Articles | Volume 15, issue 18
https://doi.org/10.5194/bg-15-5503-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-15-5503-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
First in situ estimations of small phytoplankton carbon and nitrogen uptake rates in the Kara, Laptev, and East Siberian seas
P. Sadanandan Bhavya
Department of Oceanography, Pusan National University,
Busan 609-735, Korea
Jang Han Lee
Department of Oceanography, Pusan National University,
Busan 609-735, Korea
Ho Won Lee
Department of Oceanography, Pusan National University,
Busan 609-735, Korea
Jae Joong Kang
Department of Oceanography, Pusan National University,
Busan 609-735, Korea
Jae Hyung Lee
Department of Oceanography, Pusan National University,
Busan 609-735, Korea
Dabin Lee
Department of Oceanography, Pusan National University,
Busan 609-735, Korea
So Hyun An
Department of Oceanography, Pusan National University,
Busan 609-735, Korea
Dean A. Stockwell
Institute of Marine Science, University of Alaska, Fairbanks, AK
99775, USA
Terry E. Whitledge
Institute of Marine Science, University of Alaska, Fairbanks, AK
99775, USA
Sang Heon Lee
CORRESPONDING AUTHOR
Department of Oceanography, Pusan National University,
Busan 609-735, Korea
Related authors
No articles found.
Sang H. Lee, Bo Kyung Kim, Yu Jeong Lim, HuiTae Joo, Jae Joong Kang, Dabin Lee, Jisoo Park, Sun-Yong Ha, and Sang Hoon Lee
Biogeosciences, 14, 3705–3713, https://doi.org/10.5194/bg-14-3705-2017, https://doi.org/10.5194/bg-14-3705-2017, 2017
Short summary
Short summary
Little information on the contribution of small-sized phytoplankton is currently available in the Amundsen Sea. Based on a strong negative correlation between the contributions of small phytoplankton and the total daily primary production of phytoplankton found in this study, we concluded that a potential decrease in total primary production would be led by increasing contribution of small phytoplankton in the Amundsen Sea under rapidly warming environmental conditions.
Sang Heon Lee, Jang Han Lee, Howon Lee, Jae Joong Kang, Jae Hyung Lee, Dabin Lee, SoHyun An, Dean A. Stockwell, and Terry E. Whitledge
Biogeosciences Discuss., https://doi.org/10.5194/bg-2017-234, https://doi.org/10.5194/bg-2017-234, 2017
Manuscript not accepted for further review
Short summary
Short summary
The Laptev and East Siberian seas are highly dynamic in terms of active processing of organic matters impacting the transport to the deep Arctic Ocean. However, they have been the least biologically studied region in the Arctic Ocean. As a part of the NABOS program, our field-measured data, which are very scarce in this region, such as major inorganic nutrient and chl-a concentrations and carbon and nitrogen uptake rates of phytoplankton in this study will be very valuable for basic ground.
Jang Han Lee, Dabin Lee, Jae Joong Kang, Hui Tae Joo, Jae Hyung Lee, Ho Won Lee, So Hyun Ahn, Chang Keun Kang, and Sang Heon Lee
Biogeosciences, 14, 1903–1917, https://doi.org/10.5194/bg-14-1903-2017, https://doi.org/10.5194/bg-14-1903-2017, 2017
Short summary
Short summary
Based on the seasonal biochemical compositions in this study, the calorific contents of the food material were 1.0–6.1 Kcal m−3. We found that a major governing factor in the biochemical composition of POM was dissolved inorganic nitrogen loading from river input. The relatively larger amount of food material and the higher calorific content of the POM found in this study reflected good nutritive conditions for sustaining productive shellfish and fish populations in Gwangyang Bay, South Korea.
M. S. Yun, T. E. Whitledge, D. Stockwell, S. H. Son, J. H. Lee, J. W. Park, D. B. Lee, J. Park, and S. H. Lee
Biogeosciences, 13, 737–749, https://doi.org/10.5194/bg-13-737-2016, https://doi.org/10.5194/bg-13-737-2016, 2016
Related subject area
Biogeochemistry: Coastal Ocean
Production and accumulation of reef framework by calcifying corals and macroalgae on a remote Indian Ocean cay
Zooplankton community succession and trophic links during a mesocosm experiment in the coastal upwelling off Callao Bay (Peru)
Temporal and spatial evolution of bottom-water hypoxia in the St Lawrence estuarine system
Significant nutrient consumption in the dark subsurface layer during a diatom bloom: a case study on Funka Bay, Hokkaido, Japan
Contrasts in dissolved, particulate, and sedimentary organic carbon from the Kolyma River to the East Siberian Shelf
Sediment quality assessment in an industrialized Greek coastal marine area (western Saronikos Gulf)
Limits and CO2 equilibration of near-coast alkalinity enhancement
Role of phosphorus in the seasonal deoxygenation of the East China Sea shelf
Interannual variability of the initiation of the phytoplankton growing period in two French coastal ecosystems
Spatio-temporal distribution, photoreactivity and environmental control of dissolved organic matter in the sea-surface microlayer of the eastern marginal seas of China
Metabolic alkalinity release from large port facilities (Hamburg, Germany) and impact on coastal carbon storage
A Numerical reassessment of the Gulf of Mexico carbon system in connection with the Mississippi River and global ocean
Observed and projected global warming pressure on coastal hypoxia
Benthic alkalinity fluxes from coastal sediments of the Baltic and North seas: comparing approaches and identifying knowledge gaps
Investigating the effect of nickel concentration on phytoplankton growth to assess potential side-effects of ocean alkalinity enhancement
Unprecedented summer hypoxia in southern Cape Cod Bay: an ecological response to regional climate change?
Interannual variabilities, long-term trends, and regulating factors of low-oxygen conditions in the coastal waters off Hong Kong
Causes of the extensive hypoxia in the Gulf of Riga in 2018
Trawling effects on biogeochemical processes are mediated by fauna in high-energy biogenic-reef-inhabited coastal sediments
Drought recorded by Ba∕Ca in coastal benthic foraminifera
A nitrate budget of the Bohai Sea based on an isotope mass balance model
Suspended particulate matter drives the spatial segregation of nitrogen turnover along the hyper-turbid Ems estuary
Marine CO2 system variability along the northeast Pacific Inside Passage determined from an Alaskan ferry
Reviews and syntheses: Spatial and temporal patterns in seagrass metabolic fluxes
Mixed layer depth dominates over upwelling in regulating the seasonality of ecosystem functioning in the Peruvian upwelling system
Temporal dynamics of surface ocean carbonate chemistry in response to natural and simulated upwelling events during the 2017 coastal El Niño near Callao, Peru
Pelagic primary production in the coastal Mediterranean Sea: variability, trends, and contribution to basin-scale budgets
Contrasting patterns of carbon cycling and dissolved organic matter processing in two phytoplankton–bacteria communities
Biophysical controls on seasonal changes in the structure, growth, and grazing of the size-fractionated phytoplankton community in the northern South China Sea
Seasonal dispersal of fjord meltwaters as an important source of iron and manganese to coastal Antarctic phytoplankton
Modeling cyanobacteria life cycle dynamics and historical nitrogen fixation in the Baltic Proper
Simultaneous assessment of oxygen- and nitrate-based net community production in a temperate shelf sea from a single ocean glider
Reviews and syntheses: Physical and biogeochemical processes associated with upwelling in the Indian Ocean
Particulate organic carbon dynamics in the Gulf of Lion shelf (NW Mediterranean) using a coupled hydrodynamic–biogeochemical model
Technical note: Novel triple O2 sensor aquatic eddy covariance instrument with improved time shift correction reveals central role of microphytobenthos for carbon cycling in coral reef sands
Long-term spatiotemporal variations in and expansion of low-oxygen conditions in the Pearl River estuary: a study synthesizing observations during 1976–2017
Fe-binding organic ligands in coastal and frontal regions of the western Antarctic Peninsula
Temporal variability and driving factors of the carbonate system in the Aransas Ship Channel, TX, USA: a time series study
Nitrogen loss processes in response to upwelling in a Peruvian coastal setting dominated by denitrification – a mesocosm approach
Retracing hypoxia in Eckernförde Bight (Baltic Sea)
The impact of the freeze–melt cycle of land-fast ice on the distribution of dissolved organic matter in the Laptev and East Siberian seas (Siberian Arctic)
The fate of upwelled nitrate off Peru shaped by submesoscale filaments and fronts
Coastal processes modify projections of some climate-driven stressors in the California Current System
Upwelling-induced trace gas dynamics in the Baltic Sea inferred from 8 years of autonomous measurements on a ship of opportunity
Destruction and reinstatement of coastal hypoxia in the South China Sea off the Pearl River estuary
Hypersaline tidal flats as important “blue carbon” systems: a case study from three ecosystems
Drivers and impact of the seasonal variability of the organic carbon offshore transport in the Canary upwelling system
Organic carbon densities and accumulation rates in surface sediments of the North Sea and Skagerrak
An observation-based evaluation and ranking of historical Earth system model simulations in the northwest North Atlantic Ocean
Characterizing the origins of dissolved organic carbon in coastal seawater using stable carbon isotope and light absorption characteristics
M. James McLaughlin, Cindy Bessey, Gary A. Kendrick, John Keesing, and Ylva S. Olsen
Biogeosciences, 20, 1011–1026, https://doi.org/10.5194/bg-20-1011-2023, https://doi.org/10.5194/bg-20-1011-2023, 2023
Short summary
Short summary
Coral reefs face increasing pressures from environmental change at present. The coral reef framework is produced by corals and calcifying algae. The Kimberley region of Western Australia has escaped land-based anthropogenic impacts. Specimens of the dominant coral and algae were collected from Browse Island's reef platform and incubated in mesocosms to measure calcification and production patterns of oxygen. This study provides important data on reef building and climate-driven effects.
Patricia Ayón Dejo, Elda Luz Pinedo Arteaga, Anna Schukat, Jan Taucher, Rainer Kiko, Helena Hauss, Sabrina Dorschner, Wilhelm Hagen, Mariona Segura-Noguera, and Silke Lischka
Biogeosciences, 20, 945–969, https://doi.org/10.5194/bg-20-945-2023, https://doi.org/10.5194/bg-20-945-2023, 2023
Short summary
Short summary
Ocean upwelling regions are highly productive. With ocean warming, severe changes in upwelling frequency and/or intensity and expansion of accompanying oxygen minimum zones are projected. In a field experiment off Peru, we investigated how different upwelling intensities affect the pelagic food web and found failed reproduction of dominant zooplankton. The changes projected could severely impact the reproductive success of zooplankton communities and the pelagic food web in upwelling regions.
Mathilde Jutras, Alfonso Mucci, Gwenaëlle Chaillou, William A. Nesbitt, and Douglas W. R. Wallace
Biogeosciences, 20, 839–849, https://doi.org/10.5194/bg-20-839-2023, https://doi.org/10.5194/bg-20-839-2023, 2023
Short summary
Short summary
The deep waters of the lower St Lawrence Estuary and gulf have, in the last decades, experienced a strong decline in their oxygen concentration. Below 65 µmol L-1, the waters are said to be hypoxic, with dire consequences for marine life. We show that the extent of the hypoxic zone shows a seven-fold increase in the last 20 years, reaching 9400 km2 in 2021. After a stable period at ~ 65 µmol L⁻¹ from 1984 to 2019, the oxygen level also suddenly decreased to ~ 35 µmol L-1 in 2020.
Sachi Umezawa, Manami Tozawa, Yuichi Nosaka, Daiki Nomura, Hiroji Onishi, Hiroto Abe, Tetsuya Takatsu, and Atsushi Ooki
Biogeosciences, 20, 421–438, https://doi.org/10.5194/bg-20-421-2023, https://doi.org/10.5194/bg-20-421-2023, 2023
Short summary
Short summary
We conducted repetitive observations in Funka Bay, Japan, during the spring bloom 2019. We found nutrient concentration decreases in the dark subsurface layer during the bloom. Incubation experiments confirmed that diatoms could consume nutrients at a substantial rate, even in darkness. We concluded that the nutrient reduction was mainly caused by nutrient consumption by diatoms in the dark.
Dirk Jong, Lisa Bröder, Tommaso Tesi, Kirsi H. Keskitalo, Nikita Zimov, Anna Davydova, Philip Pika, Negar Haghipour, Timothy I. Eglinton, and Jorien E. Vonk
Biogeosciences, 20, 271–294, https://doi.org/10.5194/bg-20-271-2023, https://doi.org/10.5194/bg-20-271-2023, 2023
Short summary
Short summary
With this study, we want to highlight the importance of studying both land and ocean together, and water and sediment together, as these systems function as a continuum, and determine how organic carbon derived from permafrost is broken down and its effect on global warming. Although on the one hand it appears that organic carbon is removed from sediments along the pathway of transport from river to ocean, it also appears to remain relatively ‘fresh’, despite this removal and its very old age.
Georgia Filippi, Manos Dassenakis, Vasiliki Paraskevopoulou, and Konstantinos Lazogiannis
Biogeosciences, 20, 163–189, https://doi.org/10.5194/bg-20-163-2023, https://doi.org/10.5194/bg-20-163-2023, 2023
Short summary
Short summary
The pollution of the western Saronikos Gulf from heavy metals has been examined through the study of marine sediment cores. It is a deep gulf (maximum depth 440 m) near Athens affected by industrial and volcanic activity. Eight cores were received from various stations and depths and analysed for their heavy metal content and geochemical characteristics. The results were evaluated by using statistical methods, environmental indicators and comparisons with old data.
Jing He and Michael D. Tyka
Biogeosciences, 20, 27–43, https://doi.org/10.5194/bg-20-27-2023, https://doi.org/10.5194/bg-20-27-2023, 2023
Short summary
Short summary
Recently, ocean alkalinity enhancement (OAE) has gained interest as a scalable way to address the urgent need for negative CO2 emissions. In this paper we examine the capacity of different coastlines to tolerate alkalinity enhancement and the time scale of CO2 uptake following the addition of a given quantity of alkalinity. The results suggest that OAE has significant potential and identify specific favorable and unfavorable coastlines for its deployment.
Arnaud Laurent, Haiyan Zhang, and Katja Fennel
Biogeosciences, 19, 5893–5910, https://doi.org/10.5194/bg-19-5893-2022, https://doi.org/10.5194/bg-19-5893-2022, 2022
Short summary
Short summary
The Changjiang is the main terrestrial source of nutrients to the East China Sea (ECS). Nutrient delivery to the ECS has been increasing since the 1960s, resulting in low oxygen (hypoxia) during phytoplankton decomposition in summer. River phosphorus (P) has increased less than nitrogen, and therefore, despite the large nutrient delivery, phytoplankton growth can be limited by the lack of P. Here, we investigate this link between P limitation, phytoplankton production/decomposition, and hypoxia.
Coline Poppeschi, Guillaume Charria, Anne Daniel, Romaric Verney, Peggy Rimmelin-Maury, Michaël Retho, Eric Goberville, Emilie Grossteffan, and Martin Plus
Biogeosciences, 19, 5667–5687, https://doi.org/10.5194/bg-19-5667-2022, https://doi.org/10.5194/bg-19-5667-2022, 2022
Short summary
Short summary
This paper aims to understand interannual changes in the initiation of the phytoplankton growing period (IPGP) in the current context of global climate changes over the last 20 years. An important variability in the timing of the IPGP is observed with a trend towards a later IPGP during this last decade. The role and the impact of extreme events (cold spells, floods, and wind burst) on the IPGP is also detailed.
Lin Yang, Jing Zhang, Anja Engel, and Gui-Peng Yang
Biogeosciences, 19, 5251–5268, https://doi.org/10.5194/bg-19-5251-2022, https://doi.org/10.5194/bg-19-5251-2022, 2022
Short summary
Short summary
Enrichment factors of dissolved organic matter (DOM) in the eastern marginal seas of China exhibited a significant spatio-temporal variation. Photochemical and enrichment processes co-regulated DOM enrichment in the sea-surface microlayer (SML). Autochthonous DOM was more frequently enriched in the SML than terrestrial DOM. DOM in the sub-surface water exhibited higher aromaticity than that in the SML.
Mona Norbisrath, Johannes Pätsch, Kirstin Dähnke, Tina Sanders, Gesa Schulz, Justus E. E. van Beusekom, and Helmuth Thomas
Biogeosciences, 19, 5151–5165, https://doi.org/10.5194/bg-19-5151-2022, https://doi.org/10.5194/bg-19-5151-2022, 2022
Short summary
Short summary
Total alkalinity (TA) regulates the oceanic storage capacity of atmospheric CO2. TA is also metabolically generated in estuaries and influences coastal carbon storage through its inflows. We used water samples and identified the Hamburg port area as the one with highest TA generation. Of the overall riverine TA load, 14 % is generated within the estuary. Using a biogeochemical model, we estimated potential effects on the coastal carbon storage under possible anthropogenic and climate changes.
Le Zhang and Z. George Xue
Biogeosciences, 19, 4589–4618, https://doi.org/10.5194/bg-19-4589-2022, https://doi.org/10.5194/bg-19-4589-2022, 2022
Short summary
Short summary
We adopt a high-resolution carbon model for the Gulf of Mexico (GoM) and calculate the decadal trends of important carbon system variables in the GoM from 2001 to 2019. The GoM surface CO2 values experienced a steady increase over the past 2 decades, and the ocean surface pH is declining. Although carbonate saturation rates remain supersaturated with aragonite, they show a slightly decreasing trend. The northern GoM is a stronger carbon sink than we thought.
Michael M. Whitney
Biogeosciences, 19, 4479–4497, https://doi.org/10.5194/bg-19-4479-2022, https://doi.org/10.5194/bg-19-4479-2022, 2022
Short summary
Short summary
Coastal hypoxia is a major environmental problem of increasing severity. The 21st-century projections analyzed indicate global coastal waters will warm and experience rapid declines in oxygen. The forecasted median coastal trends for increasing sea surface temperature and decreasing oxygen capacity are 48 % and 18 % faster than the rates observed over the last 4 decades. Existing hypoxic areas are expected to worsen, and new hypoxic areas likely will emerge under these warming-related pressures.
Bryce Van Dam, Nele Lehmann, Mary A. Zeller, Andreas Neumann, Daniel Pröfrock, Marko Lipka, Helmuth Thomas, and Michael Ernst Böttcher
Biogeosciences, 19, 3775–3789, https://doi.org/10.5194/bg-19-3775-2022, https://doi.org/10.5194/bg-19-3775-2022, 2022
Short summary
Short summary
We quantified sediment–water exchange at shallow sites in the North and Baltic seas. We found that porewater irrigation rates in the former were approximately twice as high as previously estimated, likely driven by relatively high bioirrigative activity. In contrast, we found small net fluxes of alkalinity, ranging from −35 µmol m−2 h−1 (uptake) to 53 µmol m−2 h−1 (release). We attribute this to low net denitrification, carbonate mineral (re-)precipitation, and sulfide (re-)oxidation.
Jiaying Abby Guo, Robert Strzepek, Anusuya Willis, Aaron Ferderer, and Lennart Thomas Bach
Biogeosciences, 19, 3683–3697, https://doi.org/10.5194/bg-19-3683-2022, https://doi.org/10.5194/bg-19-3683-2022, 2022
Short summary
Short summary
Ocean alkalinity enhancement is a CO2 removal method with significant potential, but it can lead to a perturbation of the ocean with trace metals such as nickel. This study tested the effect of increasing nickel concentrations on phytoplankton growth and photosynthesis. We found that the response to nickel varied across the 11 phytoplankton species tested here, but the majority were rather insensitive. We note, however, that responses may be different under other experimental conditions.
Malcolm E. Scully, W. Rockwell Geyer, David Borkman, Tracy L. Pugh, Amy Costa, and Owen C. Nichols
Biogeosciences, 19, 3523–3536, https://doi.org/10.5194/bg-19-3523-2022, https://doi.org/10.5194/bg-19-3523-2022, 2022
Short summary
Short summary
For two consecutive summers, the bottom waters in southern Cape Cod Bay became severely depleted of dissolved oxygen. Low oxygen levels in bottom waters have never been reported in this area before, and this unprecedented occurrence is likely the result of a new algae species that recently began blooming during the late-summer months. We present data suggesting that blooms of this new species are the result of regional climate change including warmer waters and changes in summer winds.
Zheng Chen, Bin Wang, Chuang Xu, Zhongren Zhang, Shiyu Li, and Jiatang Hu
Biogeosciences, 19, 3469–3490, https://doi.org/10.5194/bg-19-3469-2022, https://doi.org/10.5194/bg-19-3469-2022, 2022
Short summary
Short summary
Deterioration of low-oxygen conditions in the coastal waters off Hong Kong was revealed by monitoring data over two decades. The declining wind forcing and the increasing nutrient input contributed significantly to the areal expansion and intense deterioration of low-oxygen conditions. Also, the exacerbated eutrophication drove a shift in the dominant source of organic matter from terrestrial inputs to in situ primary production, which has probably led to an earlier onset of hypoxia in summer.
Stella-Theresa Stoicescu, Jaan Laanemets, Taavi Liblik, Māris Skudra, Oliver Samlas, Inga Lips, and Urmas Lips
Biogeosciences, 19, 2903–2920, https://doi.org/10.5194/bg-19-2903-2022, https://doi.org/10.5194/bg-19-2903-2022, 2022
Short summary
Short summary
Coastal basins with high input of nutrients often suffer from oxygen deficiency. In summer 2018, the extent of oxygen depletion was exceptional in the Gulf of Riga. We analyzed observational data and found that extensive oxygen deficiency appeared since the water layer close to the seabed, where oxygen is consumed, was separated from the surface layer. The problem worsens if similar conditions restricting vertical transport of oxygen occur more frequently in the future.
Justin C. Tiano, Jochen Depestele, Gert Van Hoey, João Fernandes, Pieter van Rijswijk, and Karline Soetaert
Biogeosciences, 19, 2583–2598, https://doi.org/10.5194/bg-19-2583-2022, https://doi.org/10.5194/bg-19-2583-2022, 2022
Short summary
Short summary
This study gives an assessment of bottom trawling on physical, chemical, and biological characteristics in a location known for its strong currents and variable habitats. Although trawl gears only removed the top 1 cm of the seabed surface, impacts on reef-building tubeworms significantly decreased carbon and nutrient cycling. Lighter trawls slightly reduced the impact on fauna and nutrients. Tubeworms were strongly linked to biogeochemical and faunal aspects before but not after trawling.
Inda Brinkmann, Christine Barras, Tom Jilbert, Tomas Næraa, K. Mareike Paul, Magali Schweizer, and Helena L. Filipsson
Biogeosciences, 19, 2523–2535, https://doi.org/10.5194/bg-19-2523-2022, https://doi.org/10.5194/bg-19-2523-2022, 2022
Short summary
Short summary
The concentration of the trace metal barium (Ba) in coastal seawater is a function of continental input, such as riverine discharge. Our geochemical records of the severely hot and dry year 2018, and following wet year 2019, reveal that prolonged drought imprints with exceptionally low Ba concentrations in benthic foraminiferal calcium carbonates of coastal sediments. This highlights the potential of benthic Ba / Ca to trace past climate extremes and variability in coastal marine records.
Shichao Tian, Birgit Gaye, Jianhui Tang, Yongming Luo, Wenguo Li, Niko Lahajnar, Kirstin Dähnke, Tina Sanders, Tianqi Xiong, Weidong Zhai, and Kay-Christian Emeis
Biogeosciences, 19, 2397–2415, https://doi.org/10.5194/bg-19-2397-2022, https://doi.org/10.5194/bg-19-2397-2022, 2022
Short summary
Short summary
We constrain the nitrogen budget and in particular the internal sources and sinks of nitrate in the Bohai Sea by using a mass-based and dual stable isotope approach based on δ15N and δ18O of nitrate. Based on available mass fluxes and isotope data an updated nitrogen budget is proposed. Compared to previous estimates, it is more complete and includes the impact of the interior cycle (nitrification) on the nitrate pool. The main external nitrogen sources are rivers contributing 19.2 %–25.6 %.
Gesa Schulz, Tina Sanders, Justus E. E. van Beusekom, Yoana G. Voynova, Andreas Schöl, and Kirstin Dähnke
Biogeosciences, 19, 2007–2024, https://doi.org/10.5194/bg-19-2007-2022, https://doi.org/10.5194/bg-19-2007-2022, 2022
Short summary
Short summary
Estuaries can significantly alter nutrient loads before reaching coastal waters. Our study of the heavily managed Ems estuary (Northern Germany) reveals three zones of nitrogen turnover along the estuary with water-column denitrification in the most upstream hyper-turbid part, nitrate production in the middle reaches and mixing/nitrate uptake in the North Sea. Suspended particulate matter was the overarching control on nitrogen cycling in the hyper-turbid estuary.
Wiley Evans, Geoffrey T. Lebon, Christen D. Harrington, Yuichiro Takeshita, and Allison Bidlack
Biogeosciences, 19, 1277–1301, https://doi.org/10.5194/bg-19-1277-2022, https://doi.org/10.5194/bg-19-1277-2022, 2022
Short summary
Short summary
Information on the marine carbon dioxide system along the northeast Pacific Inside Passage has been limited. To address this gap, we instrumented an Alaskan ferry in order to characterize the marine carbon dioxide system in this region. Data over a 2-year period were used to assess drivers of the observed variability, identify the timing of severe conditions, and assess the extent of contemporary ocean acidification as well as future levels consistent with a 1.5 °C warmer climate.
Melissa Ward, Tye L. Kindinger, Heidi K. Hirsh, Tessa M. Hill, Brittany M. Jellison, Sarah Lummis, Emily B. Rivest, George G. Waldbusser, Brian Gaylord, and Kristy J. Kroeker
Biogeosciences, 19, 689–699, https://doi.org/10.5194/bg-19-689-2022, https://doi.org/10.5194/bg-19-689-2022, 2022
Short summary
Short summary
Here, we synthesize the results from 62 studies reporting in situ rates of seagrass metabolism to highlight spatial and temporal variability in oxygen fluxes and inform efforts to use seagrass to mitigate ocean acidification. Our analyses suggest seagrass meadows are generally autotrophic and variable in space and time, and the effects on seawater oxygen are relatively small in magnitude.
Tianfei Xue, Ivy Frenger, A. E. Friederike Prowe, Yonss Saranga José, and Andreas Oschlies
Biogeosciences, 19, 455–475, https://doi.org/10.5194/bg-19-455-2022, https://doi.org/10.5194/bg-19-455-2022, 2022
Short summary
Short summary
The Peruvian system supports 10 % of the world's fishing yield. In the Peruvian system, wind and earth’s rotation bring cold, nutrient-rich water to the surface and allow phytoplankton to grow. But observations show that it grows worse at high upwelling. Using a model, we find that high upwelling happens when air mixes the water the most. Then phytoplankton is diluted and grows slowly due to low light and cool upwelled water. This study helps to estimate how it might change in a warming climate.
Shao-Min Chen, Ulf Riebesell, Kai G. Schulz, Elisabeth von der Esch, Eric P. Achterberg, and Lennart T. Bach
Biogeosciences, 19, 295–312, https://doi.org/10.5194/bg-19-295-2022, https://doi.org/10.5194/bg-19-295-2022, 2022
Short summary
Short summary
Oxygen minimum zones in the ocean are characterized by enhanced carbon dioxide (CO2) levels and are being further acidified by increasing anthropogenic atmospheric CO2. Here we report CO2 system measurements in a mesocosm study offshore Peru during a rare coastal El Niño event to investigate how CO2 dynamics may respond to ongoing ocean deoxygenation. Our observations show that nitrogen limitation, productivity, and plankton community shift play an important role in driving the CO2 dynamics.
Paula Maria Salgado-Hernanz, Aurore Regaudie-de-Gioux, David Antoine, and Gotzon Basterretxea
Biogeosciences, 19, 47–69, https://doi.org/10.5194/bg-19-47-2022, https://doi.org/10.5194/bg-19-47-2022, 2022
Short summary
Short summary
For the first time, this study presents the characteristics of primary production in coastal regions of the Mediterranean Sea based on satellite-borne observations for the period 2002–2016. The study concludes that there are significant spatial and temporal variations among different regions. Quantifying primary production is of special importance in the marine food web and in the sequestration of carbon dioxide from the atmosphere to the deep waters.
Samu Elovaara, Eeva Eronen-Rasimus, Eero Asmala, Tobias Tamelander, and Hermanni Kaartokallio
Biogeosciences, 18, 6589–6616, https://doi.org/10.5194/bg-18-6589-2021, https://doi.org/10.5194/bg-18-6589-2021, 2021
Short summary
Short summary
Dissolved organic matter (DOM) is a significant carbon pool in the marine environment. The composition of the DOM pool, as well as its interaction with microbes, is complex, yet understanding it is important for understanding global carbon cycling. This study shows that two phytoplankton species have different effects on the composition of the DOM pool and, through the DOM they produce, on the ensuing microbial community. These communities in turn have different effects on DOM composition.
Yuan Dong, Qian P. Li, Zhengchao Wu, Yiping Shuai, Zijia Liu, Zaiming Ge, Weiwen Zhou, and Yinchao Chen
Biogeosciences, 18, 6423–6434, https://doi.org/10.5194/bg-18-6423-2021, https://doi.org/10.5194/bg-18-6423-2021, 2021
Short summary
Short summary
Temporal change of plankton growth and grazing are less known in the coastal ocean, not to mention the relevant controlling mechanisms. Here, we performed monthly size-specific dilution experiments outside a eutrophic estuary over a 1-year cycle. Phytoplankton growth was correlated to nutrients and grazing mortality to total chlorophyll a. A selective grazing on small cells may be important for maintaining high abundance of large-chain-forming diatoms in this eutrophic system.
Kiefer O. Forsch, Lisa Hahn-Woernle, Robert M. Sherrell, Vincent J. Roccanova, Kaixuan Bu, David Burdige, Maria Vernet, and Katherine A. Barbeau
Biogeosciences, 18, 6349–6375, https://doi.org/10.5194/bg-18-6349-2021, https://doi.org/10.5194/bg-18-6349-2021, 2021
Short summary
Short summary
We show that for an unperturbed cold western Antarctic Peninsula fjord, the seasonality of iron and manganese is linked to the dispersal of metal-rich meltwater sources. Geochemical measurements of trace metals in meltwaters, porewaters, and seawater, collected during two expeditions, showed a seasonal cycle of distinct sources. Finally, model results revealed that the dispersal of surface meltwater and meltwater plumes originating from under the glacier is sensitive to katabatic wind events.
Jenny Hieronymus, Kari Eilola, Malin Olofsson, Inga Hense, H. E. Markus Meier, and Elin Almroth-Rosell
Biogeosciences, 18, 6213–6227, https://doi.org/10.5194/bg-18-6213-2021, https://doi.org/10.5194/bg-18-6213-2021, 2021
Short summary
Short summary
Dense blooms of cyanobacteria occur every summer in the Baltic Proper and can add to eutrophication by their ability to turn nitrogen gas into dissolved inorganic nitrogen. Being able to correctly estimate the size of this nitrogen fixation is important for management purposes. In this work, we find that the life cycle of cyanobacteria plays an important role in capturing the seasonality of the blooms as well as the size of nitrogen fixation in our ocean model.
Tom Hull, Naomi Greenwood, Antony Birchill, Alexander Beaton, Matthew Palmer, and Jan Kaiser
Biogeosciences, 18, 6167–6180, https://doi.org/10.5194/bg-18-6167-2021, https://doi.org/10.5194/bg-18-6167-2021, 2021
Short summary
Short summary
The shallow shelf seas play a large role in the global cycling of CO2 and also support large fisheries. We use an autonomous underwater vehicle in the central North Sea to measure the rates of change in oxygen and nutrients.
Using these data we determine the amount of carbon dioxide taken out of the atmosphere by the sea and measure how productive the region is.
These observations will be useful for improving our predictive models and help us predict and adapt to a changing ocean.
Puthenveettil Narayana Menon Vinayachandran, Yukio Masumoto, Michael J. Roberts, Jenny A. Huggett, Issufo Halo, Abhisek Chatterjee, Prakash Amol, Garuda V. M. Gupta, Arvind Singh, Arnab Mukherjee, Satya Prakash, Lynnath E. Beckley, Eric Jorden Raes, and Raleigh Hood
Biogeosciences, 18, 5967–6029, https://doi.org/10.5194/bg-18-5967-2021, https://doi.org/10.5194/bg-18-5967-2021, 2021
Short summary
Short summary
Upwelling in the coastal ocean triggers biological productivity and thus enhances fisheries. Therefore, understanding the phenomenon of upwelling and the underlying mechanisms is important. In this paper, the present understanding of the upwelling along the coastline of the Indian Ocean from the coast of Africa all the way up to the coast of Australia is reviewed. The review provides a synthesis of the physical processes associated with upwelling and its impact on the marine ecosystem.
Gaël Many, Caroline Ulses, Claude Estournel, and Patrick Marsaleix
Biogeosciences, 18, 5513–5538, https://doi.org/10.5194/bg-18-5513-2021, https://doi.org/10.5194/bg-18-5513-2021, 2021
Short summary
Short summary
The Gulf of Lion shelf is one of the most productive areas in the Mediterranean. A model is used to study the mechanisms that drive the particulate organic carbon (POC). The model reproduces the annual cycle of primary production well. The shelf appears as an autotrophic ecosystem with a high production and as a source of POC for the adjacent basin. The increase in temperature induced by climate change could impact the trophic status of the shelf.
Alireza Merikhi, Peter Berg, and Markus Huettel
Biogeosciences, 18, 5381–5395, https://doi.org/10.5194/bg-18-5381-2021, https://doi.org/10.5194/bg-18-5381-2021, 2021
Short summary
Short summary
The aquatic eddy covariance technique is a powerful method for measurements of solute fluxes across the sediment–water interface. Data measured by conventional eddy covariance instruments require a time shift correction that can result in substantial flux errors. We introduce a triple O2 sensor eddy covariance instrument that by design eliminates these errors. Deployments next to a conventional instrument in the Florida Keys demonstrate the improvements achieved through the new design.
Jiatang Hu, Zhongren Zhang, Bin Wang, and Jia Huang
Biogeosciences, 18, 5247–5264, https://doi.org/10.5194/bg-18-5247-2021, https://doi.org/10.5194/bg-18-5247-2021, 2021
Short summary
Short summary
In situ observations over 42 years were used to explore the long-term changes to low-oxygen conditions in the Pearl River estuary. Apparent expansion of the low-oxygen conditions in summer was identified, primarily due to the combined effects of increased anthropogenic inputs and decreased sediment load. Large areas of severe low-oxygen events were also observed in early autumn and were formed by distinct mechanisms. The estuary seems to be growing into a seasonal, estuary-wide hypoxic zone.
Indah Ardiningsih, Kyyas Seyitmuhammedov, Sylvia G. Sander, Claudine H. Stirling, Gert-Jan Reichart, Kevin R. Arrigo, Loes J. A. Gerringa, and Rob Middag
Biogeosciences, 18, 4587–4601, https://doi.org/10.5194/bg-18-4587-2021, https://doi.org/10.5194/bg-18-4587-2021, 2021
Short summary
Short summary
Organic Fe speciation is investigated along a natural gradient of the western Antarctic Peninsula from an ice-covered shelf to the open ocean. The two major fronts in the region affect the distribution of ligands. The excess ligands not bound to dissolved Fe (DFe) comprised up to 80 % of the total ligand concentrations, implying the potential to solubilize additional Fe input. The ligands on the shelf can increase the DFe residence time and fuel local primary production upon ice melt.
Melissa R. McCutcheon, Hongming Yao, Cory J. Staryk, and Xinping Hu
Biogeosciences, 18, 4571–4586, https://doi.org/10.5194/bg-18-4571-2021, https://doi.org/10.5194/bg-18-4571-2021, 2021
Short summary
Short summary
We used 5+ years of discrete samples and 10 months of hourly sensor measurements to explore temporal variability and environmental controls on pH and pCO2 at the Aransas Ship Channel. Seasonal and diel variability were both present but small compared to other regions in the literature. Despite the small tidal range, tidal control often surpassed biological control. In comparison with sensor data, discrete samples were generally representative of mean annual and seasonal carbonate chemistry.
Kai G. Schulz, Eric P. Achterberg, Javier Arístegui, Lennart T. Bach, Isabel Baños, Tim Boxhammer, Dirk Erler, Maricarmen Igarza, Verena Kalter, Andrea Ludwig, Carolin Löscher, Jana Meyer, Judith Meyer, Fabrizio Minutolo, Elisabeth von der Esch, Bess B. Ward, and Ulf Riebesell
Biogeosciences, 18, 4305–4320, https://doi.org/10.5194/bg-18-4305-2021, https://doi.org/10.5194/bg-18-4305-2021, 2021
Short summary
Short summary
Upwelling of nutrient-rich deep waters to the surface make eastern boundary upwelling systems hot spots of marine productivity. This leads to subsurface oxygen depletion and the transformation of bioavailable nitrogen into inert N2. Here we quantify nitrogen loss processes following a simulated deep water upwelling. Denitrification was the dominant process, and budget calculations suggest that a significant portion of nitrogen that could be exported to depth is already lost in the surface ocean.
Heiner Dietze and Ulrike Löptien
Biogeosciences, 18, 4243–4264, https://doi.org/10.5194/bg-18-4243-2021, https://doi.org/10.5194/bg-18-4243-2021, 2021
Short summary
Short summary
In recent years fish-kill events caused by oxygen deficit have been reported in Eckernförde Bight (Baltic Sea). This study sets out to understand the processes causing respective oxygen deficits by combining high-resolution coupled ocean circulation biogeochemical modeling, monitoring data, and artificial intelligence.
Jens A. Hölemann, Bennet Juhls, Dorothea Bauch, Markus Janout, Boris P. Koch, and Birgit Heim
Biogeosciences, 18, 3637–3655, https://doi.org/10.5194/bg-18-3637-2021, https://doi.org/10.5194/bg-18-3637-2021, 2021
Short summary
Short summary
The Arctic Ocean receives large amounts of river water rich in terrestrial dissolved organic matter (tDOM), which is an important component of the Arctic carbon cycle. Our analysis shows that mixing of three major freshwater sources is the main factor that regulates the distribution of tDOM concentrations in the Siberian shelf seas. In this context, the formation and melting of the land-fast ice in the Laptev Sea and the peak spring discharge of the Lena River are of particular importance.
Jaard Hauschildt, Soeren Thomsen, Vincent Echevin, Andreas Oschlies, Yonss Saranga José, Gerd Krahmann, Laura A. Bristow, and Gaute Lavik
Biogeosciences, 18, 3605–3629, https://doi.org/10.5194/bg-18-3605-2021, https://doi.org/10.5194/bg-18-3605-2021, 2021
Short summary
Short summary
In this paper we quantify the subduction of upwelled nitrate due to physical processes on the order of several kilometers in the coastal upwelling off Peru and its effect on primary production. We also compare the prepresentation of these processes in a high-resolution simulation (~2.5 km) with a more coarsely resolved simulation (~12 km). To do this, we combine high-resolution shipboard observations of physical and biogeochemical parameters with a complex biogeochemical model configuration.
Samantha A. Siedlecki, Darren Pilcher, Evan M. Howard, Curtis Deutsch, Parker MacCready, Emily L. Norton, Hartmut Frenzel, Jan Newton, Richard A. Feely, Simone R. Alin, and Terrie Klinger
Biogeosciences, 18, 2871–2890, https://doi.org/10.5194/bg-18-2871-2021, https://doi.org/10.5194/bg-18-2871-2021, 2021
Short summary
Short summary
Future ocean conditions can be simulated using projected trends in fossil fuel use paired with Earth system models. Global models generally do not include local processes important to coastal ecosystems. These coastal processes can alter the degree of change projected. Higher-resolution models that include local processes predict modified changes in carbon stressors when compared to changes projected by global models in the California Current System.
Erik Jacobs, Henry C. Bittig, Ulf Gräwe, Carolyn A. Graves, Michael Glockzin, Jens D. Müller, Bernd Schneider, and Gregor Rehder
Biogeosciences, 18, 2679–2709, https://doi.org/10.5194/bg-18-2679-2021, https://doi.org/10.5194/bg-18-2679-2021, 2021
Short summary
Short summary
We use a unique data set of 8 years of continuous carbon dioxide (CO2) and methane (CH4) surface water measurements from a commercial ferry to study upwelling in the Baltic Sea. Its seasonality and regional and interannual variability are examined. Strong upwelling events drastically increase local surface CO2 and CH4 levels and are mostly detected in late summer after long periods of impaired mixing. We introduce an extrapolation method to estimate regional upwelling-induced trace gas fluxes.
Yangyang Zhao, Khanittha Uthaipan, Zhongming Lu, Yan Li, Jing Liu, Hongbin Liu, Jianping Gan, Feifei Meng, and Minhan Dai
Biogeosciences, 18, 2755–2775, https://doi.org/10.5194/bg-18-2755-2021, https://doi.org/10.5194/bg-18-2755-2021, 2021
Short summary
Short summary
In situ oxygen consumption rates were estimated for the first time during destruction of coastal hypoxia as disturbed by a typhoon and its reinstatement in the South China Sea off the Pearl River estuary. The reinstatement of summer hypoxia was rapid with a comparable timescale with that of its initial disturbance from frequent tropical cyclones, which has important implications for better understanding the intermittent nature of coastal hypoxia and its prediction in a changing climate.
Dylan R. Brown, Humberto Marotta, Roberta B. Peixoto, Alex Enrich-Prast, Glenda C. Barroso, Mario L. G. Soares, Wilson Machado, Alexander Pérez, Joseph M. Smoak, Luciana M. Sanders, Stephen Conrad, James Z. Sippo, Isaac R. Santos, Damien T. Maher, and Christian J. Sanders
Biogeosciences, 18, 2527–2538, https://doi.org/10.5194/bg-18-2527-2021, https://doi.org/10.5194/bg-18-2527-2021, 2021
Short summary
Short summary
Hypersaline tidal flats (HTFs) are coastal ecosystems with freshwater deficits often occurring in arid or semi-arid regions near mangrove supratidal zones with no major fluvial contributions. This study shows that HTFs are important carbon and nutrient sinks which may be significant given their extensive coverage. Our findings highlight a previously unquantified carbon as well as a nutrient sink and suggest that coastal HTF ecosystems could be included in the emerging blue carbon framework.
Giulia Bonino, Elisa Lovecchio, Nicolas Gruber, Matthias Münnich, Simona Masina, and Doroteaciro Iovino
Biogeosciences, 18, 2429–2448, https://doi.org/10.5194/bg-18-2429-2021, https://doi.org/10.5194/bg-18-2429-2021, 2021
Short summary
Short summary
Seasonal variations of processes such as upwelling and biological production that happen along the northwestern African coast can modulate the temporal variability of the biological activity of the adjacent open North Atlantic hundreds of kilometers away from the coast thanks to the lateral transport of coastal organic carbon. This happens with a temporal delay, which is smaller than a season up to roughly 500 km from the coast due to the intense transport by small-scale filaments.
Markus Diesing, Terje Thorsnes, and Lilja Rún Bjarnadóttir
Biogeosciences, 18, 2139–2160, https://doi.org/10.5194/bg-18-2139-2021, https://doi.org/10.5194/bg-18-2139-2021, 2021
Short summary
Short summary
The upper 10 cm of the seafloor of the North Sea and Skagerrak contain 231×106 t of carbon in organic form. The Norwegian Trough, the deepest sedimentary basin in the studied area, stands out as a zone of strong organic carbon accumulation with rates on par with neighbouring fjords. Conversely, large parts of the North Sea are characterised by rapid organic carbon degradation and negligible accumulation. This dual character is likely typical for continental shelf sediments worldwide.
Arnaud Laurent, Katja Fennel, and Angela Kuhn
Biogeosciences, 18, 1803–1822, https://doi.org/10.5194/bg-18-1803-2021, https://doi.org/10.5194/bg-18-1803-2021, 2021
Short summary
Short summary
CMIP5 and CMIP6 models, and a high-resolution regional model, were evaluated by comparing historical simulations with observations in the northwest North Atlantic, a climate-sensitive and biologically productive ocean margin region. Many of the CMIP models performed poorly for biological properties. There is no clear link between model resolution and skill in the global models, but there is an overall improvement in performance in CMIP6 from CMIP5. The regional model performed best.
Heejun Han, Jeomshik Hwang, and Guebuem Kim
Biogeosciences, 18, 1793–1801, https://doi.org/10.5194/bg-18-1793-2021, https://doi.org/10.5194/bg-18-1793-2021, 2021
Short summary
Short summary
The main source of excess DOC occurring in coastal seawater off an artificial lake, which is enclosed by a dike along the western coast of South Korea, was determined using a combination of various biogeochemical tools including DOC and nutrient concentrations, stable carbon isotope, and optical properties (absorbance and fluorescence) of dissolved organic matter in two different seasons (March 2017 and September 2018).
Cited articles
Agawin, N. S., Duarte, C. M., and Agustí, S.: Nutrient and temperature
control of the contribution of picoplankton to phytoplankton biomass and
production, Limnol. Oceanogr., 45, 591–600, 2000.
Anderson, L. G. and Kaltin, S.: Carbon fluxes in the Arctic Ocean-potential
impact by climate change, Polar Res., 20, 225–232, 2001.
Anderson, L. G., Jutterström, S., Kaltin, S., Jones, E. P., and
Björk, G.: Variability in river runoff distribution in the Eurasian Basin
of the Arctic Ocean, J. Geophys. Res.-Oceans, 109, https://doi.org/10.1029/2003JC001773, 2004.
Anderson, L. G., Jutterström, S., Hjalmarsson, S., Wåhlström, I.,
and Semiletov, I.: Out-gassing of CO2 from Siberian Shelf seas by
terrestrial organic matter decomposition, Geophys. Res. Lett., 36, L20601, https://doi.org/10.1029/2009GL040046,
2009.
Aksnes, D. L. and Egge, J. K.: A theoretical model for nutrient uptake in
phytoplankton, Mar. Ecol.-Prog. Ser., 70, 65–72, 1991.
Ardyna, M., Babin, M., Gosselin, M., Devred, E., Rainville, L., and Tremblay,
J. É.: Recent Arctic Ocean sea ice loss triggers novel fall phytoplankton
blooms, Geophys. Res. Lett., 41, 6207–6212, 2014.
Arrigo, K. R. and van Dijken, G. L.: Secular trends in Arctic Ocean net
primary production, J. Geophys. Res., 116, C09011, https://doi.org/10.1029/2011JC007151,
2011.
Arrigo, K. R. and van Dijken, G. L.: Continued increases in Arctic Ocean
primary production, Prog. Oceanogr., 136, 60–70, 2015.
Arrigo, K. R., van Dijken, G., and Pabi, S.: Impact of a shrinking Arctic ice
cover on marine primary production, Geophys. Res. Lett., 35, L19603, https://doi.org/10.1029/2008GL035028,
2008.
Arrigo, K. R., Perovich, D. K., Pickart, R. S., Brown, Z. W., Van Dijken, G.
L., Lowry, K. E., Mills, M. M., Palmer, M. A., Balch, W. M., Bahr, F., and
Bates, N. R.: Massive phytoplankton blooms under Arctic sea ice, Science,
336, 1408–1408, 2012.
Bates, N. R. and Mathis, J. T.: The Arctic Ocean marine carbon cycle:
evaluation of air-sea CO2 exchanges, ocean acidification impacts and
potential feedbacks, Biogeosciences, 6, 2433–2459,
https://doi.org/10.5194/bg-6-2433-2009, 2009.
Bates, N. R., Moran, S. B., Hansell, D. A., and Mathis, J. T.: An increasing
CO2 sink in the Arctic Ocean due to sea-ice loss, Geophys. Res.
Lett., 33, L23609, https://doi.org/10.1029/2006GL027028, 2006.
Bélanger, S., Babin, M., and Larouche, P.: An empirical ocean color
algorithm for estimating the contribution of chromophoric dissolved organic
matter to total light absorption in optically complex waters, J. Geophys.
Res., 13, C04027, https://doi.org/10.1029/2007JC004436, 2008.
Bélanger, S., Babin, M., and Tremblay, J.-É.: Increasing cloudiness
in Arctic damps the increase in phytoplankton primary production due to sea
ice receding, Biogeosciences, 10, 4087–4101,
https://doi.org/10.5194/bg-10-4087-2013, 2013.
Bhavya, P. S., Kumar, S., Gupta, G. V. M., Sudheesh, V., Sudharma, K. V.,
Varrier, D. S., Dhanya, K. R., and Saravanane, N.: Nitrogen uptake dynamics
in a tropical eutrophic estuary (Cochin estuary) and adjacent coastal regions
during pre-monsoon, Estuar. Coast., 39, 54–67,
https://doi.org/10.1007/s12237-015-9982-y, 2016.
Bhavya, P. S., Kumar, S., Gupta, G. V. M., and Sudheesh, V.: Carbon uptake
rates in the Cochin estuary and adjoining coastal Arabian Sea, Estuar.
Coast., 40, 447–456, https://doi.org/10.1007/s12237-016-0147-4, 2017.
Boetius, A. and Damm, E.: Benthic oxygen uptake, hydrolytic potentials and
microbial biomass at the Arctic continental slope, Deep-Sea Res. Pt. I, 45,
239–275, 1998.
Bopp, L., Monfray, P., Aumont, O., Dufresne, J. L., Le Treut, H., Madec, G.,
Terray, L., and Orr, J. C.: Potential impact of climate change on marine
export production, Global Biogeochem. Cy., 15, 81–99, 2001.
Cai, W. J., Chen, L., Chen, B., Gao, Z., Lee, S. H., Chen, J., Pierrot, D.,
Sullivan, K., Wang, Y., Hu, X., and Huang, W. J.: Decrease in the
CO2 uptake capacity in an ice-free Arctic Ocean basin, Science,
329, 556–559, 2010.
Carmack, E. C. and Macdonald, R. W.: Oceanography of the Canadian Shelf of
the Beaufort Sea: a setting for marine life, Arctic, 55, 29–45,
2002.
Carmack, E. C., Aagaard, K., Swift, J. H., MacDonald, R. W., McLaughlin, F.
A., Jones, E. P., Perkin, R. G., Smith, J. N., Ellis, K. M., and Killius, L.
R.: Changes in temperature and tracer distributions within the Arctic Ocean:
Results from the 1994 Arctic Ocean section, Deep-Sea Res. Pt. II, 44,
1487–1502, 1997.
Clasby, R. C., Horner, R., and Alexander, V.: An in situ method for measuring
primary productivity of Arctic sea ice algae, J. Fish. Res. Board Can., 30,
835–838, 1973.
Codispoti, L. A. and Richards, F. A.: Micronutrient distributions in the East
Siberian and Laptev seas during summer 1963, Arctic, 21, 67–83,
1968.
Comiso, J. C., Parkinson, C. L., Gersten, R., and Stock, L.: Accelerated
decline in the Arctic sea ice cover, Geophys. Res. Lett., 35, L01703, https://doi.org/10.1029/2007GL031972,
2008.
Daufresne, M., Lengfellner, K., and Sommer, U.: Global warming benefits the
small in aquatic ecosystems, P. Natl. Acad. Sci. USA, 106, 12788–12793,
2009.
Dmitrenko, I. A., Polyakov, I. V., Kirillov, S. A., Timokhov, L. A., Simmons,
H. L., Ivanov, V. V., and Walsh, D.: Seasonal variability of Atlantic water
on the continental slope of the Laptev Sea during 2002–2004, Earth Planet.
Sc. Lett., 244, 735–743, 2006.
Dugdale, R. and Goering, J.: Uptake of new and regenerated forms of nitrogen
in primary productivity, Limnol. Oceanogr., 12, 196–206, 1967.
Dugdale, R. C. and Wilkerson, F. P.: The use of 15N to measure
nitrogen uptake in eutrophic oceans; experimental considerations, Limnol.
Oceanogr., 31, 673–689, 1986.
Eastman, R. and Warren, S. G.: Interannual variations of Arctic cloud types
in relation to sea ice, J. Climate, 23, 4216–4232, 2010.
Eppley, R. W. and Thomas, W. H.: Comparison of half-saturation constants for
growth and nitrate uptake of marine phytoplankton, J. Phycol., 5, 375–379,
1969.
Falk-Petersen, S., Hop, H., Budgell, W. P., Hegseth, E. N., Korsnes, R.,
Løyning, T. B., Ørbæk, J. B., Kawamura, T., and Shirasawa, K.:
Physical and ecological processes in the marginal ice zone of the northern
Barents Sea during the summer melt period, J. Marine Syst., 27, 131–159,
2000.
Glibert, P. M.: Regional studies of daily, seasonal and size fraction
variability in ammonium remineralization, Mari. Biol., 70, 209–222, 1982.
Glibert, P. M., Kana, T. M., and Brown, K.: From limitation to excess: the
consequences of substrate excess and stoichiometry for phytoplankton
physiology, trophodynamics and biogeochemistry, and the implications for
modeling, J. Marine Syst., 125, 14–28, 2013.
Gosselin, M., Levasseur, M., Wheeler, P. A., Horner, R. A., and Booth, B. C.:
New measurements of phytoplankton and ice algal production in the Arctic
Ocean, Deep-Sea Res. Pt. II, 44, 1623–1644, 1997.
Gradinger, R.: Sea-ice algae: major contributors to primary production and
algal biomass in the Chukchi and Beaufort seas during May/June 2002, Deep-Sea
Res. Pt. II, 44, 1623–1644, https://doi.org/10.1016/j.dsr2.2008.10.016,
2009.
Grover, J. P.: Influence of cell shape and size on algal competitive ability,
J. Phycol., 25, 402–405, 1989.
Grover, J. P.: Resource competition in a variable environment: phytoplankton
growing according to the variable-internal-stores model, Am. Nat., 138,
811–835, 1991.
Harrison, W. G. and Cota, G. F.: Primary production in polar waters: relation
to nutrient availability, Polar Res., 10, 87–104, 1991.
Harrison W. G., Li, W. K. W., Smith, J. C., Head, E. J. H., and Longhurst, A.
R.: Depth profiles of plankton, particulate organic matter and microbial
activity in the Eastern Canadian Arctic during summer, Polar Biol., 7,
207–224, 1987.
Hein, M., Folager Pedersen, M., and Sand-Jensen, K.: Size-dependent nitrogen
uptake in micro- and macroalgae, Mar. Ecol.-Prog. Ser., 118, 247–253, 1995.
Hill, V., Ardyna, M., Lee, S. H., and Varela, D. E.: Decadal trends in
phytoplankton production in the Pacific Arctic Region from 1950 to 2012,
Deep-Sea Res. Pt. II, https://doi.org/10.1016/j.dsr2.2016.12.015, in press, 2017.
Hill, V. J. and Cota, G. F.: Spatial patterns of primary production in the
Chukchi Sea in the spring and summer of 2002, Deep-Sea Res. Pt. II, 52,
3344–3354, 2005.
Hodal, H. and Kristiansen, S.: The importance of small-celled phytoplankton
in spring blooms at the marginal ice zone in the northern Barents Sea,
Deep-Sea Res. Pt. II, 55, 2176–2185, 2008.
Horner, R. and Schrader, G. C.: Relative contributions of ice algae,
phytoplankton, and benthic microalgae to primary production in nearshore
regions of the Beaufort Sea, Arctic, 35, 485–503, 1982.
Jakobsson, M. and IBCAO Editorial Board Members: Improvement to the
International Bathymetric Chart of the Arctic Ocean (IBCAO): Updating the
Data Base and the Grid Model, EOS T. Am. Geophys. Un., 82, Fall Meet. Suppl.,
Abstract no. OS11B-0371, 2001.
Joo, H., Son, S., Park, J. W., Kang, J. J., Jeong, J. Y., Kwon, J. I., Kang,
C. K., and Lee, S. H.: Small phytoplankton contribution to the total primary
production in the highly productive Ulleung Basin in the East/Japan Sea,
Deep-Sea Res. Pt. II, 143, 54–61, 2017.
Kahru, M., Lee, Z., Mitchell, B. G., and Nevison, C. D.: Effects of sea ice
cover on satellite-detected primary production in the Arctic Ocean, Biol.
Letters, 12, 20160223, https://doi.org/10.1098/rsbl.2016.0223, 2016.
Kirk, J. T. O.: Light and Photosynthesis in the Aquatic Ecosystems, Cambridge
Univ. Press, Cambridge, UK, 1983.
Kwok, R., Cunningham, G. F., Wensnahan, M., Rigor, I., Zwally, H. J., and Yi,
D.: Thinning and volume loss of the Arctic Ocean sea ice cover: 2003–2008,
J. Geophys. Res., 114, C07005, https://doi.org/10.1029/2009JC005312, 2009.
Lee, S. H. and Whitledge, T. E.: Primary and new production in the deep
Canada Basin during summer 2002, Polar Biol., 28, 190–197, 2005.
Lee, S. H., Whitledge, T. E., and Kang, S.: Recent carbon and nitrogen uptake
rates of phytoplankton in Bering Strait and the Chukchi Sea, Cont. Shelf
Res., 27, 2231–2249, 2007.
Lee, S. H., Joo, H. M., Liu, Z., Chen, J., and He, J.: Phytoplankton
productivity in newly opened waters of the Western Arctic Ocean, Deep-Sea
Res. Pt. II, 81, 18–27, 2012.
Lee, S. H., Yun, M. S., Kim, B. K., Joo, H., Kang, S. J., Kang, C. K., and
Whitledge, T. E.: Contribution of small phytoplankton to total primary
production in the Chukchi Sea, Cont. Shelf Res., 68, 43–50, 2013.
Lee, S. H., Kim, B. K., Lim, Y. J., Joo, H., Kang, J. J., Lee, D., Park, J.,
Ha, S.-Y., and Lee, S. H.: Small phytoplankton contribution to the standing
stocks and the total primary production in the Amundsen Sea, Biogeosciences,
14, 3705–3713, https://doi.org/10.5194/bg-14-3705-2017, 2017a.
Lee, S. H., Joo, H. T., Lee, J. H., Lee, J. H., Kang, J. J., Lee, H. W., Lee, D., and Kang, C. K.: Seasonal carbon
uptake rates of phytoplankton in the northern East/Japan Sea, Deep-Sea Res.
Pt. II, 143, 45–53, https://doi.org/10.1016/j.dsr2.2017.04.009, 2017b.
Legendre, L., Ackley, S. F., Dieckmann, G. S., Gulliksen, B., Horner, R.,
Hoshiai, T., Melnikov, I. A., Reeburgh, W. S., Spindler, M., and Sullivan, C.
W.: Ecology of sea ice biota, Polar Biol., 12, 429–444, 1992.
Levi, B. G.: The decreasing Arctic ice cover, Phys. Today, 53, 19–20,
https://doi.org/10.1063/1.882931, 2000.
Li, J., Glibert, P. M., and Alexander, J. A.: Effects of ambient DIN : DIP
ratio on the nitrogen uptake of harmful dinoflagellate Prorocentrum minimum and Prorocentrum donghaiense in turbidistat, Chin. J.
Oceanol. Limn., 29, 746–761, 2011.
Li, W. K., McLaughlin, F. A., Lovejoy, C., and Carmack, E. C.: Smallest algae
thrive as the Arctic Ocean freshens, Science, 326, 539, https://doi.org/10.1126/science.1179798, 2009.
Martin, J., Tremblay, J. É., Gagnon, J., Tremblay, G., Lapoussière,
A., Jose, C., Poulin, M., Gosselin, M., Gratton, Y., and Michel, C.:
Prevalence, structure and properties of subsurface chlorophyll maxima in
Canadian Arctic waters, Mar. Ecol.-Progr. Ser., 412, 69–84, 2010.
Maslowski, W., Marble, D., Walczowski, W., Schauer, U., Clement, J. L., and
Semtner, A. J.: On climatological mass, heat, and salt transports through the
Barents Sea and Fram Strait from a pan-Arctic coupled ice-ocean model
simulation, J. Geophys. Res.-Oceans, 109, C03032, https://doi.org/10.1029/2001JC001039, 2004.
McCarthy, J. J., Garside, C., and Nevins, J. L.: Nitrogen dynamics during the
Arabian Sea northeast monsoon, Deep-Sea Res. Pt. II, 46, 1623–1664, 1999.
McLaughlin, F. A., Carmack, E. C., Jackson, J. M., Ingram, R. G., and Allen,
S. E.: Identification, characterization, and change of the near-surface
temperature maximum in the Canada Basin, 1993–2008, Doctoral dissertation,
University of British Columbia, 2010.
Niebauer, H. J., Alexander, V., and Henrichs, S.: Physical and biological
oceanographic interaction in the spring bloom at the Bering Sea marginal ice
edge zone, J. Geophys. Res.-Oceans, 95, 22229–22241, 1990.
Overland, J. E. and Wang, M.: When will the summer Arctic be nearly sea ice
free?, Geophys. Res. Lett., 40, 2097–2101, 2013.
Pabi, S., van Dijken, G., and Arrigo, K. R.: Primary production in the Arctic
Ocean, 1998–2006, J. Geophys. Res., 113, C08005, https://doi.org/10.1029/2007JC004578,
2008.
Parkinson, C. L., Cavalieri, D. J., Gloersen, P., Zwally, J. H., and Comiso,
J. C.: Arctic sea ice extents, areas, and trends, 1978–1996, J. Geophys.
Res., 104, 20837–20856, 1999.
Peterson, B. J., Holmes, R. M., McClelland, J. W., Vörösmarty, C. J.,
Lammers, R. B., Shiklomanov, A. I., Shiklomanov, I. A., and Rahmstorf, S.:
Increasing river discharge to the Arctic Ocean, Science, 298, 2171–2173,
2002.
Platt, T., Harrison, W. G., Irwin, B., Horne, E. P., and Gallegos, C. L.:
Photosynthesis and photo adaptation of marine phytoplankton in the Arctic,
Deep-Sea Res. Pt. I, 29, 1159–1170, 1982.
Quadfasel, D.: Oceanography: The Atlantic heat conveyor slows, Nature, 438,
565–566, 2005.
Rachold, V., Grigoriev, M. N., Are, F. E., Solomon, S., Reimnitz, E.,
Kassens, H., and Antonow, M.: Coastal erosion vs. riverine sediment discharge
in the Arctic shelf seas, Int. J. Earth. Sci., 89, 450–460, 2000.
Redfield, A. C.: The influence of organisms on the composition of seawater,
The Sea, 2, 26–77, 1963.
Sakshaug, E.: Primary and Secondary Production in the Arctic Seas, in: The
Organic Carbon Cycle in the Arctic Ocean, edited by: Stein, R. and MacDonald,
R. W., Springer, Berlin, Heidelberg, 2004.
Sakshaug, E. and Holm-Hansen, O.: Factors governing pelagic production in
polar oceans, in: Marine phytoplankton and productivity, 1–18, Springer,
Berlin, Heidelberg, 1984.
Semiletov, I., Dudarev, O., Luchin, V., Charkin, A., Shin, K. H., and Tanaka,
N.: The East Siberian Sea as a transition zone between Pacific-derived waters
and Arctic shelf waters, Geophys. Res. Lett., 32, L10614, https://doi.org/10.1029/2005GL022490, 2005.
Shiklomanov, I. A., Shiklomanov, A. I., Lammers, R. B., Peterson, B. J., and
Vorosmarty, C. J.: The dynamics of river water inflow to the Arctic Ocean,
in: The freshwater budget of the Arctic Ocean (281–296), Springer,
Dordrecht, 2000.
Shuter, B. G.: Size dependence of phophorus and nitrogen subsistence quotas
in unicellular microrganisms, Limnol. Oceanogr., 23, 1248–1255, 1978.
Slagstad, D., Ellingsen, I. H., and Wassmann, P.: Evaluating primary and
secondary production in an Arctic Ocean void of summer sea ice: an
experimental simulation approach, Prog. Oceanogr., 90, 117–131, 2011.
Slawyk, G., Collos, Y., and Auclair, J. C.: The use of the 13C and
15N isotopes for the simultaneous measurement of carbon and
nitrogen turnover rates in marine phytoplankton, Limnol. Oceanogr., 22,
925–932, 1977.
Son, S. H., Campbell, J., Dowell, M., Yoo, S., and Noh, J.: Primary
production in the Yellow Sea determined by ocean color remote sensing, Mar.
Ecol.-Prog. Ser., 303, 91–103, 2005.
Steinacher, M., Joos, F., Frölicher, T. L., Bopp, L., Cadule, P., Cocco,
V., Doney, S. C., Gehlen, M., Lindsay, K., Moore, J. K., Schneider, B., and
Segschneider, J.: Projected 21st century decrease in marine productivity: a
multi-model analysis, Biogeosciences, 7, 979–1005,
https://doi.org/10.5194/bg-7-979-2010, 2010.
Stroeve, J., Holland, M. M., Meier, W., Stroeve, J, Holland, M. M., Meier, W., Scambos, T., and Serreze, M.: Arctic sea ice decline: faster than forecast, Geophys. Res.
Lett., 34, L09501, https://doi.org/10.1029/2007GL029703, 2008.
Subba Rao, D. V. and Platt, T.: Primary production of Arctic waters, Polar
Biol., 3, 191–210, 1984.
Talling, J. F.: The phytoplankton population as a compound photosynthetic
system, New Phytol., 56, 133–149, 1957.
Thomas, M. K., Kremer, C. T., Klausmeier, C. A., and Litchman, E.: A global
pattern of thermal adaptation in marine phytoplankton, Science, 338,
1085–1088, 2012.
Tremblay, J. E. and Gagnon, G.: The effects of irradiance and nutrient supply
on the productivity of Arctic waters: a perspective on climate change, in:
Influence of climate change on the changing Arctic and sub-Arctic conditions.
Proceedings of the NATO advanced research workshop, edited by: Nihoul, J. C.
J. and Kostianoy, A. G., Liège, May 2008, Springer, Dordrecht, 73–94,
2009.
Tremblay, J. É., Legendre, L., Klein, B., and Therriault, C.:
Size-differential uptake of nitrogen and carbon in a marginal sea (Gulf of
St. Lawrance, Canada): Significance of diel periodicity and urea uptake,
Deep-Sea Res. Pt. II, 47, 489–518, 2000.
Tremblay, J. É., Gratton, Y., Carmack, E. C., Payne, C. D., and Price, N.
M.: Impact of the large-scale Arctic circulation and the North Water Polynya
on nutrient inventories in Baffin Bay, J. Geophys. Res.-Oceans, 107, 26–31,
2002.
Vancoppenolle, M., Meiners, K. M., Michel, C., Bopp, L., Brabant, F., Carnat,
G., Delille, B., Lannuzel, D., Madec, G., Moreau, S., and Tison, J. L.: Role
of sea ice in global biogeochemical cycles: emerging views and challenges,
Quaternary Sci. Rev., 79, 207–230, 2013.
Vavrus, S. J., Holland, M. M., Jahn, A., Bailey, D. A., and Blazey, B. A.:
Twenty-first-century Arctic climate change in CCSM4, J. Climate, 25,
2696–2710, 2012.
Vedernikov, V. I., Demidov, A. B., and Sudbin, A. I.: Primary production and
chlorophyll in the Kara Sea in September 1993, Okeanologiya, 34, 693–703,
1994.
Walsh, J. J.: Arctic carbon sinks: present and future, Global. Biogeochem.
Cy., 3, 393–411, https://doi.org/10.1029/GB003i004p00393, 1989.
Wassmann, P., Duarte, C. M., Agusti, S., and Sejr, M. K.: Footprints of
climate change in the Arctic marine ecosystem, Glob. Change Biol., 17,
1235–1249, 2011.
Whitledge, T. E., Malloy, S. C., Patton, C. J., and Wirick, C. D.: Automated
nutrient analyses in seawater (No. BNL-51398), Brookhaven National Lab.,
Upton, NY, USA, 1981.
Yun, M. S., Chung, K. H., Zimmermann, S., Zhao, J., Joo, H. M., and Lee, S.
H.: Phytoplankton productivity and its response to higher light levels in the
Canada Basin, Polar Biol., 35, 257–268, 2012.
Yun, M. S., Kim, B. K., Joo, H. T., Yang, E. J., Nishino, S., Chung, K. H.,
Kang, S., and Lee, S. H.: Regional productivity of phytoplankton in the
Western Arctic Ocean during summer in 2010, Deep-Sea Res. Pt. II, 120,
61–71, 2015.
Altmetrics
Final-revised paper
Preprint