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A New Type of Plankton Food Web Functioning in Coastal Waters Revealed by Coupling Monte Carlo Markov Chain Linear Inverse Metho
A new type of plankton food web functioning in coastal waters revealed by coupling Monte Carlo Markov Chain Linear Inverse method and Ecological Network Analysis Marouan Meddeb, Nathalie Niquil, Boutheina Grami, Kaouther Mejri, Matilda Haraldsson, Aurélie Chaalali, Olivier Pringault, Asma Sakka Hlaili To cite this version: Marouan Meddeb, Nathalie Niquil, Boutheina Grami, Kaouther Mejri, Matilda Haraldsson, et al.. A new type of plankton food web functioning in coastal waters revealed by coupling Monte Carlo Markov Chain Linear Inverse method and Ecological Network Analysis. Ecological Indicators, Elsevier, 2019, 104, pp.67-85. 10.1016/j.ecolind.2019.04.077. hal-02146355 HAL Id: hal-02146355 https://hal.archives-ouvertes.fr/hal-02146355 Submitted on 3 Jun 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. 1 A new type of plankton food web functioning in coastal waters revealed by coupling 2 Monte Carlo Markov Chain Linear Inverse method and Ecological Network Analysis 3 4 5 Marouan Meddeba,b*, Nathalie Niquilc, Boutheïna Gramia,d, Kaouther Mejria,b, Matilda 6 Haraldssonc, Aurélie Chaalalic,e,f, Olivier Pringaultg, Asma Sakka Hlailia,b 7 8 aUniversité de Carthage, Faculté des Sciences de Bizerte, Laboratoire de phytoplanctonologie 9 7021 Zarzouna, Bizerte, Tunisie. -
Phytoplankton As Key Mediators of the Biological Carbon Pump: Their Responses to a Changing Climate
sustainability Review Phytoplankton as Key Mediators of the Biological Carbon Pump: Their Responses to a Changing Climate Samarpita Basu * ID and Katherine R. M. Mackey Earth System Science, University of California Irvine, Irvine, CA 92697, USA; [email protected] * Correspondence: [email protected] Received: 7 January 2018; Accepted: 12 March 2018; Published: 19 March 2018 Abstract: The world’s oceans are a major sink for atmospheric carbon dioxide (CO2). The biological carbon pump plays a vital role in the net transfer of CO2 from the atmosphere to the oceans and then to the sediments, subsequently maintaining atmospheric CO2 at significantly lower levels than would be the case if it did not exist. The efficiency of the biological pump is a function of phytoplankton physiology and community structure, which are in turn governed by the physical and chemical conditions of the ocean. However, only a few studies have focused on the importance of phytoplankton community structure to the biological pump. Because global change is expected to influence carbon and nutrient availability, temperature and light (via stratification), an improved understanding of how phytoplankton community size structure will respond in the future is required to gain insight into the biological pump and the ability of the ocean to act as a long-term sink for atmospheric CO2. This review article aims to explore the potential impacts of predicted changes in global temperature and the carbonate system on phytoplankton cell size, species and elemental composition, so as to shed light on the ability of the biological pump to sequester carbon in the future ocean. -
Fertilizing the Ocean with Iron Is This a Viable Way to Help Reduce Carbon Dioxide Levels in the Atmosphere?
380 Fertilizing the Ocean with Iron Is this a viable way to help reduce carbon dioxide levels in the atmosphere? 360 ive me half a tanker of iron, and I’ll give you an ice Twenty years on, Martin’s line is still viewed alternately age” may rank as the catchiest line ever uttered by a as a boast or a quip—an opportunity too good to pass up or a biogeochemist.“G The man responsible was the late John Martin, misguided remedy doomed to backfire. Yet over the same pe- former director of the Moss Landing Marine Laboratory, who riod, unrelenting increases in carbon emissions and mount- discovered that sprinkling iron dust in the right ocean waters ing evidence of climate change have taken the debate beyond could trigger plankton blooms the size of a small city. In turn, academic circles and into the free market. the billions of cells produced might absorb enough heat-trap- Today, policymakers, investors, economists, environ- ping carbon dioxide to cool the Earth’s warming atmosphere. mentalists, and lawyers are taking notice of the idea. A few Never mind that Martin companies are planning new, was only half serious when larger experiments. The ab- 340 he made the remark (in his Ocean Iron Fertilization sence of clear regulations for “best Dr. Strangelove accent,” either conducting experiments he later recalled) at an infor- An argument for: Faced with the huge at sea or trading the results mal seminar at Woods Hole consequences of climate change, iron’s in “carbon offset” markets Oceanographic Institution outsized ability to put carbon into the oceans complicates the picture. -
Biological Oceanography - Legendre, Louis and Rassoulzadegan, Fereidoun
OCEANOGRAPHY – Vol.II - Biological Oceanography - Legendre, Louis and Rassoulzadegan, Fereidoun BIOLOGICAL OCEANOGRAPHY Legendre, Louis and Rassoulzadegan, Fereidoun Laboratoire d'Océanographie de Villefranche, France. Keywords: Algae, allochthonous nutrient, aphotic zone, autochthonous nutrient, Auxotrophs, bacteria, bacterioplankton, benthos, carbon dioxide, carnivory, chelator, chemoautotrophs, ciliates, coastal eutrophication, coccolithophores, convection, crustaceans, cyanobacteria, detritus, diatoms, dinoflagellates, disphotic zone, dissolved organic carbon (DOC), dissolved organic matter (DOM), ecosystem, eukaryotes, euphotic zone, eutrophic, excretion, exoenzymes, exudation, fecal pellet, femtoplankton, fish, fish lavae, flagellates, food web, foraminifers, fungi, harmful algal blooms (HABs), herbivorous food web, herbivory, heterotrophs, holoplankton, ichthyoplankton, irradiance, labile, large planktonic microphages, lysis, macroplankton, marine snow, megaplankton, meroplankton, mesoplankton, metazoan, metazooplankton, microbial food web, microbial loop, microheterotrophs, microplankton, mixotrophs, mollusks, multivorous food web, mutualism, mycoplankton, nanoplankton, nekton, net community production (NCP), neuston, new production, nutrient limitation, nutrient (macro-, micro-, inorganic, organic), oligotrophic, omnivory, osmotrophs, particulate organic carbon (POC), particulate organic matter (POM), pelagic, phagocytosis, phagotrophs, photoautotorphs, photosynthesis, phytoplankton, phytoplankton bloom, picoplankton, plankton, -
Phytoplankton
Phytoplankton • What are the phytoplankton? • How do the main groups differ? Phytoplankton Zooplankton Nutrients Plankton “wandering” or “drifting” (incapable of sustained, directed horizontal movement) www.shellbackdon.com Nekton Active swimmers Components of the Plankton Virioplankton: Viruses Bacterioplankton: Bacteria — free living planktobacteria; epibacteria attached to larger particles Mycoplankton: Fungi Phytoplankton: Photosynthetic microalgae, cyanobacteria, and prochlorophytes Zooplankton: Heterotrophic — Protozooplankton (unicellular) and Metazooplankton (larval and adult crustaceans, larval fish, coelenterates…) Components of the Phytoplankton: Older scheme Netplankton: Plankton that is retained on a net or screen, usually Inspecting a small plankton 20 - 100 µm net. In: "From the Surface to the Bottom of the Sea" by H. Nanoplankton: Plankton that Bouree, 1912, Fig. 49, p. 61. passes the net, but Library Call Number 525.8 B77. which is > 2 µm Ultrananoplankton: Plankton < 2µm Components of the Plankton (older scheme) Netplankton: Plankton that is retained on a net or screen, usually 20 - 100 µm Nanoplankton: Plankton that passes the net, but which is > 2 µm Ultrananoplankton: Plankton < 2µm Microzooplankton: Zooplankton in the microplankton (i.e., < 200 µm) Length Scales to Define Plankton Groups Sieburth, J. M., Smetacek, V. and Lenz, J. (1978). Pelagic ecosystem structure: Heterotrophic compartments of the plankton and their relationship to plankton size fractions. Limnol. Oceanogr. 23: 1256-1263. Terminology and Scales: -
Collection and Analysis of a Global Marine Phytoplankton Primary
Discussions https://doi.org/10.5194/essd-2021-230 Earth System Preprint. Discussion started: 7 July 2021 Science c Author(s) 2021. CC BY 4.0 License. Open Access Open Data Collection and analysis of a global marine phytoplankton primary production dataset Franceso Mattei1,2,3, Michele Scardi1,2 1Department of Biology, University of Rome “Tor Vergata”, Via della Ricerca Scientifica (no street number), Rome, 00133, 5 Italy. 2CoNISMa, Piazzale Flaminio, 9, Rome, 00196, Italy. 3 Ph.D. Program in Evolutionary Biology and Ecology, Department of Biology, University of Rome Tor Vergata. Correspondence to: Francesco Mattei ([email protected]) Keywords: Phytoplankton primary production, Marine ecology, Global marine primary productivity. 10 Abstract. Phytoplankton primary production is a key oceanographic process. It has relationships with the marine food webs dynamics, the global carbon cycle and the Earth’s climate. The study of phytoplankton production on a global scale relies on indirect approaches due to field campaigns difficulties. Modelling approaches require in situ data for calibration and validation. In fact, the need for more phytoplankton primary production data was highlighted several times during the last decades. Most of the available primary production datasets are scattered in various repositories, reporting heterogeneous information 15 and missing records. We decided to retrieve field measurements of marine phytoplankton production from several sources and create a homogeneous and ready to use dataset. We handled missing data and added variables related to primary production which were not present in the original datasets. Subsequently, we performed a general analysis of the highlighting the relationships between the variables from a numerical and an ecological perspective. -
PHYTOPLANKTON Grass of The
S. G. No. 9 Oregon State University Extension Service Rev. December 1973 FIGURE 6: Oregon State Univer- sity's Marine Science Center in MARINE ADVISORY PROGRAM Newport, Oregon, is engaged in re- search, teaching, marine extension, and related activities under the Sea Grant Program of the National Oceanic and Atmospheric Adminis- tration. Located on Yaquina Bay, the center attracts thousands of visitors yearly to view the exhibits PHYTOPLANKTON of oceanographic phenomena and the aquaria of most of Oregon's marine fishes and invertebrates. Scientists studying the charac- grass of the sea teristics of life in the ocean (in- cluding phytoplankton) and in estu- aries work in various laboratories at the center. The Marine Science Center is home port for OSU School of Ocea- nography vessels, ranging in size from 180 to 33 feet (the 180-foot BY HERBERT CURL, JR. Yaquina and the 80-foot Cayuse PROFESSOR OF OCEANOGRAPHY are shown at the right). OREGON STATE UNIVERSITY Anyone taking a trip at sea or walking on the beach Want to Know More About Phytoplankton? Press, 1943—out of print; reprinted Ann Arbor: notices that nearshore water along coasts is frequently University Microfilms, Inc., University of Michigan). For the student or teacher who wishes to learn green or brown and sometimes even red. Often these more about phytoplankton, the following publications colors signify the presence of mud or silt carried into offer detailed information about phytoplankton and Want Other Marine Information? the sea by rivers or stirred up from the bottom if the their relationship to the ocean and mankind. Oregon State University's Extension Marine Advis- water is sufficiently shallow. -
Ocean Iron Fertilization Experiments – Past, Present, and Future Looking to a Future Korean Iron Fertilization Experiment in the Southern Ocean (KIFES) Project
Biogeosciences, 15, 5847–5889, 2018 https://doi.org/10.5194/bg-15-5847-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 3.0 License. Reviews and syntheses: Ocean iron fertilization experiments – past, present, and future looking to a future Korean Iron Fertilization Experiment in the Southern Ocean (KIFES) project Joo-Eun Yoon1, Kyu-Cheul Yoo2, Alison M. Macdonald3, Ho-Il Yoon2, Ki-Tae Park2, Eun Jin Yang2, Hyun-Cheol Kim2, Jae Il Lee2, Min Kyung Lee2, Jinyoung Jung2, Jisoo Park2, Jiyoung Lee1, Soyeon Kim1, Seong-Su Kim1, Kitae Kim2, and Il-Nam Kim1 1Department of Marine Science, Incheon National University, Incheon 22012, Republic of Korea 2Korea Polar Research Institute, Incheon 21990, Republic of Korea 3Woods Hole Oceanographic Institution, MS 21, 266 Woods Hold Rd., Woods Hole, MA 02543, USA Correspondence: Il-Nam Kim ([email protected]) Received: 2 November 2016 – Discussion started: 15 November 2016 Revised: 16 August 2018 – Accepted: 18 August 2018 – Published: 5 October 2018 Abstract. Since the start of the industrial revolution, hu- providing insight into mechanisms operating in real time and man activities have caused a rapid increase in atmospheric under in situ conditions. To maximize the effectiveness of carbon dioxide (CO2) concentrations, which have, in turn, aOIF experiments under international aOIF regulations in the had an impact on climate leading to global warming and future, we therefore suggest a design that incorporates sev- ocean acidification. Various approaches have been proposed eral components. (1) Experiments conducted in the center of to reduce atmospheric CO2. The Martin (or iron) hypothesis an eddy structure when grazing pressure is low and silicate suggests that ocean iron fertilization (OIF) could be an ef- levels are high (e.g., in the SO south of the polar front during fective method for stimulating oceanic carbon sequestration early summer). -
Plankton Biomass and Food Web Structure
Plankton Biomass and Food Web Structure Matthew Church OCN 621 Spring 2009 Food Web Structure is Central to Elemental Cycling “Microsystems” In every liter of seawater there are all the organisms for a complete, functional ecosystem. These organisms form the fabric of life in the sea - the other organisms are embroidery on this fabric. Important things to know about ocean ecosystems • Population size and biomass (biogenic carbon): provides information on energy available to support the food web • Growth, production, metabolism: turnover of material through the food web and insight into physiology. • Controls on growth and population size In a “typical” liter of seawater… •Fish None • Zooplankton 10 • Diatoms 1,000 • Dinoflagellates 10,000 • Nanoflagellates 1,000,000 • Cyanobacteria 100,000,000 • Prokaryotes 1,000,000,000 • Viruses 10,000,000,000 High abundance does not necessarily equate to high biomass. Size is important. 1011 1010 Viruses 109 Bacteria 108 Cyanobacteria 107 106 Protists 105 104 103 102 101 Phytoplankton 100 Abudance (number per liter)Abudance 10-1 Zooplankton 10-2 0.01 0.1 1 10 100 1000 Size (µm) Why are pelagic organisms so small? Consider a spherical cell: SA = 3.1 µm2 SA= 4πr2 r = 0.50 µm V = 0.52 µm3 SA : V = 15.7 V= 4/3 πr3 SA = 12.6 µm2 r = 1.0 V = 4.2 µm3 SA : V = 3.0 The smaller the cell, the larger the SA:V Greater SA:V increases their ability to absorb nutrients from a dilute solution. This may allow smaller cells to out compete larger cells for limiting nutrients. -
Great Plankton Sink Off Distance Learning Activity
Great Plankton Sink Off Distance Learning Activity Introduction: Explore the wonderful and diverse world of plankton and get creative by making your very own plankton. Learn about how these (mostly) microscopic organisms survive in the big blue ocean and the vital role they play in the ocean’s food web. This activity is great for all ages. Make sure to check out the guided activity video! Materials: • Large container of water (something with depth like a bucket, storage bin, etc.) • Stopwatch/ timer • Modeling clay or play dough broken up into quarter sized balls • Materials to build plankton (pipe cleaners, popsicle sticks, paper clips, beads, misc. craft supplies) • Paper/ white board for recording times Background: Plankton are a group of marine and freshwater organisms that drift through the water. Many of these plankton can swim but they are too small to move against a current. The word plankton comes from the Greek word “planktos” which means wandering. There are two types of plankton, phytoplankton and zooplankton. Phytoplankton are the plant like plankton. Like plants they photosynthesize to create food and oxygen. About 50% of the oxygen in our atmosphere is produced by phytoplankton. Phytoplankton is eaten zooplankton. Zooplankton are animal plankton and most ocean animals, including fish, crustaceans and mollusks, begin their lives with a planktonic stage. These tiny plants and animals are the base of the food web in the ocean. Plankton are eaten by many animals including crustaceans, fish, and even baleen whales. Phytoplankton Zooplankton • Plant like • Animal like • Photosynthesize to create food • Eat other organisms • Single celled organism • Single celled or multi-celled Don’t forget to share your plankton creation with us on Twitter or Instagram! Phytoplankton lives near the top of the ocean in an area called the photic zone to photosynthesize. -
Plankton Guide 2010.Pmd
GUIDE TO THE COMMON INSHORE of Southern California - 4th Edition Late megalopa larva of a crab. Robert Perry Malibu High School, and UCLA OceanGLOBE Condensed for public educational purposes from the textbook, Ocean Images: the Plankton, available online at www.Blurb.com name_______________________________________________________ rev. 2010-01 page 1 table of contents: PHYTOPLANKTON: PROTISTA: Diatoms . .. 3 PROTISTA: Dinoflagellates. 7 ZOOPLANKTON: PROTISTA: Protozoa . 10 ANIMALIA: Cnidaria . 11 Platyhelminthes . 12 Bryozoa . 13 Rotifera . 13 Polychaeta . 14 Mollusca . 15 Crustaceans Copepods . 16 Crustacean larvae . 17 Other holoplanktonic crustaceans . 18 Echinodermata . 19 Chordata . 20 CALCULATING THE ABUNDANCE OF PLANKTON PER CUBIC METER OF SEAWATER. 21 All photography © Robert Perry www.MarineBioPhotography.com All Rights Reserved. This booklet has been made available for non-profit, direct, face-to-face, educational purposes only. With special thanks to the crew of the R/V Sea World UCLA, 1995-2008. and the crew of the Condor Express, and the crew of the dive boat Peace. And a special thanks to the students who paddled for plankton at Zuma Beach as part of their research project at Malibu High School. Go Sharks ! page 2 PHYTOPLANKTON 1- Introduction to the Diatoms. Members of the Division Chrysophyta (or Bacillariophyta) are known as diatoms. The word “Diatom” comes from the Greek Dia, = across, and tom, = to cut. This refers to the fact that diatoms are enclosed within two glass (SiO2) shells which split across the middle and separate from each other during reproduction. One shell is older (the epitheca) and is slightly larger than the other, younger shell (the hypotheca). The smaller fits inside the larger like a “pill box” or Altoid® mint container. -
Ocean Primary Production
Learning Ocean Science through Ocean Exploration Section 6 Ocean Primary Production Photosynthesis very ecosystem requires an input of energy. The Esource varies with the system. In the majority of ocean ecosystems the source of energy is sunlight that drives photosynthesis done by micro- (phytoplankton) or macro- (seaweeds) algae, green plants, or photosynthetic blue-green or purple bacteria. These organisms produce ecosystem food that supports the food chain, hence they are referred to as primary producers. The balanced equation for photosynthesis that is correct, but seldom used, is 6CO2 + 12H2O = C6H12O6 + 6H2O + 6O2. Water appears on both sides of the equation because the water molecule is split, and new water molecules are made in the process. When the correct equation for photosynthe- sis is used, it is easier to see the similarities with chemo- synthesis in which water is also a product. Systems Lacking There are some ecosystems that depend on primary Primary Producers production from other ecosystems. Many streams have few primary producers and are dependent on the leaves from surrounding forests as a source of food that supports the stream food chain. Snow fields in the high mountains and sand dunes in the desert depend on food blown in from areas that support primary production. The oceans below the photic zone are a vast space, largely dependent on food from photosynthetic primary producers living in the sunlit waters above. Food sinks to the bottom in the form of dead organisms and bacteria. It is as small as marine snow—tiny clumps of bacteria and decomposing microalgae—and as large as an occasional bonanza—a dead whale.