Meinrat O. Andreae, born in 1949 in Augsburg, is a German biogeochemist. Since 1987, he has worked as Director and Scientific Member at the Max Planck Institute for Chemistry (MPIC) in Mainz. [1]
Meinrat O. Andreae studied chemistry, mineralogy, and geochemistry at the Universities of Karlsruhe and Göttingen. In his diploma thesis, he studied the chemical composition and isotope geochemistry of highly metamorphic rocks of southern Norway. In 1977, he completed his PhD in oceanography from the Scripps Institution of Oceanography at the University of California at San Diego. In his doctoral thesis, he examined the chemical speciation of arsenic in the ocean. He discovered that planktonic algae regulate the oxidation state of arsenic in seawater and synthesize a variety of organoarsenic compounds. A secondary discovery of his work was that marine phytoplankton also manufactures the raw materials for the volatile sulfur compound dimethyl sulfide.
Andreae taught oceanography in the Department of Oceanography at Florida State University in Tallahassee, from 1978 until 1982 as an assistant professor, then from 1982 to 1986 as associate professor, and from 1986 to 1987 as full professor. During this time he researched the biogeochemical cycle of sulfur in the ocean and in the atmosphere. Along with Robert Jay Charlson, James Lovelock, and Stephen G. Warren, he developed the CLAW hypothesis, named after the initials of the authors. This hypothesis states that dimethyl sulfide from the ocean is converted in the atmosphere to sulfate particles, which then influence the formation of clouds and therefore the climate. Other works from this period were concerned with biogeochemical transformations of compounds of arsenic, antimony, selenium, tellurium and tin in the marine and terrestrial ecosystems. In the 1980s, he was together with Paul Crutzen one of the first scientists to discover the worldwide importance of biomass burning.
In 1987 he was appointed member of the Max Planck Institute for Chemistry (MPIC) in Mainz as director and scientific member. He initiated the Biogeochemistry Department at the MPIC and designed a broad research agenda on the chemical aspects of Earth System Science. There, he continued his work on biogeochemical cycles of trace metals, and extended his studies to the formation of aerosols from marine sulfur emissions. Campaigns in the Amazon forest then led to a new focus, the biogeochemical processes of exchange between tropical forests and the atmosphere. On expeditions in the Congo, the Amazon, and Southern Africa he studied the emissions from vegetation fires, the exchange of trace gases, and the production of biogenic aerosol particles. Since 2000, research into the role of atmospheric aerosols in the climate system has been at the center of Andreae's research. In 2009, he set up a new working group, applying methods of isotope geochemistry and mass spectrometry to problems of paleoclimatology and marine biogeochemistry.
As a visiting professor, Andreae taught at the University of Antwerp, the National Center for Atmospheric Research in Boulder, the University of California, Irvine and the California Institute of Technology in Pasadena. He is a member of the scientific steering committee of the Large Scale Biosphere Atmosphere Experiment in Amazonia (LBA) and was chairman of the IGBP's Integrated land Ecosystem Atmospheric Processes Study (ILEAPS). In addition, Andreae is a reviewing editor of the journal Science. In 2009 he became a fellow of the American Association for the Advancement of Science, [2] in 2012 he became a Foreign Member of the Brazilian Academy of Arts and Sciences, in 2013 he was elected as a Foreign Honorary Member of the American Academy of Arts and Sciences, [3] and in 2014 he was awarded the Waldo E. Smith Medal [4] and became a fellow of the American Geophysical Union. In 2010, Andreae was awarded the degree of Doctor honoris causa by the Ghent University in Belgium.
Meinrat O. Andreae and his coworkers have published nearly 500 articles in scientific journals and books.
The scientists of the MPIC Department of Biogeochemistry, in close cooperation with the Departments of Atmospheric Chemistry and Multiphase Chemistry, study interactions between the atmosphere and biosphere of our planet. The results of these studies contribute to the understanding of global biogeochemical cycles, global climate processes, and the impact of mankind on these processes.
A biogeochemical cycle, or more generally a cycle of matter, is the movement and transformation of chemical elements and compounds between living organisms, the atmosphere, and the Earth's crust. Major biogeochemical cycles include the carbon cycle, the nitrogen cycle and the water cycle. In each cycle, the chemical element or molecule is transformed and cycled by living organisms and through various geological forms and reservoirs, including the atmosphere, the soil and the oceans. It can be thought of as the pathway by which a chemical substance cycles the biotic compartment and the abiotic compartments of Earth. The biotic compartment is the biosphere and the abiotic compartments are the atmosphere, lithosphere and hydrosphere.
Cloud condensation nuclei (CCNs), also known as cloud seeds, are small particles typically 0.2 μm, or one hundredth the size of a cloud droplet. CCNs are a unique subset of aerosols in the atmosphere on which water vapour condenses. This can affect the radiative properties of clouds and the overall atmosphere. Water vapour requires a non-gaseous surface to make the transition to a liquid; this process is called condensation.
Biogeochemistry is the scientific discipline that involves the study of the chemical, physical, geological, and biological processes and reactions that govern the composition of the natural environment. In particular, biogeochemistry is the study of biogeochemical cycles, the cycles of chemical elements such as carbon and nitrogen, and their interactions with and incorporation into living things transported through earth scale biological systems in space and time. The field focuses on chemical cycles which are either driven by or influence biological activity. Particular emphasis is placed on the study of carbon, nitrogen, oxygen, sulfur, iron, and phosphorus cycles. Biogeochemistry is a systems science closely related to systems ecology.
The Surface Ocean Lower Atmosphere Study (SOLAS) is a global and multidisciplinary research project dedicated to understanding the key biogeochemical-physical interactions and feedbacks between the ocean and the atmosphere. Further, SOLAS seeks to link ocean-atmosphere interactions with climate and people. Achievements of these goals are essential in order to understand and quantify the role that ocean-atmosphere interactions play in the regulation of climate and global change.
The iron cycle (Fe) is the biogeochemical cycle of iron through the atmosphere, hydrosphere, biosphere and lithosphere. While Fe is highly abundant in the Earth's crust, it is less common in oxygenated surface waters. Iron is a key micronutrient in primary productivity, and a limiting nutrient in the Southern ocean, eastern equatorial Pacific, and the subarctic Pacific referred to as High-Nutrient, Low-Chlorophyll (HNLC) regions of the ocean.
Dimethyl sulfide (DMS) or methylthiomethane is an organosulfur compound with the formula (CH3)2S. It is the simplest thioether and has a characteristic disagreeable odor. It is a flammable liquid that boils at 37 °C (99 °F). It is a component of the smell produced from cooking of certain vegetables, notably maize, cabbage, beetroot, and seafoods. It is also an indication of bacterial contamination in malt production and brewing. It is a breakdown product of dimethylsulfoniopropionate (DMSP), and is also produced by the bacterial metabolism of methanethiol.
The Max Planck Institute for Chemistry is a non-university research institute under the auspices of the Max Planck Society in Mainz, Germany. It was created as the Kaiser Wilhelm Institute for Chemistry in 1911 in Berlin.
The CLAW hypothesis proposes a negative feedback loop that operates between ocean ecosystems and the Earth's climate. The hypothesis specifically proposes that particular phytoplankton that produce dimethyl sulfide are responsive to variations in climate forcing, and that these responses act to stabilise the temperature of the Earth's atmosphere. The CLAW hypothesis was originally proposed by Robert Jay Charlson, James Lovelock, Meinrat Andreae and Stephen G. Warren, and takes its acronym from the first letter of their surnames.
Marine chemistry, also known as ocean chemistry or chemical oceanography, is the study of the chemical composition and processes of the world’s oceans, including the interactions between seawater, the atmosphere, the seafloor, and marine organisms. This field encompasses a wide range of topics, such as the cycling of elements like carbon, nitrogen, and phosphorus, the behavior of trace metals, and the study of gases and nutrients in marine environments. Marine chemistry plays a crucial role in understanding global biogeochemical cycles, ocean circulation, and the effects of human activities, such as pollution and climate change, on oceanic systems. It is influenced by plate tectonics and seafloor spreading, turbidity, currents, sediments, pH levels, atmospheric constituents, metamorphic activity, and ecology.
Ulrich "Uli" Pöschl is an Austrian chemist who was appointed Director of the newly founded Department of Multiphase Chemistry at the Max Planck Institute for Chemistry in Mainz, Germany on 1 October 2012.
Mary Ann Moran is a distinguished research professor of marine sciences at the University of Georgia in Athens. She studies the role of bacteria in Earth's marine nutrient cycles, and is a leader in the fields of marine sciences and biogeochemistry. Her work is focused on how microbes interact with dissolved organic matter and the impact of microbial diversity on the global carbon and sulfur cycles. By defining the roles of diverse bacteria in the carbon and sulfur cycles, she connects the biogeochemical and organismal approaches in marine science.
Marine biogeochemical cycles are biogeochemical cycles that occur within marine environments, that is, in the saltwater of seas or oceans or the brackish water of coastal estuaries. These biogeochemical cycles are the pathways chemical substances and elements move through within the marine environment. In addition, substances and elements can be imported into or exported from the marine environment. These imports and exports can occur as exchanges with the atmosphere above, the ocean floor below, or as runoff from the land.
Jennifer G. Murphy is a Canadian environmental chemist and an associate professor at the University of Toronto. She is known for her research how air pollutants such as increased reactive nitrogen affect the global climate.
The North Atlantic Aerosols and Marine Ecosystems Study (NAAMES) was a five-year scientific research program that investigated aspects of phytoplankton dynamics in ocean ecosystems, and how such dynamics influence atmospheric aerosols, clouds, and climate. The study focused on the sub-arctic region of the North Atlantic Ocean, which is the site of one of Earth's largest recurring phytoplankton blooms. The long history of research in this location, as well as relative ease of accessibility, made the North Atlantic an ideal location to test prevailing scientific hypotheses in an effort to better understand the role of phytoplankton aerosol emissions on Earth's energy budget.
Nadine Unger is a Professor of Atmospheric Chemistry at the University of Exeter. She has studied the role of human activities and forests on the Earth's climate.
Eugen Seibold is a German research vessel designed for contamination-free sampling of seawater, plankton, and air. Starting from 2018, exchange processes between atmosphere and ocean are studied. The vessel has been funded by the Werner Siemens Foundation and is operated by the Max Planck Institute for Chemistry (MPI) in Mainz.
The arsenic (As) cycle is the biogeochemical cycle of natural and anthropogenic exchanges of arsenic terms through the atmosphere, lithosphere, pedosphere, hydrosphere, and biosphere. Although arsenic is naturally abundant in the Earth's crust, long-term exposure and high concentrations of arsenic can be detrimental to human health.
The Scientific Committee on Oceanic Research (SCOR) is an interdisciplinary body of the International Science Council. SCOR was established in 1957, coincident with the International Geophysical Year of 1957-1958. It sought to bring scientists together to answer key ocean science questions and improve opportunities for marginalised scientists.
Colin Dermot O'Dowd is an Irish physicist and atmospheric scientist.
Patricia Ana Matrai is a marine scientist known for her work on the cycling of sulfur. She is a senior research scientist at Bigelow Laboratory for Ocean Sciences.