Ice melt influence on summertime net community production along the Western Antarctic Peninsula

The Western Antarctic Peninsula (WAP) is a highly productive marine environment that is undergoing rapid change, with consequences for productivity and total ecosystem carbon cycling. We present continuous underway O2/Ar estimates of net community production (NCPO2Ar) in austral summer 2012, 2013 and 2014 at sub-kilometer horizontal resolution within the Palmer Long-Term Ecological Research (Pal-LTER) grid region of the WAP. Substantial spatial variability is observed with NCPO2Ar ranging from 0 to 790 mmol O2 m−2 d−1 and considerable interannual variability with mean values in the grid region of 54.4±48.5, 44.6±40.5, and 85.6±75.9 mmol O2 m−2 d−1 in 2012, 2013 and 2014 respectively. Based on a strong correlation (r2=0.83) between residence time integrated NCPO2Ar and NCPDIC derived from seasonal DIC drawdown, we find the observed NCPO2Ar spatial and interannual variability to be consistent with the December–January NCPDIC magnitude. Seeking to explain the mechanistic drivers of NCP in the WAP, we observe a linear relationship between NCPO2Ar and meteoric water content derived from δ18O and salinity. This correlation may be due to Fe supply from glacial melt and/or strengthening of stratification and relief of light limitation. Elevated surface Fe availability, as indicated by Fv/Fm and measurements of surface water dissolved Fe and Mn (a rough proxy for recent potential Fe availability), and shallower, more stable mixed layers are present where meteoric water and/or sea ice melt is high near the coast. Light limitation is evident in the WAP when mixed layer depths are greater than ~40 m. Additionally we document hotspots of NCP associated with submarine canyons along the WAP. While it is difficult to predict how the physical-biological system might evolve under changing climatic conditions, it is evident that NCP, and potentially carbon flux out of the mixed layer, along the WAP will be sensitive to shifts in meltwater input and timing.

[1]  P. Boyd,et al.  The biogeochemical cycle of iron in the ocean , 2010 .

[2]  C. Nevison,et al.  Correcting oceanic O2/Ar‐net community production estimates for vertical mixing using N2O observations , 2014 .

[3]  S. Stammerjohn,et al.  Effect of continental shelf canyons on phytoplankton biomass and community composition along the western Antarctic Peninsula , 2015 .

[4]  Dennis A. Hansell,et al.  Effect of nutrient amendments on bacterioplankton production, community structure, and DOC utilization in the northwestern Sargasso Sea , 2002, Aquatic Microbial Ecology.

[5]  R. Wanninkhof,et al.  Evaluating gas transfer velocity parameterizations using upper ocean radon distributions , 2011 .

[6]  J. Tison,et al.  Iron study during a time series in the western Weddell pack ice , 2008 .

[7]  S. Stammerjohn,et al.  Recent Changes in Phytoplankton Communities Associated with Rapid Regional Climate Change Along the Western Antarctic Peninsula , 2009, Science.

[8]  M. Ardelan,et al.  Natural iron enrichment around the Antarctic Peninsula in the Southern Ocean , 2009 .

[9]  Maria Vernet,et al.  Marine pelagic ecosystems: the West Antarctic Peninsula , 2007, Philosophical Transactions of the Royal Society B: Biological Sciences.

[10]  J. Kohut,et al.  Adélie Penguin Foraging Location Predicted by Tidal Regime Switching , 2013, PloS one.

[11]  K. Baker,et al.  Seasonal and interannual variability of phytoplankton biomass west of the Antarctic Peninsula , 1998 .

[12]  D. Steinberg,et al.  Microzooplankton community composition along the Western Antarctic Peninsula , 2013 .

[13]  P. Tortell,et al.  Biological and physical controls on N2, O2, and CO2 distributions in contrasting Southern Ocean surface waters , 2015 .

[14]  Meng Zhou,et al.  The influence of shelf processes in delivering dissolved iron to the HNLC waters of the Drake Passage, Antarctica , 2013 .

[15]  Andrew J. Watson,et al.  A mesoscale phytoplankton bloom in the polar Southern Ocean stimulated by iron fertilization , 2000, Nature.

[16]  S. Stammerjohn,et al.  Penguin biogeography along the West Antarctic Peninsula : testing the canyon hypothesis with Palmer LTER observations , 2013 .

[17]  K. Arrigo,et al.  Estimates of net community production in the Southern Ocean determined from time series observations (2002–2011) of nutrients, dissolved inorganic carbon, and surface ocean pCO2 in Drake Passage , 2015 .

[18]  R. Wanninkhof Relationship between wind speed and gas exchange over the ocean , 1992 .

[19]  P. Tréguer,et al.  On iron limitation of the Southern Ocean : experimental observations in the Weddell and Scotia Seas. , 1990 .

[20]  S. Emerson,et al.  The solubility of neon, nitrogen and argon in distilled water and seawater , 2004 .

[21]  S. Stammerjohn,et al.  Dynamics of dissolved iron and other bioactive trace metals (Mn, Ni, Cu, Zn) in the Amundsen Sea Polynya, Antarctica , 2015 .

[22]  S. Fitzwater,et al.  Iron in Antarctic waters , 1990, Nature.

[23]  B. Mitchell,et al.  Observations of modeling of the Antartic phytoplankton crop in relation to mixing depth , 1991 .

[24]  H. Ducklow,et al.  The Freshwater System West of the Antarctic Peninsula: Spatial and Temporal Changes , 2013 .

[25]  H. Ducklow,et al.  Interannual variability in net community production at the Western Antarctic Peninsula region (1997–2014) , 2016 .

[26]  S. Stammerjohn,et al.  Western Antarctic Peninsula physical oceanography and spatio-temporal variability , 2008 .

[27]  B. Tilbrook,et al.  Continuous high-frequency dissolved O2/Ar measurements by equilibrator inlet mass spectrometry. , 2009, Analytical chemistry.

[28]  C. Hassler,et al.  Physiological characteristics of open ocean and coastal phytoplankton communities of Western Antarctic Peninsula and Drake Passage waters , 2015 .

[29]  S. Doney,et al.  Evaluation of the Southern Ocean O2/Ar‐based NCP estimates in a model framework , 2013 .

[30]  P. Quay,et al.  Evidence of O2 consumption in underway seawater lines: Implications for air‐sea O2 and CO2 fluxes , 2010 .

[31]  R. Sherrell,et al.  Automated on-line flow-injection ICP-MS determination of trace metals (Mn, Fe, Co, Ni, Cu and Zn) in open ocean seawater: Application to the GEOTRACES program , 2013 .

[32]  R. Sherrell,et al.  Sampling for particulate trace element determination using water sampling bottles: methodology and comparison to in situ pumps , 2012 .

[33]  S. Stammerjohn,et al.  Sea ice in the western Antarctic Peninsula region : Spatio-temporal variability from ecological and climate change perspectives , 2008 .

[34]  S. Stammerjohn,et al.  Winter and spring controls on the summer food web of the coastal West Antarctic Peninsula , 2014, Nature Communications.

[35]  R. C. Baker,et al.  Fluorometric Techniques For The Measurement Of Oceanic Chlorophyll In The Support Of Remote Sensing Author , 1981 .

[36]  O. Schofield,et al.  Summertime grazing impact of the dominant macrozooplankton off the Western Antarctic Peninsula , 2012 .

[37]  P. Sedwick,et al.  Regulation of algal blooms in Antarctic Shelf Waters by the release of iron from melting sea ice , 1997 .

[38]  A. Dickson Thermodynamics of the dissociation of boric acid in synthetic seawater from 273.15 to 318.15 K , 1990 .

[39]  S. Stammerjohn,et al.  Multiscale control of bacterial production by phytoplankton dynamics and sea ice along the western Antarctic Peninsula: A regional and decadal investigation , 2012 .

[40]  Oscar Schofield,et al.  West Antarctic Peninsula: An Ice-Dependent Coastal Marine Ecosystem in Transition , 2013 .

[41]  E. Hazen,et al.  Super-Aggregations of Krill and Humpback Whales in Wilhelmina Bay, Antarctic Peninsula , 2011, PloS one.

[42]  M. DeGrandpre,et al.  Dissolved O2/Ar and other methods reveal rapid changes in productivity during a Lagrangian experiment in the Southern Ocean , 2012 .

[43]  Shigenobu Takeda,et al.  Influence of iron availability on nutrient consumption ratio of diatoms in oceanic waters , 1998, Nature.

[44]  Louis I. Gordon,et al.  Oxygen solubility in seawater : better fitting equations , 1992 .

[45]  S. Stammerjohn,et al.  Long-term (1993-2013) changes in macrozooplankton off the Western Antarctic Peninsula , 2015 .

[46]  B. Tilbrook,et al.  The influence of iron and light on net community production in the Subantarctic and Polar Frontal Zones , 2010 .

[47]  M. Vernet,et al.  Interannual Variability in the Distribution of the Phytoplankton Standing Stock across the Seasonal Sea-Ice Zone West of the Antarctic Peninsula , 2005 .

[48]  R. Anadón,et al.  Vertical biogenic particle flux during Austral summer in the Antarctic Peninsula area , 2002 .

[49]  M. Timmermans,et al.  Physical and biological controls on oxygen saturation variability in the upper Arctic Ocean , 2014 .

[50]  C. D. Keeling,et al.  Ocean pCO2 calculated from dissolved inorganic carbon, alkalinity, and equations for K1 and K2: validation based on laboratory measurements of CO2 in gas and seawater at equilibrium , 2000 .

[51]  S. Stammerjohn,et al.  Primary production within the sea-ice zone west of the Antarctic Peninsula: I—Sea ice, summer mixed layer, and irradiance , 2008 .

[52]  David G. Vaughan,et al.  Recent Trends in Melting Conditions on the Antarctic Peninsula and Their Implications for Ice-sheet Mass Balance and Sea Level , 2006 .

[53]  Seelye Martin,et al.  A laboratory study of dissolved noble gas anomaly due to ice formation , 1988 .

[54]  P. Statham,et al.  Ice sheets as a significant source of highly reactive nanoparticulate iron to the oceans , 2014, Nature Communications.

[55]  B. Mitchell,et al.  Light limitation of phytoplankton biomass and macronutrient utilization in the Southern Ocean , 1991 .

[56]  P. Falkowski,et al.  New estimates of Southern Ocean biological production rates from O2/Ar ratios and the triple isotope composition of O2 , 2007 .

[57]  Dennis A. Hansell,et al.  Biogeochemical regimes, net community production and carbon export in the Ross Sea, Antarctica , 2000, Deep Sea Research Part II: Topical Studies in Oceanography.

[58]  Ulf Riebesell,et al.  Synthesis of iron fertilization experiments: From the iron age in the age of enlightenment , 2005 .

[59]  H. Matsueda,et al.  Net community production in the marginal ice zone and its importance for the variability of the oceanic pCO2 in the Southern Ocean south of Australia , 2002 .

[60]  B. Prézelin,et al.  The linkage between Upper Circumpolar Deep Water (UCDW) and phytoplankton assemblages on the west Antarctic Peninsula continental shelf , 2000 .

[61]  C. J. Carrillo,et al.  Processes regulating oxygen and carbon dioxide in surface waters west of the Antarctic Peninsula , 2004 .

[62]  Dennis A. Hansell,et al.  Net community production of dissolved organic carbon , 1998 .

[63]  R. Geider,et al.  Interpretation of fast repetition rate (FRR) fluorescence: signatures of phytoplankton community structure versus physiological state , 2009 .

[64]  E. Hazen,et al.  Austral fall! winter transition of mesozooplankton assemblages and krill aggregations in an embayment west of the Antarctic Peninsula , 2012 .

[65]  S. Stammerjohn,et al.  Changing distributions of sea ice melt and meteoric water west of the Antarctic Peninsula , 2017 .

[66]  Brian M. Hopkinson,et al.  Iron limitation across chlorophyll gradients in the southern Drake Passage: Phytoplankton responses to iron addition and photosynthetic indicators of iron stress , 2007 .

[67]  M. Vernet,et al.  Glacial meltwater dynamics in coastal waters west of the Antarctic peninsula , 2002, Proceedings of the National Academy of Sciences of the United States of America.

[68]  P. Falkowski,et al.  Measuring photosynthetic parameters in individual algal cells by Fast Repetition Rate fluorometry , 1999, Photosynthesis Research.

[69]  S. Emerson,et al.  Biological productivity along Line P in the subarctic northeast Pacific: In situ versus incubation‐based methods , 2012 .

[70]  E. Laws,et al.  Photosynthetic quotients, new production and net community production in the open ocean , 1991 .

[71]  P. Sedwick,et al.  Estimating the benthic efflux of dissolved iron on the Ross Sea continental shelf , 2014 .

[72]  Maria Vernet,et al.  Export production and its regulating factors in the West Antarctica Peninsula region of the Southern Ocean , 2012 .

[73]  B. Tilbrook,et al.  The Southern Ocean Biological Response to Aeolian Iron Deposition , 2007, Science.

[74]  B. Mitchell,et al.  Seasonal and interannual variability of particulate organic carbon within the Southern Ocean from satellite ocean color observations , 2010 .

[75]  S. Epstein,et al.  Variation of O18 content of waters from natural sources , 1953 .

[76]  S. Doney,et al.  Two decades of inorganic carbon dynamics along the West Antarctic Peninsula , 2015 .

[77]  D. Karl RACER: Research on antarctic coastal ecosystem rates , 1991 .

[78]  M. Meredith,et al.  Wintertime controls on summer stratification and productivity at the western Antarctic Peninsula , 2013 .

[79]  C. Sweeney,et al.  Biological and physical controls on O 2 /Ar, Ar and p CO 2 variability at the Western Antarctic Peninsula and in the Drake Passage , 2017 .