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Lapointe BE, Brewton RA, Herren LW, Wang M, Hu C, McGillicuddy DJ, Lindell S, Hernandez FJ, Morton PL. Nutrient content and stoichiometry of pelagic Sargassum reflects increasing nitrogen availability in the Atlantic Basin. Nat Commun 2021; 12:3060. [PMID: 34031385 PMCID: PMC8144625 DOI: 10.1038/s41467-021-23135-7] [Citation(s) in RCA: 29] [Impact Index Per Article: 9.7] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/30/2020] [Accepted: 04/09/2021] [Indexed: 11/25/2022] Open
Abstract
The pelagic brown macroalgae Sargassum spp. have grown for centuries in oligotrophic waters of the North Atlantic Ocean supported by natural nutrient sources, such as excretions from associated fishes and invertebrates, upwelling, and N2 fixation. Using a unique historical baseline, we show that since the 1980s the tissue %N of Sargassum spp. has increased by 35%, while %P has decreased by 44%, resulting in a 111% increase in the N:P ratio (13:1 to 28:1) and increased P limitation. The highest %N and δ15N values occurred in coastal waters influenced by N-rich terrestrial runoff, while lower C:N and C:P ratios occurred in winter and spring during peak river discharges. These findings suggest that increased N availability is supporting blooms of Sargassum and turning a critical nursery habitat into harmful algal blooms with catastrophic impacts on coastal ecosystems, economies, and human health.
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Affiliation(s)
- B E Lapointe
- Harbor Branch Oceanographic Institute, Florida Atlantic University, Fort Pierce, FL, USA.
| | - R A Brewton
- Harbor Branch Oceanographic Institute, Florida Atlantic University, Fort Pierce, FL, USA
| | - L W Herren
- Harbor Branch Oceanographic Institute, Florida Atlantic University, Fort Pierce, FL, USA
| | - M Wang
- College of Marine Science, University of South Florida, St. Petersburg, FL, USA
| | - C Hu
- College of Marine Science, University of South Florida, St. Petersburg, FL, USA
| | | | - S Lindell
- Woods Hole Oceanographic Institution, Woods Hole, MA, USA
| | - F J Hernandez
- Division of Coastal Sciences, University of Southern Mississippi, Ocean Springs, MS, USA
| | - P L Morton
- Florida State University/National High Magnetic Field Lab, Tallahassee, FL, USA
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2
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Baker AR, Landing WM, Bucciarelli E, Cheize M, Fietz S, Hayes CT, Kadko D, Morton PL, Rogan N, Sarthou G, Shelley RU, Shi Z, Shiller A, van Hulten MMP. Trace element and isotope deposition across the air-sea interface: progress and research needs. Philos Trans A Math Phys Eng Sci 2016; 374:20160190. [PMID: 29035268 PMCID: PMC5069538 DOI: 10.1098/rsta.2016.0190] [Citation(s) in RCA: 5] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Accepted: 06/30/2016] [Indexed: 05/24/2023]
Abstract
The importance of the atmospheric deposition of biologically essential trace elements, especially iron, is widely recognized, as are the difficulties of accurately quantifying the rates of trace element wet and dry deposition and their fractional solubility. This paper summarizes some of the recent progress in this field, particularly that driven by the GEOTRACES, and other, international research programmes. The utility and limitations of models used to estimate atmospheric deposition flux, for example, from the surface ocean distribution of tracers such as dissolved aluminium, are discussed and a relatively new technique for quantifying atmospheric deposition using the short-lived radionuclide beryllium-7 is highlighted. It is proposed that this field will advance more rapidly by using a multi-tracer approach, and that aerosol deposition models should be ground-truthed against observed aerosol concentration data. It is also important to improve our understanding of the mechanisms and rates that control the fractional solubility of these tracers. Aerosol provenance and chemistry (humidity, acidity and organic ligand characteristics) play important roles in governing tracer solubility. Many of these factors are likely to be influenced by changes in atmospheric composition in the future. Intercalibration exercises for aerosol chemistry and fractional solubility are an essential component of the GEOTRACES programme.This article is part of the themed issue 'Biological and climatic impacts of ocean trace element chemistry'.
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Affiliation(s)
- A R Baker
- Centre for Ocean and Atmospheric Science, School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, UK
| | - W M Landing
- Department of Earth, Ocean and Atmospheric Science, Florida State University, Tallahassee, FL 32306, USA
| | - E Bucciarelli
- LEMAR/IUEM, UMR 6539 CNRS-UBO-IRD-IFREMER, Place Nicolas Copernic, Technopôle Brest Iroise, 29280 Plouzané, France
| | - M Cheize
- LEMAR/IUEM, UMR 6539 CNRS-UBO-IRD-IFREMER, Place Nicolas Copernic, Technopôle Brest Iroise, 29280 Plouzané, France
| | - S Fietz
- Department of Earth Sciences, Stellenbosch University, 7600 Stellenbosch, South Africa
| | - C T Hayes
- Department of Marine Science, University of Southern Mississippi, Stennis Space Center, Kiln, MS 39529, USA
| | - D Kadko
- Applied Research Center, Florida International University, 10555 West Flagler St., Engineering Center Suite 2100, Miami, FL 33174, USA
| | - P L Morton
- Department of Earth, Ocean and Atmospheric Science, Florida State University, Tallahassee, FL 32306, USA
| | - N Rogan
- GEOMAR, Helmholtz Centre for Ocean Research Kiel, 1-3 Wischhofstrasse, Kiel 24148, Germany
| | - G Sarthou
- LEMAR/IUEM, UMR 6539 CNRS-UBO-IRD-IFREMER, Place Nicolas Copernic, Technopôle Brest Iroise, 29280 Plouzané, France
| | - R U Shelley
- LEMAR/IUEM, UMR 6539 CNRS-UBO-IRD-IFREMER, Place Nicolas Copernic, Technopôle Brest Iroise, 29280 Plouzané, France
| | - Z Shi
- School of Geography Earth and Environmental Sciences, University of Birmingham, Birmingham, UK
| | - A Shiller
- Department of Marine Science, University of Southern Mississippi, Stennis Space Center, Kiln, MS 39529, USA
| | - M M P van Hulten
- Laboratoire des Sciences du Climat et de l'Environnement (LSCE), IPSL, CEA-Orme des Merisiers, 91191 Gif-sur-Yvette, France
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Anderson RF, Cheng H, Edwards RL, Fleisher MQ, Hayes CT, Huang KF, Kadko D, Lam PJ, Landing WM, Lao Y, Lu Y, Measures CI, Moran SB, Morton PL, Ohnemus DC, Robinson LF, Shelley RU. How well can we quantify dust deposition to the ocean? Philos Trans A Math Phys Eng Sci 2016; 374:rsta.2015.0285. [PMID: 29035251 DOI: 10.1098/rsta.2015.02852016] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.1] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Subscribe] [Scholar Register] [Accepted: 08/10/2016] [Indexed: 05/25/2023]
Abstract
Deposition of continental mineral aerosols (dust) in the Eastern Tropical North Atlantic Ocean, between the coast of Africa and the Mid-Atlantic Ridge, was estimated using several strategies based on the measurement of aerosols, trace metals dissolved in seawater, particulate material filtered from the water column, particles collected by sediment traps and sediments. Most of the data used in this synthesis involve samples collected during US GEOTRACES expeditions in 2010 and 2011, although some results from the literature are also used. Dust deposition generated by a global model serves as a reference against which the results from each observational strategy are compared. Observation-based dust fluxes disagree with one another by as much as two orders of magnitude, although most of the methods produce results that are consistent with the reference model to within a factor of 5. The large range of estimates indicates that further work is needed to reduce uncertainties associated with each method before it can be applied routinely to map dust deposition to the ocean. Calculated dust deposition using observational strategies thought to have the smallest uncertainties is lower than the reference model by a factor of 2-5, suggesting that the model may overestimate dust deposition in our study area.This article is part of the themed issue 'Biological and climatic impacts of ocean trace element chemistry'.
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Affiliation(s)
- R F Anderson
- Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY 10964, USA
- Department of Earth and Environmental Sciences, Columbia University, New York, NY 10027, USA
| | - H Cheng
- Department of Earth Sciences, University of Minnesota, Minneapolis, MN 55455, USA
- Institute of Global Environmental Change, Xi'an Jiaotong University, Xi'an, People's Republic of China
| | - R L Edwards
- Department of Earth Sciences, University of Minnesota, Minneapolis, MN 55455, USA
| | - M Q Fleisher
- Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY 10964, USA
| | - C T Hayes
- Department of Marine Science, University of Southern Mississippi, Stennis Space Center, MS 39529, USA
| | - K-F Huang
- Institute of Earth Sciences, Academia Sinica, Taipei, Taiwan, Republic of China
| | - D Kadko
- Applied Research Center, Florida International University, Miami, FL 33174, USA
| | - P J Lam
- Department of Ocean Sciences, University of California Santa Cruz, Santa Cruz, CA 95064, USA
| | - W M Landing
- Department of Earth, Ocean and Atmospheric Science, Florida State University, Tallahassee, FL 32306, USA
| | - Y Lao
- Department of Laboratory Services, Massachusetts Water Resources Authority, 190 Tafts Avenue, Winthrop, MA 02152, USA
| | - Y Lu
- Earth Observatory of Singapore, 50 Nanyang Avenue, Singapore 639798, Republic of Singapore
| | - C I Measures
- Department of Oceanography, University of Hawaii, Honolulu, HI 96822, USA
| | - S B Moran
- College of Fisheries and Ocean Sciences, University of Alaska Fairbanks, Fairbanks, AK 99775, USA
| | - P L Morton
- Department of Earth, Ocean and Atmospheric Science, Florida State University, Tallahassee, FL 32306, USA
| | - D C Ohnemus
- Bigelow Laboratory for Ocean Sciences, East Boothbay, ME 04544, USA
| | - L F Robinson
- School of Earth Sciences, University of Bristol, Queens Road, Bristol BS8 1RJ, UK
| | - R U Shelley
- LEMAR/UMR CNRS 6539/IUEM, Technopôle Brest-Iroise, Place Nicolas Copernic, Plouzané 29280, France
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Anderson RF, Cheng H, Edwards RL, Fleisher MQ, Hayes CT, Huang KF, Kadko D, Lam PJ, Landing WM, Lao Y, Lu Y, Measures CI, Moran SB, Morton PL, Ohnemus DC, Robinson LF, Shelley RU. How well can we quantify dust deposition to the ocean? Philos Trans A Math Phys Eng Sci 2016; 374:20150285. [PMID: 29035251 PMCID: PMC5069522 DOI: 10.1098/rsta.2015.0285] [Citation(s) in RCA: 6] [Impact Index Per Article: 0.8] [Reference Citation Analysis] [What about the content of this article? (0)] [Affiliation(s)] [Abstract] [Key Words] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Accepted: 08/10/2016] [Indexed: 05/09/2023]
Abstract
Deposition of continental mineral aerosols (dust) in the Eastern Tropical North Atlantic Ocean, between the coast of Africa and the Mid-Atlantic Ridge, was estimated using several strategies based on the measurement of aerosols, trace metals dissolved in seawater, particulate material filtered from the water column, particles collected by sediment traps and sediments. Most of the data used in this synthesis involve samples collected during US GEOTRACES expeditions in 2010 and 2011, although some results from the literature are also used. Dust deposition generated by a global model serves as a reference against which the results from each observational strategy are compared. Observation-based dust fluxes disagree with one another by as much as two orders of magnitude, although most of the methods produce results that are consistent with the reference model to within a factor of 5. The large range of estimates indicates that further work is needed to reduce uncertainties associated with each method before it can be applied routinely to map dust deposition to the ocean. Calculated dust deposition using observational strategies thought to have the smallest uncertainties is lower than the reference model by a factor of 2-5, suggesting that the model may overestimate dust deposition in our study area.This article is part of the themed issue 'Biological and climatic impacts of ocean trace element chemistry'.
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Affiliation(s)
- R F Anderson
- Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY 10964, USA
- Department of Earth and Environmental Sciences, Columbia University, New York, NY 10027, USA
| | - H Cheng
- Department of Earth Sciences, University of Minnesota, Minneapolis, MN 55455, USA
- Institute of Global Environmental Change, Xi'an Jiaotong University, Xi'an, People's Republic of China
| | - R L Edwards
- Department of Earth Sciences, University of Minnesota, Minneapolis, MN 55455, USA
| | - M Q Fleisher
- Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY 10964, USA
| | - C T Hayes
- Department of Marine Science, University of Southern Mississippi, Stennis Space Center, MS 39529, USA
| | - K-F Huang
- Institute of Earth Sciences, Academia Sinica, Taipei, Taiwan, Republic of China
| | - D Kadko
- Applied Research Center, Florida International University, Miami, FL 33174, USA
| | - P J Lam
- Department of Ocean Sciences, University of California Santa Cruz, Santa Cruz, CA 95064, USA
| | - W M Landing
- Department of Earth, Ocean and Atmospheric Science, Florida State University, Tallahassee, FL 32306, USA
| | - Y Lao
- Department of Laboratory Services, Massachusetts Water Resources Authority, 190 Tafts Avenue, Winthrop, MA 02152, USA
| | - Y Lu
- Earth Observatory of Singapore, 50 Nanyang Avenue, Singapore 639798, Republic of Singapore
| | - C I Measures
- Department of Oceanography, University of Hawaii, Honolulu, HI 96822, USA
| | - S B Moran
- College of Fisheries and Ocean Sciences, University of Alaska Fairbanks, Fairbanks, AK 99775, USA
| | - P L Morton
- Department of Earth, Ocean and Atmospheric Science, Florida State University, Tallahassee, FL 32306, USA
| | - D C Ohnemus
- Bigelow Laboratory for Ocean Sciences, East Boothbay, ME 04544, USA
| | - L F Robinson
- School of Earth Sciences, University of Bristol, Queens Road, Bristol BS8 1RJ, UK
| | - R U Shelley
- LEMAR/UMR CNRS 6539/IUEM, Technopôle Brest-Iroise, Place Nicolas Copernic, Plouzané 29280, France
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5
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Morton PL. Intraocular lens prostheses in cataract surgery. Can Fam Physician 1979; 25:593-597. [PMID: 21297741 PMCID: PMC2383079] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [What about the content of this article? (0)] [Abstract] [Subscribe] [Scholar Register] [Indexed: 05/30/2023]
Abstract
The introduction of intraocular lens prostheses presents some real advantages for aphakic patients, but these must be balanced against practical and theoretical objections. Indications include the patient's advancing age, inability to use contact lenses and the presence of monocular cataract. Contraindications include the young patient, the one-eyed patient, and the presence of any ocular disease known to prejudice success.
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