Maureen Conte

Last updated
Maureen Conte
Alma materColumbia University
Scientific career
Thesis The biogeochemistry of particulate lipids in warm-core Gulf Stream ring systems  (1990)

Maureen Hatcher Conte is biogeochemist known for her work using particles to define the long-term cycling of chemical compounds in seawater.

Contents

Education and career

Conte has a B.A. from Johns Hopkins University (1975), and an M.A. (1982), M.Phil. (1987), and Ph.D. (1989) from Columbia University. [1] Her Ph.D. examined lipids found in particles in the Gulf Stream. [2] Following her Ph.D. she conducted postdoctoral work at the University of Bristol before joining Woods Hole Oceanographic Institution in 1994. As of 2022 Conte is a senior scientist at the Bermuda Institute of Ocean Sciences and a fellow at the Marine Biological Laboratory. [3] Conte is the lead investigator for the Ocean Flux Program, [1] a program that has been examining particles in the Sargasso Sea since 1978. [4] [5]

Research

Conte is known for her work on the organic compounds found in particles. [6] Her early work examined the consumption of organic matter, [7] and the development of methods to analyze lipids from seawater. [8] [9] Subsequently, she examined the different types of lipids found in organisms such as coccolithophores. [10] [11] At the Bermuda Atlantic Time-series Study site, Conte has used long-term measurements of particles to quantify changes in the flux of organic carbon to the seafloor over time, [12] [13] and used the presence of alkenones in particles to track changes in ocean temperatures over time. [14] [15] Through her research she has characterized how hurricanes impact the flow of organic carbon to the seafloor, [16] [17] and examined the impact of cold shock on sea turtles that are trapped in cold waters off Cape Cod. [18] Conte's research involves spending extended periods of time on research ships, [19] and in 2020, her research was delayed because she could not collect her samples due to the COVID-19 pandemic. [20]

Selected publications

Related Research Articles

<span class="mw-page-title-main">Coccolithophore</span> Unicellular algae responsible for the formation of chalk

Coccolithophores, or coccolithophorids, are single-celled organisms which are part of the phytoplankton, the autotrophic (self-feeding) component of the plankton community. They form a group of about 200 species, and belong either to the kingdom Protista, according to Robert Whittaker's five-kingdom system, or clade Hacrobia, according to a newer biological classification system. Within the Hacrobia, the coccolithophores are in the phylum or division Haptophyta, class Prymnesiophyceae. Coccolithophores are almost exclusively marine, are photosynthetic, and exist in large numbers throughout the sunlight zone of the ocean.

<span class="mw-page-title-main">Biological pump</span> Carbon capture process in oceans

The biological pump (or ocean carbon biological pump or marine biological carbon pump) is the ocean's biologically driven sequestration of carbon from the atmosphere and land runoff to the ocean interior and seafloor sediments. In other words, it is a biologically mediated process which results in the sequestering of carbon in the deep ocean away from the atmosphere and the land. The biological pump is the biological component of the "marine carbon pump" which contains both a physical and biological component. It is the part of the broader oceanic carbon cycle responsible for the cycling of organic matter formed mainly by phytoplankton during photosynthesis (soft-tissue pump), as well as the cycling of calcium carbonate (CaCO3) formed into shells by certain organisms such as plankton and mollusks (carbonate pump).

<span class="mw-page-title-main">Coccolith</span>

Coccoliths are individual plates or scales of calcium carbonate formed by coccolithophores and cover the cell surface arranged in the form of a spherical shell, called a coccosphere.

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.

<i>Emiliania huxleyi</i> Unicellular algae responsible for the formation of chalk

Emiliania huxleyi is a species of coccolithophore found in almost all ocean ecosystems from the equator to sub-polar regions, and from nutrient rich upwelling zones to nutrient poor oligotrophic waters. It is one of thousands of different photosynthetic plankton that freely drift in the photic zone of the ocean, forming the basis of virtually all marine food webs. It is studied for the extensive blooms it forms in nutrient-depleted waters after the reformation of the summer thermocline. Like other coccolithophores, E. huxleyi is a single-celled phytoplankton covered with uniquely ornamented calcite disks called coccoliths. Individual coccoliths are abundant in marine sediments although complete coccospheres are more unusual. In the case of E. huxleyi, not only the shell, but also the soft part of the organism may be recorded in sediments. It produces a group of chemical compounds that are very resistant to decomposition. These chemical compounds, known as alkenones, can be found in marine sediments long after other soft parts of the organisms have decomposed. Alkenones are most commonly used by earth scientists as a means to estimate past sea surface temperatures.

Paleoceanography is the study of the history of the oceans in the geologic past with regard to circulation, chemistry, biology, geology and patterns of sedimentation and biological productivity. Paleoceanographic studies using environment models and different proxies enable the scientific community to assess the role of the oceanic processes in the global climate by the re-construction of past climate at various intervals. Paleoceanographic research is also intimately tied to paleoclimatology.

Alkenones are long-chain unsaturated methyl and ethyl n-ketones produced by a few phytoplankton species of the class Prymnesiophyceae. Alkenones typically contain between 35 and 41 carbon atoms and with between two and four double bonds. Uniquely for biolipids, alkenones have a spacing of five methylene groups between double bonds, which are of the less common E configuration. The biological function of alkenones remains under debate although it is likely that they are storage lipids. Alkenones were first described in ocean sediments recovered from Walvis Ridge and then shortly afterwards in cultures of the marine coccolithophore Emiliania huxleyi. The earliest known occurrence of alkenones is during the Aptian 120 million years ago. They are used in organic geochemistry as a proxy for past sea surface temperature.

<span class="mw-page-title-main">Cariaco Basin</span>

The Cariaco Basin lies off the north central coast of Venezuela and forms the Gulf of Cariaco. It is bounded on the east by Margarita Island, Cubagua Island, and the Araya Peninsula; on the north by Tortuga Island and the Tortuga Banks; on the west by Cape Codera and the rocks known as Farallón Centinela; and on the south by the coast of Venezuela.

<span class="mw-page-title-main">Diel vertical migration</span> A pattern of daily vertical movement characteristic of many aquatic species

Diel vertical migration (DVM), also known as diurnal vertical migration, is a pattern of movement used by some organisms, such as copepods, living in the ocean and in lakes. The word "diel" comes from Latin: diēs, lit. 'day', and means a 24-hour period. The migration occurs when organisms move up to the uppermost layer of the sea at night and return to the bottom of the daylight zone of the oceans or to the dense, bottom layer of lakes during the day. It is important to the functioning of deep-sea food webs and the biologically driven sequestration of carbon.

<span class="mw-page-title-main">Oceanic carbon cycle</span> Ocean/atmosphere carbon exchange process

The oceanic carbon cycle is composed of processes that exchange carbon between various pools within the ocean as well as between the atmosphere, Earth interior, and the seafloor. The carbon cycle is a result of many interacting forces across multiple time and space scales that circulates carbon around the planet, ensuring that carbon is available globally. The Oceanic carbon cycle is a central process to the global carbon cycle and contains both inorganic carbon and organic carbon. Part of the marine carbon cycle transforms carbon between non-living and living matter.

<span class="mw-page-title-main">Mode water</span> Type of water mass which is nearly vertically homogeneous

Mode water is defined as a particular type of water mass, which is nearly vertically homogeneous. Its vertical homogeneity is caused by the deep vertical convection in winter. The first term to describe this phenomenon is 18° water, which was used by Valentine Worthington to describe the isothermal layer in the northern Sargasso Sea cool to a temperature of about 18 °C each winter. Then Masuzawa introduced the subtropical mode water concept to describe the thick layer of temperature 16–18 °C in the northwestern North Pacific subtropical gyre, on the southern side of the Kuroshio Extension. The terminology mode water was extended to the thick near-surface layer north of the Subantarctic Front by McCartney, who identified and mapped the properties of the Subantarctic mode water (SAMW). After that, McCartney and Talley then applied the term subpolar mode water (SPMW) to the thick near-surface mixed layers in the North Atlantic’s subpolar gyre.

<span class="mw-page-title-main">Particulate organic matter</span>

Particulate organic matter (POM) is a fraction of total organic matter operationally defined as that which does not pass through a filter pore size that typically ranges in size from 0.053 millimeters (53 μm) to 2 millimeters.

<span class="mw-page-title-main">Lipid pump</span>

The lipid pump sequesters carbon from the ocean's surface to deeper waters via lipids associated with overwintering vertically migratory zooplankton. Lipids are a class of hydrocarbon rich, nitrogen and phosphorus deficient compounds essential for cellular structures. This lipid carbon enters the deep ocean as carbon dioxide produced by respiration of lipid reserves and as organic matter from the mortality of zooplankton.

Cindy Lee is a retired Distinguished Professor known for her research characterizing the compounds that comprise marine organic matter.

<span class="mw-page-title-main">Particulate inorganic carbon</span>

Particulate inorganic carbon (PIC) can be contrasted with dissolved inorganic carbon (DIC), the other form of inorganic carbon found in the ocean. These distinctions are important in chemical oceanography. Particulate inorganic carbon is sometimes called suspended inorganic carbon. In operational terms, it is defined as the inorganic carbon in particulate form that is too large to pass through the filter used to separate dissolved inorganic carbon.

<span class="mw-page-title-main">Great Calcite Belt</span> High-calcite region of the Southern Ocean

The Great Calcite Belt (GCB) refers to a region of the ocean where there are high concentrations of calcite, a mineral form of calcium carbonate. The belt extends over a large area of the Southern Ocean surrounding Antarctica. The calcite in the Great Calcite Belt is formed by tiny marine organisms called coccolithophores, which build their shells out of calcium carbonate. When these organisms die, their shells sink to the bottom of the ocean, and over time, they accumulate to form a thick layer of calcite sediment.

<span class="mw-page-title-main">Martin curve</span> Mathematical representation of particulate organic carbon export to ocean floor

The Martin curve is a power law used by oceanographers to describe the export to the ocean floor of particulate organic carbon (POC). The curve is controlled with two parameters: the reference depth in the water column, and a remineralisation parameter which is a measure of the rate at which the vertical flux of POC attenuates. It is named after the American oceanographer John Martin.

Low-nutrient, low-chlorophyll (LNLC)regions are aquatic zones that are low in nutrients and consequently have low rate of primary production, as indicated by low chlorophyll concentrations. These regions can be described as oligotrophic, and about 75% of the world's oceans encompass LNLC regions. A majority of LNLC regions are associated with subtropical gyres but are also present in areas of the Mediterranean Sea, and some inland lakes. Physical processes limit nutrient availability in LNLC regions, which favors nutrient recycling in the photic zone and selects for smaller phytoplankton species. LNLC regions are generally not found near coasts, owing to the fact that coastal areas receive more nutrients from terrestrial sources and upwelling. In marine systems, seasonal and decadal variability of primary productivity in LNLC regions is driven in part by large-scale climatic regimes leading to important effects on the global carbon cycle and the oceanic carbon cycle.

Hilairy Ellen Hartnett is professor at Arizona State University known for her work on biogeochemical processes in modern and paleo-environments.

Elisabeth Lynn Sikes is an American geoscientist who is a professor at Rutgers University. Her research considers carbon cycling. She was awarded the 2022 Scientific Committee on Antarctic Research Medal for Excellence in Research.

References

  1. 1 2 "Dr. Maureen Conte | Team Members | About BIOS | BIOS - Bermuda Institute of Ocean Sciences". www.bios.edu. Retrieved 2022-04-09.
  2. Conte, Maureen Hatcher (1991). The biogeochemistry of particulate lipids in warm-core Gulf Stream ring systems (Thesis). OCLC   82869924.
  3. "Conte CV" (PDF). Retrieved April 9, 2022.
  4. Conte, Maureen; Weber, JC (2014-03-01). "Particle Flux in the Deep Sargasso Sea: The 35-Year Oceanic Flux Program Time Series". Oceanography. 27 (1): 142–147. doi: 10.5670/oceanog.2014.17 . hdl: 1912/6582 . ISSN   1042-8275.
  5. Earle, Sylvia A.; Glover, Linda; Glover, Linda K. (2009). Ocean: An Illustrated Atlas. National Geographic Books. p. 121. ISBN   978-1-4262-0319-0.
  6. "Autobiographical Sketches of Women in Oceanography". Oceanography. 18 (1): 97. March 2005.
  7. Bishop, J.K.B.; Conte, M.H.; Wiebe, P.H.; Roman, M.R.; Langdon, C. (1986). "Particulate matter production and consumption in deep mixed layers: observations in a warm-core ring". Deep Sea Research Part A. Oceanographic Research Papers. 33 (11–12): 1813–1841. Bibcode:1986DSRA...33.1813B. doi:10.1016/0198-0149(86)90081-6.
  8. Conte, Maureen H.; Bishop, James K. B. (1988). "Nanogram quantification of nonpolar lipid classes in environmental samples by high performance thin layer chromatography". Lipids. 23 (5): 493–500. doi:10.1007/BF02535526. ISSN   0024-4201. S2CID   31322887.
  9. Conte, Maureen H.; Eglinton, Geoffrey; Madureira, Luiz A.S. (1992). "Long-chain alkenones and alkyl alkenoates as palaeotemperature indicators: their production, flux and early sedimentary diagenesis in the Eastern North Atlantic". Organic Geochemistry. 19 (1–3): 287–298. Bibcode:1992OrGeo..19..287C. doi:10.1016/0146-6380(92)90044-X.
  10. Conte, Maureen H.; Thompson, Anthony; Eglinton, Geoffrey; Green, John C. (1995). "Lipid Biomarker Diversity in the Coccolithophorid Emiliania Huxleyi (Prymnesiophyceae) and the Related Species Gephyrocapsa Oceanica1". Journal of Phycology. 31 (2): 272–282. doi:10.1111/j.0022-3646.1995.00272.x. ISSN   0022-3646. S2CID   85989423.
  11. Conte, Maureen H; Thompson, Anthony; Lesley, David; Harris, Roger P (1998). "Genetic and Physiological Influences on the Alkenone/Alkenoate Versus Growth Temperature Relationship in Emiliania huxleyi and Gephyrocapsa Oceanica". Geochimica et Cosmochimica Acta. 62 (1): 51–68. Bibcode:1998GeCoA..62...51C. doi:10.1016/S0016-7037(97)00327-X.
  12. Conte, Maureen H; Ralph, Nate; Ross, Edith H (2001). "Seasonal and interannual variability in deep ocean particle fluxes at the Oceanic Flux Program (OFP)/Bermuda Atlantic Time Series (BATS) site in the western Sargasso Sea near Bermuda". Deep Sea Research Part II: Topical Studies in Oceanography. 48 (8–9): 1471–1505. Bibcode:2001DSRII..48.1471C. doi:10.1016/S0967-0645(00)00150-8.
  13. Conte, M.H.; Dickey, T.D.; Weber, J.C.; Johnson, R.J.; Knap, A.H. (2003). "Transient physical forcing of pulsed export of bioreactive material to the deep Sargasso Sea". Deep Sea Research Part I: Oceanographic Research Papers. 50 (10–11): 1157–1187. Bibcode:2003DSRI...50.1157C. doi:10.1016/S0967-0637(03)00141-9.
  14. Conte, M.H; Weber, J.C; King, L.L; Wakeham, S.G (2001). "The alkenone temperature signal in western North Atlantic surface waters". Geochimica et Cosmochimica Acta. 65 (23): 4275–4287. Bibcode:2001GeCoA..65.4275C. doi:10.1016/S0016-7037(01)00718-9.
  15. Conte, Maureen H.; Sicre, Marie-Alexandrine; Rühlemann, Carsten; Weber, John C.; Schulte, Sonja; Schulz-Bull, Detlef; Blanz, Thomas (2006). "Global temperature calibration of the alkenone unsaturation index (U K′ 37 ) in surface waters and comparison with surface sediments: ALKENONE UNSATURATION INDEX". Geochemistry, Geophysics, Geosystems. 7 (2): n/a. doi:10.1029/2005GC001054. S2CID   62825795.
  16. "Hurricane Nicole sheds light on how storms impact deep ocean". phys.org. September 19, 2019. Retrieved 2022-04-09.
  17. Pedrosa‐Pàmies, R.; Conte, M. H.; Weber, J. C.; Johnson, R. (2019). "Hurricanes Enhance Labile Carbon Export to the Deep Ocean". Geophysical Research Letters. 46 (17–18): 10484–10494. Bibcode:2019GeoRL..4610484P. doi: 10.1029/2019GL083719 . ISSN   0094-8276. S2CID   202191389.
  18. Rec, Abigail (2019-06-05). "Sea turtles trapped in Cape Cod Bay - How science is saving them". Cape Cod LIFE. Retrieved 2022-04-09.
  19. Peterson, Christy (2020-04-07). Into the Deep: Science, Technology, and the Quest to Protect the Ocean. Millbrook Press. ISBN   978-1-5415-9584-2.
  20. Moran, Barbara (May 15, 2020). "With Ships Docked And Labs Closed, Scientists' Field Research Season Fades Away". www.wbur.org. Retrieved 2022-04-09.