control ecosystem productivity, the net exchange of CO2 and other radiatively important gases between the atmosphere and the ocean, and the distribution of many biogenic elements in the marine environment. The Bermuda Atlantic Time-Series Study (BATS) is one of three long-term, ship-based ocean time series research sites, the other two being: the Hawaii Ocean Time-series (HOT) conducting systematic and sustained biogeochemical and physical oceanographic measurements at the deep-ocean site, Station ALOHA (A Long-Term Oligotrophic Habitat Assessment; 22° 45'N, 158° 00'W), located 100 km north of Oahu, Hawaii; and the Carbon Retention in a Colored Ocean Time Series (CARIACO) located in the southeastern Caribbean Sea, off the coast of Venezuela (10° 30'N, 64° 40'W) and visited by ship once per month since November 1995. Individually, the three ship-based ocean time series sites have been used to examine processes that occur in their respective geographic domains. Together, they have the potential to provide information on interannual to decadal-scale variability in global ocean processes and the climate system.
Understanding the controls on the Sargasso Sea carbon cycle requires that we not only understand each of its biogeochemical component processes but also the physical processes that move water within and through the BATS study region. The focus of the BATS program has been, and continues to be, improving our understanding of the "time-varying" components of the ocean carbon cycle, related biogenic elements of interest (e.g. nitrogen, phosphorus, silica), and identifying the relevant physical, chemical and ecosystem properties responsible for this variability. Within this context, there are a number of continuing goals and objectives for the BATS research program, including:
1. Document the seasonal, and interannual to decadal scale variability in carbon and nutrient cycles, and biological community structure in the oligotrophic gyre of the North Atlantic Ocean. This includes, for example, understanding the extent to which they are coupled or uncoupled in the surface ocean.
2. Quantify the role of ocean-atmosphere coupling and climate forcing on air-sea exchange of CO2, and carbon export to the ocean interior. Carbon cycle studies include both inorganic and organic carbon, and for the latter, both particulate and dissolved phases. Of particular interest are the controls on partitioning of carbon between particulate and dissolved phases.
3. Study the role of physical forcing (e.g., surface fluxes of heat, freshwater and momentum) on planktonic community structure and function, and impact on biogeochemical cycles (including new and export productivity).
4. Study the role of climate-induced variability in surface fluxes on planktonic community structure and function.
5. Provide a testbed for the introduction and validation of new oceanographic tools and technologies; generate a dataset that can be utilized by empiricists and modelers to test new hypotheses; and build a framework for educating and training future oceanographers.
Temporal Dynamics of Hydrography and Element Cycles, and their Spatial Context
The BATS (1988-) and Hydrostation S (1954-) time-series allow observation of seasonal to interannual to decadal changes in hydrography and elemental cycles of carbon, nitrogen and phosphorus. In the section below, we briefly discuss some of the research findings resulting from the BATS project. Over the last twenty years, temperature and salinity in the upper ocean layers of the subtropical gyre at BATS has increased significantly with concurrent changes in stratification (Johnson and Knap, pers. comm.; Bates 2007) and reorganization of the hydrological cycle. Over the last 50 years, BATS/Hydrostation S data reveal a large increase in ocean heat (~0.01o C y-1) and salt (~0.002 y-1) content in the upper ~300 m (Johnson and Knap, pers. comm.).
On societally relevant timescales (e.g., decades to centuries), oceanic biological processes sequester large quantities of atmospheric carbon, modulating the concentrations of CO2 in the lower atmosphere (IPCC 1990; 2001). The combined BATS/Hydrostation S CO2 time-series (from 1983) is the longest continuous record of oceanic uptake of anthropogenic CO2, changes in ocean acidification and an increase in CO2 inventories (IPCC 2007; Bates 2007; Bates and Peters 2007). The surface ocean DIC content has increased at an average rate of ~0.7 µmoles kg-1 yr-1 while pH has increased, and carbonate saturation states have decreased (Bates 2007). Air-sea CO2 fluxes have also increased over the last two decades as windspeed has increased in this sector of the subtropical gyre in response to climate change and climate mode variability (such as North Atlantic Oscillation, NAO; El Niño-Southern Oscillation, ENSO). However, in the North Atlantic subtropical gyre, the CO2 content of the 18oC subtropical mode water (i.e., Eighteen Degree Water, EDW; lying between the seasonal and permanent thermoclines) has increased at a rate (e.g., ~2.2 µmoles kg-1 yr-1; Bates et al. 2002) that is double the rate in surface waters. This increase has been related to changes in ocean mixing and NAO variability, and has resulted in enhanced storage of CO2 in EDW (with an upper limit of ~2.5 Pg C) over the last two decades. Over the last five years, the rate of increase in DIC content of EDW has slowed (although still increasing) while dissolved oxygen content of EDW has increased significantly by ~15 µmoles kg-1, perhaps indicative of reduced remineralization of exported organic matter from the surface ocean or the site of EDW formation.
Seasonal to Interannual Variability in Macronutrient Cycles
Historically, biologists and geochemists have been at odds about whether N or P limits primary production in the world's ocean (e.g. Codispoti 1989; Falkowski et al. 1998; Tyrrell 1999). Leaving aside the now demonstrated importance of iron from this discussion (e.g. Coale et al. 1996), Michaels et al. 2001) have hypothesized that there are feedback-dependent oscillations between N- and P-limited states mediated by the activity of nitrogen-fixers. The dominant oceanic N2-fixing species were believed to be Trichodesmium spp. and the diatom-symbiont Richelia, but new molecular biological techniques have found a great diversity of single-celled prokaryotes that possess and express the genes for N2-fixation (e.g. Zehr et al. 2001). The presence of these additional diazotrophs may further enhance the important role of N2-fixers in the global N cycle, and has significant implications for the coupling of phosphorus and nitrogen cycles in the ocean. At BATS, the presence of excess nitrate relative to Redfield proportions of phosphorus in the thermocline has been attributed to nitrogen fixation (e.g. Michaels et al. 1996; Gruber and Sarmiento 1997; Hood et al. 2001), but contradictory evidence remains about it's quantitative significance (e.g. Orcutt et al. 2001; Hansell et al. 2004). Studies on the controls and magnitude of new production in the oligotrophic gyre of the North Atlantic will continue through BATS and related projects, for example, to focus on nitrogen fixation, variability of excess nitrate (e.g. Bates and Hansell 2004) and non-Redfield C:N:P production and remineralization processes, mesoscale and submesoscale forcing/modulation of new and export production, and iron cycling and availability.
One of the significant advances made during the BATS program is a re-evaluation of the gravitational flux of particulate organic carbon (POC) from the euphotic zone which was thought to dominate biological carbon sequestration (i.e. the Biological Carbon Pump) to the deep ocean. Export production was scaled to rates of primary production (PP; e.g. Eppley and Peterson 1979), and gravitational flux scaled (exponentially decreasing with depth) to near surface sediment trap measurements (e.g. Martin et al. 1987). In contrast to expectations, however, no meaningful relationships have been found between PP and POC flux at either the BATS or HOT sites (e.g. Karl et al. 2001b; Brix et al. 2006). Instead, export pathways that were poorly quantified a decade ago - export of dissolved organic carbon (DOC), "active carbon transport" by diel migrant zooplankton and food web influences on the partitioning of primary production between POC and dissolved organic carbon (DOC) - have emerged as significant terms in the biological pump of carbon to the ocean interior (e.g. Carlson et al. 1994; Steinberg et al. 2000; Lomas et al. 2002). The question originally posed by the time-series sites, "what controls carbon export flux", is therefore still an open and active area of BATS research.
Multi-year variability in Macronutrient Cycles
During the last decade, complex coupling between ocean physics and longer time scale modes of climate variability (such as NAO and ENSO) has increasingly been demonstrated. Only more recently has coupling between ocean biogeochemical dynamics/biological community structure and mode of climate variability been demonstrated, for example, in the Pacific Ocean (Chavez et al. 2003). In the North Atlantic, significant correlative relationships between NAO and the interannual variability of many biogeochemical properties (e.g. mixed layer depth, SST, PP, nutrients; Bates 2001b; Oschlies 2001) have been shown. An inverse correlation has also been found at BATS between the NAO index and the relative abundance of haptophytes (e.g., coccolithophores; Lomas and Bates 2004) during the winter/spring bloom. Given the potential importance of this taxonomic group in the mineral ballasting of POC fluxes (e.g., Armstrong et al. 2002) greater understanding of coccolithophore population dynamics, and their role in subtropical biogeochemical cycles, under current and future ocean scenarios is clearly necessary.
Diatoms and other large phytoplankton are relatively rare (based upon size-fractionation and pigment bio-markers; Glover et al. 1988; Steinberg et al. 2001) but are actively growing and sedimenting from the surface ocean (Brzezinski and Nelson 1995a; Brzezinski and Kosman 1996; Nelson and Brzezinski 1997; Krause et al. submitted). Indeed, diatom populations at BATS contribute disproportionately to overall system productivity (Sweeney et al. 2003; Mcgillicuddy et al. 2007) and export (Nelson and Brzezinski 1997; Krause et al. submitted) through short-lived episodic events, a finding consistent with other research conducted in the North Atlantic subtropical gyre (Maranon et al. 2001). To highlight their importance for biogeochemical cycles in the Sargasso Sea, from ~1996 to ~2000 presumed active growth of resident diatom populations let to a nearly 50% drawdown in ambient silica concentrations within the euphotic zone, while suspended, but presumably sinking, biogenic silica concentrations from 200-1000 m doubled during that same period (Krause, Nelson and Lomas, in prep). The winters of 1996 to 2000 were characterized by low and sometimes negative NAO values, but since then silicate concentrations have returned to pre-1996 values (~0.8 - 1.0 µmol kg-1) and suspended biogenic silica concentrations below 200 m have decreased.
Mesoscale Variability and Spatial Context
Several major projects and BATS ancillary projects over the last five years have provided invaluable understanding of process and context for interpreting temporal variability at BATS. For example, mesoscale eddies have long been postulated as modulators of nutrient dynamics in the subtropical gyre (e.g., McGillicuddy et al. 1998a), and the recent EDDIES project has provided new understanding of this role (e.g., McGillicuddy et al. 2007). Nutrient dynamics and organic matter export were the focus of recent studies focusing on winter convective mixing (Lomas, Lipschultz, Nelson and Bates) while the CLIMODE project (Marshall, Joyce et al.) is focused on understanding the formation and fate of EDW formation in the subtropical gyre. In addition, there are ongoing studies of iron cycling (Sedwick and Church), dynamics of DMS (Dacey, Toole and Bates) and DOP (Lomas, Dyhrman and Ammerman), and water mass age-tracers such as 7Be (Kadko) at BATS. BATS provides the temporal context and observations for empirical and model understanding of these synergistic projects (e.g., EDDIES), while these studies themselves help elucidate process and mechanisms that lead to better understanding of the causes of seasonal to decadal variability at BATS and in the subtropical gyre of the North Atlantic Ocean.
The goals and objectives outlined above provide the motivation and rationale for the BATS project. The key questions and hypotheses emerging from past data synthesis and interpretation that will be evaluated in the next phase (years 21-25) of the project are described briefly below. The BATS program sampling strategy describes a core list of physical and biochemical measurements that are made, and the quality control and assurance protocols that are in place. In addition to the core sampling program, numerous ancillary research projects utilize the BATS project.
Key Questions and Hypotheses
The goals and objectives described above form the basis for continued research at the BATS site. Further to these points, it is becoming increasingly apparent that biogeochemical variability at BATS originates from a wide range of temporal scales from sub-mesoscale to multi-year/decadal. Local physical forcing link these timescales and are ultimately tied to larger-scale and longer-term atmospheric and climatic changes. Climatological forcing of ocean ecosystems by ENSO has been demonstrated in the Pacific Ocean (e.g., Karl et al. 2001a; Chavez et al. 2003). Likewise, in the deeper ocean of the Sargasso Sea, relationships between physics and climate can be clearly demonstrated (e.g., Joyce and Talley 1996). However, in the upper ocean, the inherent mesoscale variability of the Sargasso Sea (McGillicuddy and Robinson 1997; McGillicuddy et al. 1998b; McGillicuddy et al. 1999; McGillicuddy and Kosnyrev 2001) potentially masks the impact of atmospheric forcing over annual or shorter timescales, while exhibiting a very scientifically interesting dynamic in its own right. Indeed, long term modeling studies suggest the upper ocean heat and salinity budgets are balanced locally with 1-D models capturing 90% of the observed variance for the upper 100m (e.g., Johnson 2003). Despite these problems, modes of climate variability, such as NAO and ENSO have been shown to impact the interannual variability of hydrography, biogeochemistry and planktonic community structure at BATS (e.g., Bates 2001a; Bates et al. 2002; Gruber et al. 2002; Lomas and Bates 2004). For example, anomalies of temperature, integrated primary production, mixed layer depth and CO2 concentrations at BATS are significantly correlated to variability of NAO, whereas anomalies of salinity and alkalinity are correlated to ENSO variability. As the BATS time series record extends past two decades, our ability to observe and decipher relationships between climate and biogeochemistry continues to improve. Thus, one of the on-going objectives of BATS is to further investigate the mechanistic relationships between climate forcing and surface ocean biogeochemistry and ultimately improve our ability to predict the effects of climate change on subtropical ocean ecosystems.
Biological community structure within the pelagic food web has significant impacts on vertical transport and cycling of elements in the sea; in particular the partitioning of carbon fixed during primary production between particulate and dissolved pools. Generally speaking, the size distribution of primary producers, the trophic position of consumers and the extent to which both population cycles are coupled or uncoupled determines the proportion of primary production that is exported from the surface ocean as particles. This producer/consumer balance also governs the composition and sedimentation rate of these sinking particles. In many oceanic biogeographical provinces, it is blooms of diatoms that result in high rates of particle export; at BATS, diatoms and other large phytoplankton are relatively rare in the euphotic zone (based upon size-fractionation and pigment bio-markers; Glover et al. 1988; Steinberg et al. 2001) but are actively growing and sedimenting from the surface ocean (Brzezinski and Nelson 1995a; Brzezinski and Kosman 1996; Nelson and Brzezinski 1997; Krause, Nelson and Lomas, in prep.). Indeed, diatom populations at BATS contribute disproportionately to overall system productivity through short-lived episodic events (Nelson and Brzezinski 1997), a finding consistent with other research conducted in the North Atlantic subtropical gyre (Maranon et al. 2001). A recent analysis suggests that Haptophytes are also important in the partitioning of carbon between dissolved and particulate pools with anomalies in Haptophyte abundance, controlled to some extent by variability in the NAO, negatively related to particle export. The 18-years of BATS data allow us to examine how phytoplankton community structure impacts the flow of carbon in the surface ocean. A testable hypothesis is that increases in the relative abundances of diatoms at BATS should increase particle flux while increases in Haptophytes would decrease particle flux. Determining the complex interactions between the biological community and export production, for example, has added importance for understanding the potential changes in phytoplankton species succession and dominance (e.g., Tortell et al. 2002) and export production (e.g., Bopp et al. 2001) under climate change scenarios of changing ocean circulation and mixing.
Please see the BATS Web site (http://bats.bios.edu) for additional information.
ARMSTRONG, R., C. LEE, J. HEDGES, S. HONJO, and S. WAKEHAM. 2002. A new mechanistic model for organic carbon fluxes in the ocean based on the quantitative association of POC with ballast minerals. Deep Sea Research II 49: 219-236.
BATES, N. 2001a. Interannual variability of oceanic CO2 and biogeochemical properties in the Western North Atlantic subtropical gyre. Deep-Sea Research II 48: 1507-1528.
---. 2007. Interannual variability of the oceanic CO2 sink in the subtropical gyre of the North Atlantic Ocean over the last two decades. Journal of Geophysical Research: doi:10.1029/2006JC003759.
BATES, N. 2001b. Interannual variability of oceanic CO2 and biogeochemical properties in the Western North Atlantic subtropical gyre. Deep-Sea Research Part II 48: 1507-1528.
BATES, N., and D. HANSELL. 2004. Temporal variability of excess nitrate in the subtropical mode water of the North Atlantic Ocean. Marine Chemistry 84: 225-241.
BATES, N., A. MICHAELS, and A. KNAP. 1996a. Seasonal and interannual variability of the oceanic carbon dioxide system at the U.S. JGOFS Bermuda Atlantic Time-series Site. Deep Sea Research II 43: 347-383.
BATES, N., and A. PETERS. 2007. The contribution of acid deposition to ocean acidification in the subtropical North Atlantic Ocean. Marine Chemistry.
BATES, N. R., L. MERLIVAT, L. BEAUMONT, and A. C. PEQUIGNET. 2000. Intercomparison of shipboard and moored CARIOCA buoy seawater fCO(2) measurements in the Sargasso Sea. Marine Chemistry 72: 239-255.
BATES, N. R., A. F. MICHAELS, and A. H. KNAP. 1996b. Seasonal and interannual variability of oceanic carbon dioxide species at the US JGOFS Bermuda Atlantic time-series study (BATS) site (vol 43, pg 347, 1996). Deep-Sea Research Part Ii-Topical Studies in Oceanography 43: 1435-1435.
BATES, N. R., A. C. PEQUIGNET, R. J. JOHNSON, and N. GRUBER. 2002. A short-term sink for atmospheric CO2 in subtropical mode water of the North Atlantic Ocean. Nature 420: 489-493.
BATES, N. R., T. TAKAHASHI, D. W. CHIPMAN, and A. H. KNAP. 1998. Variability of pCO(2) on diel to seasonal timescales in the Sargasso Sea near Bermuda. Journal of Geophysical Research-Oceans 103: 15567-15585.
BIDIGARE, R. 1991. Analysis of algal chlorophylls and carotenoids, p. 119-123. In D. Hurd and D. Spencer [eds.], Marine Particles: Analysis and Characterization. American Geophysical Union.
BIDIGARE, R. R., L. VAN HEUKELEM, and C. TREES. 2005. Analysis of algal pigments by high-performance liquid chromatography, p. 327-346. In R. Anderson [ed.], Algal Culturing Techniques. Elsevier Press.
BOPP, L., P. MONFRAY, O. AUMONT, J. DUFRESNE, R. LE TREUT, G. MADEC, L. TERRAY, and J. ORR. 2001. Potential impact of climate change on marine export production. Global Biogeochemical Cycles 15: 81-99.
BRIX, H., N. GRUBER, D. KARL, and N. BATES. 2006. Interannual variability of the relationship between primary, net community and export production in the subtropical gyres. Deep-Sea Research II 53: 698-717.
BRZEZINSKI, M., and D. NELSON. 1995a. The annual silica cycle in the Sargasso Sea near Bermuda. Deep-Sea Research 42: 1215-1237.
BRZEZINSKI, M. A., and C. A. KOSMAN. 1996. Silica production in the Sargasso Sea during spring 1989. Marine Ecology Progress Series 142: 39-45.
BRZEZINSKI, M. A., and D. M. NELSON. 1995b. The Annual Silica Cycle in the Sargasso Sea near Bermuda. Deep-Sea Research Part I-Oceanographic Research Papers 42: 1215-1237.
CARLSON, C., H. DUCKLOW, and A. MICHAELS. 1994. Annual flux of dissolved organic carbon from the euphotic zone in the northwestern Sargasso Sea. Nature 371: 405-408.
CHAVEZ, F., J. P. RYAN, S. LLUCH-COTA, and M. NIQUEN. 2003. From anchovies to sardines and back: Multidecadal change in the Pacific Ocean. Science 299: 217-221.
COALE, K. H., K. S. JOHNSON, S. E. FITZWATER, R. M. GORDON, S. TANNER, F. P. CHAVEZ, L.
FERIOLI, C. SAKAMOTO, P. ROGERS, F. MILLERO, P. STEINBERG, P. NIGHTINGALE, D. COOPER, W. P. COCHLAN, M. R. LANDRY, J. CONSTANTINOU, G. ROLLWAGEN, A. TRASVINA, and R. KUDELA. 1996. A massive phytoplankton bloom induced by an ecosystem-scale iron fertilization experiment in the equatorial Pacific Ocean. Nature 383: 495-501.
CODISPOTI, L. 1989. Phosphorus vs. Nitrogen limitation of new and export production, p. 377-394. In W. Berger, V. Smetacek and G. Wefer [eds.], Productivity of the Ocean: Present and Past. John Wiley & Sons.
DORE, J., T. HOULIHAN, D. HEBEL, G. TIEN, L. TUPAS, and D. KARL. 1996. Freezing as a method of sample preservation for the analysis of dissolved inorganic nutrients in seawater. Marine Chemistry 53: 173-185.
DUCKLOW, H., D. KIRCHMAN, and H. QUINBY. 1992. Bacterioplankton cell growth and macromolecular synthesis in seawater cultures during the North Atlantic Bloom spring phytoplankton bloom, May 1989. Microbial Ecology 24: 125-144.
EPPLEY, R. W., and B. J. PETERSON. 1979. Particulate organic matter flux and planktonic new production in the deep ocean. Nature 282: 677-680.
FALKOWSKI, P. G., R. T. BARBER, and V. SMETACEK. 1998. Biogeochemical controls and feedbacks on ocean primary productivity. Science 281: 200-206.
FITZWATER, S., G. KNAUER, and J. MARTIN. 1982. Metal contamination and its effects on primary production measurements. Limnology and Oceanography 27: 544-551.
FUHRMAN, J. A., and F. AZAM. 1980. Bacterioplankton secondary production estimates for coastal waters of British Columbia, Antarctica and California. Applied and Environmental Microbiology 39: 1085-1095.
GLOVER, H., B. PREZELIN, L. CAMPBELL, and M. WYMAN. 1988. Pico- and ultraplankton Sargasso Sea communities: Variability and comparative distributions of Synechococcus spp. and algae. Marine Ecology Progress Series 49: 127-139.
GRUBER, N., C. D. KEELING, and N. R. BATES. 2002. Interannual variability in the North Atlantic Ocean carbon sink. Science 298: 2374-2378.
GRUBER, N., and J. SARMIENTO. 1997. Global patterns of marine nitrogen fixation and denitrification. Global Biogeochemical Cycles 11: 235-266.
HANSELL, D., and C. CARLSON. 2001. Biogeochemistry of total organic carbon and nitrogen in the Sargasso Sea: control by convective overturn. Deep-Sea Research II 48: 1649-1668.
HANSELL, D. A., N. BATES, and D. B. OLSON. 2004. Excess nitrate and nitrogen fixation in the North Atlantic Ocean. Marine Chemistry 84: 243-265.
HOOD, R. R., N. R. BATES, D. G. CAPONE, and D. B. OLSON. 2001. Modeling the effect of nitrogen fixation on carbon and nitrogen fluxes at BATS. Deep-Sea Research Part II 48: 1609-1648.
IPCC. 1990. Climate Change: The IPCC Scientific Assessment. Cambridge University Press.
---. 2001. Intergovernmental Panel on Climate Change (IPCC) Third Assessment Report. Cambridge University Press.
---. 2007. Climate Change 2007 - Impacts, Adaptation and Vulnerability. Working Group II contribution to the Fourth Assessment Report of the IPCC. Cambridge University Press.
JOHNSON, D. 1971. Simultaneous determination of arsenate and phosphate in natural waters. Environmental Science & Technology 5: 411-414.
JOHNSON, R. 2003. Climatic and mesoscale eddy modulation of the upper ocean at the Bermuda Time-series sites., p. 247, Southampton Oceanography Centre. Southampton University.
JOYCE, T., and L. TALLEY. 1996. The Bermuda Station S - a long-running oceanographic show: deeper waters show warming trend. Oceanus 39: 14-15.
KARL, D., R. BIDIGARE, and R. LETELIER. 2001a. Long-term changes in plankton community structure and productivity in the North Pacific Subtropical Gyre: the domain shift hypothesis. Deep-Sea Research II 48: 1449-1470.
KARL, D. M., J. DORE, R. LUKAS, A. F. MICHAELS, N. BATES, and A. H. KNAP. 2001b. Building the long-term picture: The U.S. JGOFS time-series programs. Oceanography 14: 6-17.
KARL, D. M., and G. TIEN. 1992. MAGIC: A sensitive and precise method for measuring dissolved phosphorus in aquatic environments. Limnology and Oceanography 37: 105-116.
KNAP, A., A. MICHAELS, R. DOW, R. JOHNSON, K. GUNDERSEN, J. SORENSEN, A. CLOSE, N. BATES, F. A. HOWSE, M. A. HAMMER, M. BEST, A. DOYLE, C. M. MICHAELS, D. HANSELL, T. Y. WATERHOUSE, R. KELLY, E. A. CAPORELLI, F. BAHR, and R. LITTLE. 1995. U.S. Joint Global Ocean Flux Study. Bermuda Atlantic Time-series Study. Data Report for BATS 49-60. U.S. JGOFS Planning Office, Woods Hole Oceanographic Institution.
KNAP, A., A. MICHAELS, R. DOW, R. JOHNSON, K. GUNDERSEN, J. SORENSEN, A. CLOSE, F. A. HOWSE, N. BATES, M. BEST, M. A. HAMMER, and A. DOYLE. 1994. U.S. Joint Global Ocean Flux Study. Bermuda Atlantic Time-series Study. Data Report for BATS 37-48. U.S. JGOFS Planning Office, Woods Hole Oceanographic Institution.
KNAP, A., A. MICHAELS, D. HANSELL, F. BAHR, N. BATES, S. BECKER, E. A. CAPORELLI, A. CLOSE, A. DOYLE, R. DOW, R. JOHNSON, R. KELLY, R. LITTLE, K. GUNDERSEN, F. A. HOWSE, and T. Y. WATERHOUSE. 1997a. U.S. Joint Global Ocean Flux Study. Bermuda Atlantic Time-series Study. Data Report for BATS 61-72. U.S. JGOFS Planning Office, Woods Hole Oceanographic Institution.
KNAP, A., A. MICHAELS, D. STEINBERG, F. BAHR, N. BATES, S. BELL, P. COUNTWAY, A. CLOSE, A. DOYLE, F. HOWSE, K. GUNDERSEN, R. JOHNSON, R. LITTLE, K. ORCUTT, R. PARSONS, C. RATHBUN, M. SANDERSON, and S. STONE. 1997b. BATS Methods Manual Version 4. U.S. JGOFS Planning Office.
KNAP, A. H., A. MICHAELS, R. DOW, R. JOHNSON, K. GUNDERSEN, G. A. KNAUER, S. E. LOHRENZ, V. A. ASPER, M. TUEL, H. DUCKLOW, H. L. QUINBY, and P. BREWER. 1991. U.S. Joint Global Ocean Flux Study. Bermuda Atlantic Time-series Study. Data Report for BATS 1-12. U.S. JGOFS Planning Office, Woods Hole Oceanographic Institution.
KNAP, A. H., A. MICHAELS, R. DOW, R. JOHNSON, K. GUNDERSEN, J. SORENSEN, A. CLOSE, M. A. HAMMER, G. A. KNAUER, S. E. LOHRENZ, V. A. ASPER, M. TUEL, H. DUCKLOW, H. L. QUINBY, P. BREWER, and R. BIDIGARE. 1992. U.S. Joint Global Ocean Flux Study. Bermuda Atlantic Time-series Study. Data Report for BATS 13-24. U.S. JGOFS Planning Office, Woods Hole Oceanographic Institution.
KNAP, A. H., A. MICHAELS, R. DOW, R. JOHNSON, K. GUNDERSEN, J. SORENSEN, A. CLOSE, F. A. HOWSE, M. A. HAMMER, N. BATES, G. A. KNAUER, S. E. LOHRENZ, V. A. ASPER, M. TUEL, H. DUCKLOW, and H. L. QUINBY. 1993. U.S. Joint Global Ocean Flux Study. Bermuda Atlantic Time-series Study. Data Report for BATS 25-36. U.S. JGOFS Planning Office, Woods Hole Oceanographic Institution.
KNAUER, G., J. MARTIN, and K. BRULAND. 1979. Fluxes of particulate carbon, nitrogen, and phosphorus in the upper water column of the northeast Pacific. Deep-Sea Research 26: 97-108.
KRAUSE, J., D. M. NELSON, and M. W. LOMAS. submitted. New and Export Production in the Subtropical Open Ocean Before Seasonal Stratification. IV. Biogenic silica production and export in response to late-winter storms. Deep Sea Research I.
LOHRENZ, S. E., G. A. KNAUER, V. L. ASPER, M. TUEL, A. F. MICHAELS, and A. H. KNAP. 1992. Seasonal Variability in Primary Production and Particle-Flux in the Northwestern Sargasso Sea - United-States Jgofs Bermuda Atlantic Time-Series Study. Deep-Sea Research Part a-Oceanographic Research Papers 39: 1373-1391.
LOMAS, M., N. BATES, A. KNAP, D. KARL, R. LUKAS, M. LANDRY, R. BIDIGARE, D. STEINBERG, and C. CARLSON. 2002. Refining our understanding of ocean biogeochemistry and ecosystem functioning. EOS 83: 559-561.
LOMAS, M. W., and N. R. BATES. 2004. Potential controls on interannual partitioning of organic carbon during the winter/spring phytoplankton bloom at the Bermuda Atlantic Time-series Study (BATS) site. Deep-Sea Research Part I 51: 1619-1636.
MARANON, E., P. HOLLIGAN, R. BARCIELA, N. GONZALEZ, B. MOURINO, M. PAZO, and M. VARELA. 2001. Patterns of phytoplankton size structure and productivity in contrasting open-ocean environments. Marine Ecology Progress Series 216: 43-56.
MARTIN, J., G. A. KNAUER, D. M. KARL, and W. BROENKOW. 1987. VERTEX: carbon cycling in the NE Pacific. Deep-Sea Research Part a-Oceanographic Research Papers 34: 267-285.
MCGILLICUDDY, D., and A. ROBINSON. 1997. Eddy-induced nutrient supply and new production in the Sargasso Sea. Deep-Sea Research II 44: 1427-1450.
MCGILLICUDDY, D., A. ROBINSON, D. SIEGEL, H. JANNASCH, R. JOHNSON, T. DICKEY, J. MCNEIL, A. MICHAELS, and A. KNAP. 1998a. Influence of mesoscale eddies on new production in the Sargasso Sea. Nature 394: 263-266.
MCGILLICUDDY, D. J., L. ANDERSON, N. R. BATES, T. BIBBY, K. O. BUESSELER, C. CARLSON, C. S. DAVIS, C. EWART, P. G. FALKOWSKI, S. A. GOLDTHWAIT, D. HANSELL, W. J. JENKINS, R. JOHNSON, V. K. KOSNYREV, J. LEDWELL, Q. LI, D. SIEGEL, and D. K. STEINBERG. 2007. Eddy/Wind interactions stimulate extraordinary mid-ocean plankton blooms. Science 316: 1021-1025.
MCGILLICUDDY, D. J., R. JOHNSON, D. A. SIEGEL, A. F. MICHAELS, N. R. BATES, and A. H. KNAP. 1999. Mesoscale variations of biogeochemical properties in the Sargasso Sea. Journal of Geophysical Research-Oceans 104: 13381-13394.
MCGILLICUDDY, D. J., and V. K. KOSNYREV. 2001. Dynamical interpolation of mesoscale flows in the TOPEX/poseidon diamond surrounding the US Joint Global Ocean Flux Study Bermuda Atlantic Time-Series Study site. Journal of Geophysical Research-Oceans 106: 16641-16656.
MCGILLICUDDY, D. J., A. R. ROBINSON, D. A. SIEGEL, H. W. JANNASCH, R. JOHNSON, T. D. DICKEY, J. MCNEIL, A. F. MICHEALS, and A. H. KNAP. 1998b. Influence of mesoscale eddies on new production in the Sargasso sea. Nature 394: 283-285.
MICHAELS, A., D. KARL, and D. CAPONE. 2001. Element stoichiometry, new production and nitrogen fixation. Oceanography 14: 68-77.
MICHAELS, A., A. KNAP, R. DOW, J. GUNDERSEN, R. JOHNSON, J. SORENSEN, A. CLOSE, G. KNAUER, S. LOHRENZ, V. ASPER, M. TUEL, and R. BIDIGARE. 1994. Seasonal patterns of ocean biogeochemistry at the U.S. JGOFS Bermuda Atlantic Time-series study site. Deep-Sea Research 41: 1013-1038.
MICHAELS, A. F., and A. H. KNAP. 1996. Overview of the US JGOFS Bermuda Atlantic Time-series Study and the Hydrostation S program. Deep-Sea Research Part II 43: 157-198.
MICHAELS, A. F., D. OLSON, J. L. SARMIENTO, J. W. AMMERMAN, K. FANNING, R. JAHNKE, A. H. KNAP, F. LIPSCHULTZ, and J. M. PROSPERO. 1996. Inputs, losses and transformations of nitrogen and phosphorus in the pelagic North Atlantic Ocean. Biogeochemistry 35: 181-226.
NELSON, D., and M. BRZEZINSKI. 1997. Diatom growth and productivity in an oligotrophic midocean gyre: a 3-yr record from the Sargasso Sea near Bermuda. Limnology and Oceanography 43: 473-486.
ORCUTT, K. M., F. LIPSCHULTZ, K. GUNDERSEN, R. ARIMOTO, A. F. MICHAELS, A. H. KNAP, and J. R. GALLON. 2001. A seasonal study of the significance of N-2 fixation by Trichodesmium spp. at the Bermuda Atlantic Time-series Study (BATS) site. Deep-Sea Research Part Ii-Topical Studies in Oceanography 48: 1583-1608.
OSCHLIES, A. 2001. NAO-induced long-term changes in nutrient supply to the surface waters of the North Atlantic. Geophysical Research Letters 28: 1751-1754.
SIEGEL, D. A., T. K. WESTBERRY, M. C. O'BRIEN, N. B. NELSON, A. F. MICHAELS, J. R. MORRISON, A. SCOTT, E. A. CAPORELLI, J. C. SORENSEN, S. MARITORENA, S. A. GARVER, E. A. BRODY, J. UBANTE, and M. A. HAMMER. 2001. Bio-optical modeling of primary production on regional scales: the Bermuda BioOptics project. Deep-Sea Research Part II 48: 1865-1896.
SMITH, D., and F. AZAM. 1992. A simple, economical method for measuring bacterial protein synthesis rates in seawater using super(3)H-leucine. Marine Microbial Food Webs 6: 107-114.
STEINBERG, D. K., C. A. CARLSON, N. R. BATES, S. A. GOLDTHWAIT, L. P. MADIN, and A. F. MICHAELS. 2000. Zooplankton vertical migration and the active transport of dissolved organic and inorganic carbon in the Sargasso Sea. Deep-Sea Research I 47: 137-158.
STEINBERG, D. K., C. A. CARLSON, N. R. BATES, R. J. JOHNSON, A. F. MICHAELS, and A. H. KNAP. 2001. Overview of the US JGOFS Bermuda Atlantic Time-series Study (BATS): a decade-scale look at ocean biology and biogeochemistry. Deep-Sea Research Part II 48: 1405-1447.
SWEENEY, E. N., D. J. MCGILLICUDDY, and K. O. BUESSELER. 2003. Biogeochemical impacts due to mesoscale eddy activity in the Sargasso Sea as measured at the Bermuda Atlantic Time-series Study (BATS). Deep-Sea Research II 50: 3017-3039.
TORTELL, P., G. DITULLIO, D. SIGMAN, and F. MOREL. 2002. CO2 effects on taxomonic composition and nutrient utilization in an Equatorial Pacific phytoplankton assemblage. Marine Ecology Progress Series 236: 37-43.
TYRRELL, T. 1999. The relative influence of nitrogen and phosphorus on oceanic primary production. Nature 400: 525-527.
WRIGHT, S., S. JEFFREY, F. MANTOURA, C. LLEWELLYN, T. BJORNLAND, D. REPETA, and N. A. WELSCHMEYER. 1991. Improved HPLC method for the analysis of chlorophylls and carotenoids from marine phytoplankton. Marine Ecology Progress Series 77: 183-196.
ZEHR, J., J. WATERBURY, P. TURNER, J. MONTOYA, E. OMOREGIE, G. STEWARD, A. HANSEN, and D. KARL. 2001. Unicellular cyanobacteria fix N2 in the subtropical North Pacific ocean. Nature 412: 635-638.
Additional Project Information