Carlos Duarte | |
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Born | Carlos Manuel Duarte July 27, 1960 Lisbon, Portugal |
Nationality | Spanish |
Alma mater | Autonomous University of Madrid McGill University |
Known for | Malaspina Expedition 2010, Scientific Basis for Blue Carbon |
Scientific career | |
Fields | Biology, Ecology |
Institutions |
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Academic advisors | Jacob Kalff |
Carlos Manuel Duarte is a marine ecologist conducting research on marine ecosystems globally, from polar to the tropical ocean and from near-shore to deep-sea ecosystems. His research addresses biodiversity in the oceans, the impacts of human activity on marine ecosystems, and the capacity of marine ecosystems to recover from these impacts. He is also interested in transdisciplinary research, collaborating with scientists and engineers across a broad range of fields to solve problems in the marine ecosystem and society. He is currently a Distinguished Professor at the King Abdullah University of Science and Technology and executive director of the Coral Research and Development Accelerator Platform. [1]
Duarte earned a bachelor's degree in environmental biology from Autonomous University of Madrid, Spain, in 1982. In 1987, he obtained a Ph.D. in limnology from McGill University, advised by Jacob Kalff.
Upon receiving a Ph.D. in biology, Duarte returned to Spain where he was a postdoctoral researcher at the Instituto de Ciencias del Mar (1987–1989), to then take a position as staff researcher with the Spanish National Research Council therein, and move to the ranks to research professor while moving to the Blanes Centre for Advanced Studies (1989-1999), and to the Mediterranean Institute for Advanced Studies, Mallorca (1999–2015). In 2011 Duarte took the role of inaugural director, and Winthrop Professor, at the UWA Oceans Institute, University of Western Australia. In 2015 he joined the Biological and Environmental Science and Engineering Division and the Red Sea Research Center at King Abdullah University of Science and Technology, where he was appointed director of the Red Sea Research Center from 2016 to 2018. He also joined the Computational Biology Research Center there in 2017. He is the founding editor-in-chief of Frontiers in Marine Science], [2] and served or has served in the editorial board of multiple scientific journals. He has published over 900 scientific papers and many books and book chapters and supervised a large number of students and early career researchers. [3] He served as elected President of the American Society of Limnology and Oceanography, the largest professional society on marine sciences, and has received multiple awards and honors for his research contributions.
He has been recognized as a “Highly Cited Researcher”, demonstrated by the production of multiple highly cited papers that rank in the top 1% by citations for a research field, in all the assessments conducted thus far, including the 2018 assessment, [4] and in 2019 was ranked within the top 0.01% (ranked 887 among 7 million scientists evaluated) across all fields, the top ranked scientists in Marine Biology and Hydrology. [5] In 2021 Duarte was ranked, by Reuters, as the 12th most influential climate scientist in the world. [6] He was also ranked the 4th top scientist in Ecology and Evolution, and the top marine scientist in their rank. [7] Since 2021 Duarte also serves as executive director for the Global Coral R&D Accelerator Platform, CORDAP. On October 27, 2021, Prof. Duarte has been appointed Academic with the Spanish Royal Academy of Sciences for his seminal contributions to further understanding marine ecosystems and their responses to global change. [8]
Duarte was originally trained as a limnologist and has contributed to understanding the ecology of freshwater plants in rivers and lakes, as well as the role of freshwater ecosystems in carbon cycling. His research in the ecology and biogeochemistry of seagrass meadows and other vegetated coastal systems eventually lead – in collaboration with different UN agencies - to the development of “Blue carbon” strategies to mitigate climate change. [9] [10] [11] Recognizing the many gaps in our understanding of the deep-sea pelagic ecosystem, Duarte led the Malaspina Circumnavigation Expedition, involving more than 500 scientists, and that sailed the oceans between 2010 and 2011 to provide a global assessment of the deep-sea pelagic ecosystem. The Malaspina Expedition 2010 has thus far released over 200 publications addressing different aspects of the biodiversity and function of the deep-sea ecosystem. [12] [13] [14] [15] [16] [17] [18] [19] [20] [21] In 2020, Duarte led an international team that, on the basis of evidences of responses of marine populations and habitats to the release of pressures, concluded that rebuilding the abundance of marine life by 2050 is an achievable Grand Challenge, and provided a road map to deliver this goal. [22]
Top 10 most cited papers of > 900 published papers:
Marine biology is the scientific study of the biology of marine life, organisms in the sea. Given that in biology many phyla, families and genera have some species that live in the sea and others that live on land, marine biology classifies species based on the environment rather than on taxonomy.
Zooplankton are the animal component of the planktonic community, having to consume other organisms to thrive. Plankton are aquatic organisms that are unable to swim effectively against currents. Consequently, they drift or are carried along by currents in the ocean, or by currents in seas, lakes or rivers.
Seagrasses are the only flowering plants which grow in marine environments. There are about 60 species of fully marine seagrasses which belong to four families, all in the order Alismatales. Seagrasses evolved from terrestrial plants which recolonised the ocean 70 to 100 million years ago.
The mesopelagiczone, also known as the middle pelagic or twilight zone, is the part of the pelagic zone that lies between the photic epipelagic and the aphotic bathypelagic zones. It is defined by light, and begins at the depth where only 1% of incident light reaches and ends where there is no light; the depths of this zone are between approximately 200 to 1,000 meters below the ocean surface.
The bathypelagic zone or bathyal zone is the part of the open ocean that extends from a depth of 1,000 to 4,000 m below the ocean surface. It lies between the mesopelagic above and the abyssopelagic below. The bathypelagic is also known as the midnight zone because of the lack of sunlight; this feature does not allow for photosynthesis-driven primary production, preventing growth of phytoplankton or aquatic plants. Although larger by volume than the photic zone, human knowledge of the bathypelagic zone remains limited by ability to explore the deep ocean.
A seagrass meadow or seagrass bed is an underwater ecosystem formed by seagrasses. Seagrasses are marine (saltwater) plants found in shallow coastal waters and in the brackish waters of estuaries. Seagrasses are flowering plants with stems and long green, grass-like leaves. They produce seeds and pollen and have roots and rhizomes which anchor them in seafloor sand.
Sallie Watson "Penny" Chisholm is an American biological oceanographer at the Massachusetts Institute of Technology. She is an expert in the ecology and evolution of ocean microbes. Her research focuses particularly on the most abundant marine phytoplankton, Prochlorococcus, that she discovered in the 1980s with Rob Olson and other collaborators. She has a TED talk about their discovery and importance called "The tiny creature that secretly powers the planet".
Neuston, also called pleuston, are organisms that live at the surface of a body of water, such as an ocean, estuary, lake, river, or pond. Neuston can live on top of the water surface or may be attached to the underside of the water surface. They may also exist in the surface microlayer that forms between the top side and the underside. Neuston have been defined as "organisms living at the air/water interface of freshwater, estuarine, and marine habitats or referring to the biota on or directly below the water’s surface layer."
Gelatinous zooplankton are fragile animals that live in the water column in the ocean. Their delicate bodies have no hard parts and are easily damaged or destroyed. Gelatinous zooplankton are often transparent. All jellyfish are gelatinous zooplankton, but not all gelatinous zooplankton are jellyfish. The most commonly encountered organisms include ctenophores, medusae, salps, and Chaetognatha in coastal waters. However, almost all marine phyla, including Annelida, Mollusca and Arthropoda, contain gelatinous species, but many of those odd species live in the open ocean and the deep sea and are less available to the casual ocean observer. Many gelatinous plankters utilize mucous structures in order to filter feed. Gelatinous zooplankton have also been called Gelata.
Picoeukaryotes are picoplanktonic eukaryotic organisms 3.0 µm or less in size. They are distributed throughout the world's marine and freshwater ecosystems and constitute a significant contribution to autotrophic communities. Though the SI prefix pico- might imply an organism smaller than atomic size, the term was likely used to avoid confusion with existing size classifications of plankton.
In the deep ocean, marine snow is a continuous shower of mostly organic detritus falling from the upper layers of the water column. It is a significant means of exporting energy from the light-rich photic zone to the aphotic zone below, which is referred to as the biological pump. Export production is the amount of organic matter produced in the ocean by primary production that is not recycled (remineralised) before it sinks into the aphotic zone. Because of the role of export production in the ocean's biological pump, it is typically measured in units of carbon. The term was coined by explorer William Beebe as observed from his bathysphere. As the origin of marine snow lies in activities within the productive photic zone, the prevalence of marine snow changes with seasonal fluctuations in photosynthetic activity and ocean currents. Marine snow can be an important food source for organisms living in the aphotic zone, particularly for organisms that live very deep in the water column.
Blue carbon is a term used in the climate change mitigation context that refers to "biologically driven carbon fluxes and storage in marine systems that are amenable to management." Most commonly, it refers to the role that tidal marshes, mangroves and seagrasses can play in carbon sequestration. Such ecosystems can contribute to climate change mitigation and also to ecosystem-based adaptation. When blue carbon ecosystems are degraded or lost they release carbon back to the atmosphere.
Alexandra (Alex) Z. Worden is a microbial ecologist and genome scientist known for her expertise in the ecology and evolution of ocean microbes and their influence on global biogeochemical cycles.
The viral shunt is a mechanism that prevents marine microbial particulate organic matter (POM) from migrating up trophic levels by recycling them into dissolved organic matter (DOM), which can be readily taken up by microorganisms. The DOM recycled by the viral shunt pathway is comparable to the amount generated by the other main sources of marine DOM.
Adina Paytan is a research professor at the Institute of Marine Sciences at the University of California, Santa Cruz. known for research into biogeochemical cycling in the present and the past. She has over 270 scientific publications in journals such as Science, Nature, Proceedings of the National Academy of Sciences, and Geophysical Research Letters.
Marine primary production is the chemical synthesis in the ocean of organic compounds from atmospheric or dissolved carbon dioxide. It principally occurs through the process of photosynthesis, which uses light as its source of energy, but it also occurs through chemosynthesis, which uses the oxidation or reduction of inorganic chemical compounds as its source of energy. Almost all life on Earth relies directly or indirectly on primary production. The organisms responsible for primary production are called primary producers or autotrophs.
Trevor Charles Platt was a British and Canadian biological oceanographer who was distinguished for his fundamental contributions to quantifying primary production by phytoplankton at various scales of space and time in the ocean.
Jean-Pierre Gattuso is a French ocean scientist conducting research globally, from the pole to the tropics and from nearshore to the open ocean. His research addresses the biology of reef-building corals, the biogeochemistry of coastal ecosystems, and the response of marine plants, animals and ecosystems to global environmental change. He is also interested in transdisciplinary research, collaborating with social scientists to address ocean-based solutions to minimize climate change and its impacts. He is currently a CNRS Research Professor at Sorbonne University.
A marine coastal ecosystem is a marine ecosystem which occurs where the land meets the ocean. Marine coastal ecosystems include many very different types of marine habitats, each with their own characteristics and species composition. They are characterized by high levels of biodiversity and productivity.
Shubha Platt, known professionally as Shubha Sathyendranath, is a marine scientist known for her work on marine optics and remote sensing of ocean colour. She is the 2021 recipient of the A.G. Huntsman Award for Excellence in the Marine Sciences.
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