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Artykuły w czasopismach na temat „Geotragus”

Autor: Grafiati

Data publikacji: 3 czerwca 2025

Data aktualizacji: 31 lipca 2025

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1

REN, LI, MIGUEL A. ALONSO-ZARAZAGA, and RUNZHI ZHANG. "Revision of the Chinese Geotragus Schoenherr with description of three new species (Coleoptera: Curculionidae: Entiminae)." Zootaxa 3619, no. 2 (2013): 161–82. http://dx.doi.org/10.11646/zootaxa.3619.2.5.

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The Chinese representatives of the entimine weevil genus Geotragus are here revised, including redescriptions of the two previously known species, G. himalayanus Boheman, 1845 and G. tuberculatus Chen, 1990, and descriptions of three new species from the Hengduan Mountains, Yunnan province, China: G. brevidens sp. nov., G. declivis sp. nov. and G. rugosus sp. nov.. Diagnostic characters of the genus, a key to Chinese species of Geotragus and a checklist of the now 11 known world species are also provided.

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2

Song, Zhenzhen, Li Ren, Runzhi Zhang, and Chenggang Zhou. "Review of the species of Leptomias Faust from Sichuan, China (Coleoptera, Curculionidae, Entiminae)." ZooKeys 678 (June 7, 2017): 97–119. https://doi.org/10.3897/zookeys.678.12543.

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An account is given of the twelve species of Leptomias Faust, 1886 occurring in the Sichuan Province of China, including the description of a new species, Leptomias verticalis Ren, Zhang & Song, sp. n. from Jiulong County, Southwest Sichuan. New locality data and remarks for the other eleven species, a key to and distribution map of all twelve Sichuan species are provided. Leptomias chenae Alonso-Zarazaga & Ren is transferred to Geotragus Schoenherr, 1845, where its valid name is G. granulatus (Chao, 1980), comb. n. in application of Art. 59.4. Structural details of Leptomias verticali

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Ren, Li, Miguel A. Alonso-Zarazaga, and Runzhi Zhang. "Revision of the Chinese Geotragus Schoenherr with description of three new species (Coleoptera: Curculionidae: Entiminae)." Zootaxa 3619, no. 2 (2013): 161–82. https://doi.org/10.11646/zootaxa.3619.2.5.

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Ren, Li, Alonso-Zarazaga, Miguel A., Zhang, Runzhi (2013): Revision of the Chinese Geotragus Schoenherr with description of three new species (Coleoptera: Curculionidae: Entiminae). Zootaxa 3619 (2): 161-182, DOI: 10.11646/zootaxa.3619.2.5

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Theodosiou, Ir, E. Athanassouli, N. Epitropou, Z. Janikian, G. Kossiaris, and K. Michail. "GEOTRAILS IN GREECE." Bulletin of the Geological Society of Greece 43, no. 2 (2017): 939. http://dx.doi.org/10.12681/bgsg.11259.

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Planning of walking and motoring geotrails around the geosites, in combination with other attractions of biotic, archaeological and cultural interest, as well as creation of interpretative, awareness printed material relevant to the geosites is one of the objectives of the project “Designation of geosites – geoparks, contribution to sustainable development”. It is a project of the Institute of Geology and Mineral Exploration (IGME), funded from the 3rd community support framework program. Furthermore, this printed material which is also available in digital form aided by the project’s data bas

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5

PETKEWICH, RACHEL. "GEOTRACES GETS GOING." Chemical & Engineering News 86, no. 35 (2008): 57–60. http://dx.doi.org/10.1021/cen-v086n035.p057.

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Dodas, Elena Masferrer, Robert F. Anderson, and Catherine Jeandel. "GEOTRACES International Program: Open Access Database of Seawater Trace Metal and Isotope Data Available." Marine Technology Society Journal 56, no. 3 (2022): 130–31. http://dx.doi.org/10.4031/mtsj.56.3.23.

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Abstract GEOTRACES (<ext-link ext-link-type="uri" xlink:href="https://www.geotraces.org/">https://www.geotraces.org/</ext-link>) is an international marine chemical program involving scientists from more than 35 countries collaborating together since 2010 in building an online atlas and open access database of high-quality hydrographical and geochemical data, under the name of GEOTRACES Intermediate Data Product. By freely releasing its data, GEOTRACES wishes to strengthen and intensify the collaboration within the marine research community itself, but also wants to invite other oc

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7

Benitez-Nelson, Claudia. "A Needle in the Haystack." Oceanography 37, no. 2 (2024): 5. http://dx.doi.org/10.5670/oceanog.2024.422.

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For the past 20 years, the GEOTRACES program has produced transformative insights into the cycling of trace elements and isotopes (TEIs) in the ocean. Modeled after the 1970s GEOSECS (Geochemical Ocean Sections Study) program, the goals of this ambitious study were to conduct large-scale measurements of TEI concentrations and to determine the biogeochemical processes that controlled their distributions throughout the global ocean. Perhaps the biggest hurdle to overcome was how to accurately measure less than nanomolar concentrations of TEIs from the deck of a 3,000 gross tonnage steel ship. Co

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8

Theodosiou, Ir, P. Paschos, E. Nicolaou, et al. "Planning of Geotrails and potential Geoparks in Greece." Schriftenreihe der Deutschen Gesellschaft für Geowissenschaften 66 (May 28, 2010): 128–29. http://dx.doi.org/10.1127/sdgg/66/2010/128.

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9

Boyle, Edward A., Cheryl Zurbrick, Jong-Mi Lee, et al. "Lead and lead isotopes in the U.S. GEOTRACES East Pacific zonal transect (GEOTRACES GP16)." Marine Chemistry 227 (December 2020): 103892. http://dx.doi.org/10.1016/j.marchem.2020.103892.

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10

Ketut Ari Pegatariana, I., Adi Susilo, Faridha Aprilia, and Bayu Hangga Triyo Eko Putro. "Tracing Geological Stories: A Geotrail Study in Purwodadi Village, Tirtoyudo District, Malang Regency." IOP Conference Series: Earth and Environmental Science 1424, no. 1 (2024): 012006. https://doi.org/10.1088/1755-1315/1424/1/012006.

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Abstract Purwodadi Village of the Tirtoyudo District, Malang Regency was recognized as one of the 75 recipients of the Indonesian Tourism Village Award (ADWI) in 2023. To identify tourism potential in this area, it is an important to develop geology-based tourism, or geotourism. The study area is located in the Southern Mountain Zone, which mainly consists of the Old Andesite Formation (OAF), Paleogene to Neogene Period in ages. The OAF has a unique features and diverse composition of geological elements, as well as their geological history. However, they were undergone erosion, making them vu

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11

Theodosiou, Ir. "DESIGNATION OF GEOSITES- PROPOSALS FOR GEOPARKS IN GREECE." Bulletin of the Geological Society of Greece 43, no. 2 (2017): 926. http://dx.doi.org/10.12681/bgsg.11258.

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During the last three years, the research project: “Geosites, geoparks contribution to sustainable development” aiming at recording and designating geosites and potential geoparks, as a means to sustainable development, funded from the 3rd Community Support Framework (CSF) programme, is developing at the Institute of Geology and Mineral Exploration of Greece (IGME). The project, according to its objectives, is divided in the following five sub-projects: 1: Identification, characterization, evaluation of geosites 2: Compilation of a DataBase and a Geographic Information System (GIS) for the geo

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12

Charette, Matthew A., Henrieta Dulaiova, Meagan E. Gonneea, et al. "GEOTRACES radium isotopes interlaboratory comparison experiment." Limnology and Oceanography: Methods 10, no. 6 (2012): 451–63. http://dx.doi.org/10.4319/lom.2012.10.451.

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13

Mawji, Edward, Reiner Schlitzer, Elena Masferrer Dodas, et al. "The GEOTRACES Intermediate Data Product 2014." Marine Chemistry 177 (December 2015): 1–8. http://dx.doi.org/10.1016/j.marchem.2015.04.005.

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14

Schlitzer, Reiner, Robert F. Anderson, Elena Masferrer Dodas, et al. "The GEOTRACES Intermediate Data Product 2017." Chemical Geology 493 (August 2018): 210–23. http://dx.doi.org/10.1016/j.chemgeo.2018.05.040.

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15

Jenkins, W. J., D. E. Lott, B. E. Longworth, J. M. Curtice, and K. L. Cahill. "The distributions of helium isotopes and tritium along the U.S. GEOTRACES North Atlantic sections (GEOTRACES GAO3)." Deep Sea Research Part II: Topical Studies in Oceanography 116 (June 2015): 21–28. http://dx.doi.org/10.1016/j.dsr2.2014.11.017.

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16

Stolz, Julian, and Heidi Elisabeth Megerle. "Geotrails as a Medium for Education and Geotourism: Recommendations for Quality Improvement Based on the Results of a Research Project in the Swabian Alb UNESCO Global Geopark." Land 11, no. 9 (2022): 1422. http://dx.doi.org/10.3390/land11091422.

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Geotourism is one of the fastest growing tourism branches. Geoparks feature prominently in geotourism as well as geoeducation. Well-designed geotrails link local geology, geoheritage and geoeducation. Unfortunately many trails do not consider or insufficiently acknowledge recent didactic and touristic findings. As a result, they fail to interest a lay audience in geological phenomena, convey relevant information, and attract tourists to the region. A catalogue of state-of-the-art criteria for the evaluation of existing geotrails based on a case study of the UNESCO Global Geopark Swabian Alb (G

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17

Perotti, Luigi, Irene Maria Bollati, Cristina Viani, et al. "Fieldtrips and Virtual Tours as Geotourism Resources: Examples from the Sesia Val Grande UNESCO Global Geopark (NW Italy)." Resources 9, no. 6 (2020): 63. http://dx.doi.org/10.3390/resources9060063.

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In the 20th anniversary year of the European Geopark Network, and 5 years on from the receipt of the UNESCO label for the geoparks, this research focuses on geotourism contents and solutions within one of the most recently designated geoparks, admitted for membership in 2013: the Sesia Val Grande UNESCO Global Geopark (Western Italian Alps). The main aim of this paper is to corroborate the use of fieldtrips and virtual tours as resources for geotourism. The analysis is developed according to: i) geodiversity and geoheritage of the geopark territory; ii) different approaches for planning fieldt

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18

Boyd, Philip W., and Matthieu Bressac. "Developing a test-bed for robust research governance of geoengineering: the contribution of ocean iron biogeochemistry." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 374, no. 2081 (2016): 20150299. http://dx.doi.org/10.1098/rsta.2015.0299.

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Geoengineering to mitigate climate change has long been proposed, but remains nebulous. Exploration of the feasibility of geoengineering first requires the development of research governance to move beyond the conceptual towards scientifically designed pilot studies. Fortuitously, 12 mesoscale (approx. 1000 km 2 ) iron enrichments, funded to investigate how ocean iron biogeochemistry altered Earth's carbon cycle in the geological past, provide proxies to better understand the benefits and drawbacks of geoengineering. The utility of these iron enrichments in the geoengineering debate is enhance

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19

Homoky, William B., Thomas Weber, William M. Berelson, et al. "Quantifying trace element and isotope fluxes at the ocean–sediment boundary: a review." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 374, no. 2081 (2016): 20160246. http://dx.doi.org/10.1098/rsta.2016.0246.

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Quantifying fluxes of trace elements and their isotopes (TEIs) at the ocean's sediment–water boundary is a pre-eminent challenge to understand their role in the present, past and future ocean. There are multiple processes that drive the uptake and release of TEIs, and properties that determine their rates are unevenly distributed (e.g. sediment composition, redox conditions and (bio)physical dynamics). These factors complicate our efforts to find, measure and extrapolate TEI fluxes across ocean basins. GEOTRACES observations are unveiling the oceanic distributions of many TEIs for the first ti

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20

Grasse, Patricia, Mark A. Brzezinski, Damien Cardinal, et al. "GEOTRACES inter-calibration of the stable silicon isotope composition of dissolved silicic acid in seawater." Journal of Analytical Atomic Spectrometry 32, no. 3 (2017): 562–78. http://dx.doi.org/10.1039/c6ja00302h.

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The first inter-calibration study of the stable silicon isotope composition of dissolved silicic acid in seawater, δ<sup>30</sup>Si(OH)<sub>4</sub>, is presented as a contribution to the international GEOTRACES program.

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21

Shin, Jaeryul, Byeongcheon Ko, Yeongmin Hong, and Huigyeong Ryu. "Development of Geotrails in Galgot beach, Geoje." Journal of The Korean Association of Regional Geographers 28, no. 3 (2022): 300–310. http://dx.doi.org/10.26863/jkarg.2022.8.28.3.300.

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22

Charette, Matthew A., Henrieta Dulaiova, Meagan E. Gonneea, et al. "Erratum: GEOTRACES radium isotopes interlaboratory comparison experiment." Limnology and Oceanography: Methods 10, no. 8 (2012): 617. http://dx.doi.org/10.4319/lom.2012.10.617.

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23

Hatta, Mariko, Chris I. Measures, Jingfeng Wu, et al. "An overview of dissolved Fe and Mn distributions during the 2010–2011 U.S. GEOTRACES north Atlantic cruises: GEOTRACES GA03." Deep Sea Research Part II: Topical Studies in Oceanography 116 (June 2015): 117–29. http://dx.doi.org/10.1016/j.dsr2.2014.07.005.

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German, C. R., K. A. Casciotti, J. C. Dutay, et al. "Hydrothermal impacts on trace element and isotope ocean biogeochemistry." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 374, no. 2081 (2016): 20160035. http://dx.doi.org/10.1098/rsta.2016.0035.

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Hydrothermal activity occurs in all ocean basins, releasing high concentrations of key trace elements and isotopes (TEIs) into the oceans. Importantly, the calculated rate of entrainment of the entire ocean volume through turbulently mixing buoyant hydrothermal plumes is so vigorous as to be comparable to that of deep-ocean thermohaline circulation. Consequently, biogeochemical processes active within deep-ocean hydrothermal plumes have long been known to have the potential to impact global-scale biogeochemical cycles. More recently, new results from GEOTRACES have revealed that plumes rich in

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Anderson, Robert F., Martin Q. Fleisher, Laura F. Robinson, et al. "GEOTRACES intercalibration of230Th,232Th,231Pa, and prospects for10Be." Limnology and Oceanography: Methods 10, no. 4 (2012): 179–213. http://dx.doi.org/10.4319/lom.2012.10.179.

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Anderson, Robert, Edward Mawji, Gregory Cutter, Christopher Measures, and Catherine Jeandel. "GEOTRACES: Changing the Way We Explore Ocean Chemistry." Oceanography 27, no. 1 (2014): 50–61. http://dx.doi.org/10.5670/oceanog.2014.07.

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Hayes, Christopher T., Robert F. Anderson, Martin Q. Fleisher, et al. "230Th and 231Pa on GEOTRACES GA03, the U.S. GEOTRACES North Atlantic transect, and implications for modern and paleoceanographic chemical fluxes." Deep Sea Research Part II: Topical Studies in Oceanography 116 (June 2015): 29–41. http://dx.doi.org/10.1016/j.dsr2.2014.07.007.

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Jickells, T. D., A. R. Baker, and R. Chance. "Atmospheric transport of trace elements and nutrients to the oceans." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 374, no. 2081 (2016): 20150286. http://dx.doi.org/10.1098/rsta.2015.0286.

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This paper reviews atmospheric inputs of trace elements and nutrients to the oceans in the context of the GEOTRACES programme and provides new data from two Atlantic GEOTRACES cruises. We consider the deposition of nitrogen to the oceans, which is now dominated by anthropogenic emissions, the deposition of mineral dust and related trace elements, and the deposition of other trace elements which have a mixture of anthropogenic and dust sources. We then consider the solubility (as a surrogate for bioavailability) of the various elements. We consider briefly the sources, atmospheric transport and

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Fitzsimmons, Jessica, and Janelle Steffen. "The “Net” Impact of Hydrothermal Venting on Oceanic Elemental Inventories: Contributions to Plume Geochemistry from the International GEOTRACES Program." Oceanography 37, no. 2 (2024): 102–15. http://dx.doi.org/10.5670/oceanog.2024.421.

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Hydrothermal vents serve as a primary interface between the cold deep ocean and the warm oceanic crust. While early research showed that seawater-rock interactions add to or remove elements from seawater during the generation of hydrothermal fluids, consideration of these fluid fluxes alone does not relay the total impact that hydrothermal systems have on seawater geochemistry. In addition, hydrothermal plumes, areas where hydrothermal fluids mix with ocean waters, are host to a range of particle precipitation and scavenging reactions that further modify gross hydrothermal fluid fluxes to def

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30

Buck, Kristen N., Peter N. Sedwick, Bettina Sohst, and Craig A. Carlson. "Organic complexation of iron in the eastern tropical South Pacific: Results from US GEOTRACES Eastern Pacific Zonal Transect (GEOTRACES cruise GP16)." Marine Chemistry 201 (April 2018): 229–41. http://dx.doi.org/10.1016/j.marchem.2017.11.007.

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31

Kenna, Timothy C., Pere Masqué, José Luís Mas, et al. "Intercalibration of selected anthropogenic radionuclides for the GEOTRACES Program." Limnology and Oceanography: Methods 10, no. 8 (2012): 590–607. http://dx.doi.org/10.4319/lom.2012.10.590.

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Höfling, Richard, and Heike Burkhardt. "Selected geotopes and geotrails in the National Geopark Ries." Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 102 (April 2, 2020): 17–32. http://dx.doi.org/10.1127/jmogv/102/0002.

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Sedwick, P. N., B. M. Sohst, S. J. Ussher, and A. R. Bowie. "A zonal picture of the water column distribution of dissolved iron(II) during the U.S. GEOTRACES North Atlantic transect cruise (GEOTRACES GA03)." Deep Sea Research Part II: Topical Studies in Oceanography 116 (June 2015): 166–75. http://dx.doi.org/10.1016/j.dsr2.2014.11.004.

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Vlachopoulos, Nikolaos, and Panagiotis Voudouris. "Preservation of the Geoheritage and Mining Heritage of Serifos Island, Greece: Geotourism Perspectives in a Potential New Global Unesco Geopark." Geosciences 12, no. 3 (2022): 127. http://dx.doi.org/10.3390/geosciences12030127.

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Serifos island is characterized by rich geodiversity, industrial and cultural heritage. The present paper focuses on the geological and mining heritage of Serifos, with the aim of integrating the island in the international environment of Geoparks, in the near future. In this geopark, Serifos can highlight the rich geological heritage of the island combined with the rich industrial heritage as expressed by mining activities since prehistoric times and the mining facilities of iron and copper mines. During the present study, six geotrails have been developed to link these cultural and ecologica

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Baker, A. R., W. M. Landing, E. Bucciarelli, et al. "Trace element and isotope deposition across the air–sea interface: progress and research needs." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 374, no. 2081 (2016): 20160190. http://dx.doi.org/10.1098/rsta.2016.0190.

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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

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Maloney, Katie M., Alexander L. Peace, Joe Hansen, et al. "Earth Science Education #7. GeoTrails: Accessible Online Tools for Outreach and Education." Geoscience Canada 50, no. 3 (2023): 73–84. http://dx.doi.org/10.12789/geocanj.2023.50.198.

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As geoscientists, we must prioritize improving our ability to communicate science to the public. Effective geoscience communication enables communities to understand how geological processes have shaped our planet and make informed decisions about Earth’s future. However, geoscience research outputs have traditionally been published in peer-reviewed journals and presented at academic conferences. Consequently, essential information about local geology is rarely available in accessible, open access, and engaging formats. Here, we propose virtual field trips, or ‘GeoTrails’, as a possible soluti

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Drápela, Emil. "Using a Geotrail for Teaching Geography: An Example of the Virtual Educational Trail “The Story of Liberec Granite”." Land 12, no. 4 (2023): 828. http://dx.doi.org/10.3390/land12040828.

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Geotrails are valuable resources for the field teaching of geography and natural history, as they amusingly explain the phenomena associated with inanimate nature and geoheritage. However, not all geotrails are frequently used for field education, in fact, most of them are only used sporadically. In order to identify the key elements needed for a geotrail to be used frequently and successfully for field education, an evaluation of the virtual nature trail “The Story of Liberec Granite”, which is one of the most used trails for educational purposes in the Czech Republic, was carried out. The ev

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Charette, Matthew A., Paul J. Morris, Paul B. Henderson, and Willard S. Moore. "Radium isotope distributions during the US GEOTRACES North Atlantic cruises." Marine Chemistry 177 (December 2015): 184–95. http://dx.doi.org/10.1016/j.marchem.2015.01.001.

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Jacquot, Jeremy E., and James W. Moffett. "Copper distribution and speciation across the International GEOTRACES Section GA03." Deep Sea Research Part II: Topical Studies in Oceanography 116 (June 2015): 187–207. http://dx.doi.org/10.1016/j.dsr2.2014.11.013.

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Saidu, Aminu, S. K. Zaky, S. S. Sani, et al. "An Examination of the Ocean Pollution Risks in Nigeria: A Review." Sahel Journal of Life Sciences FUDMA 3, no. 1 (2025): 158–72. https://doi.org/10.33003/sajols-2025-0301-19.

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Despite possessing a wealth of natural resources and diverse ecosystems, the ocean faces numerous pollution-related challenges. Pollution, defined as the discharge of unwanted and often hazardous waste, seriously jeopardizes the integrity of the Earth's support systems and the survival of human cultures. Though the global community strives through large-scale research initiatives like GEOTRACES, IMBER, and SOLAS, which have significantly increased the available data, understanding of ocean systems remains limited and unevenly distributed. This review aims to present knowledge about ocean pollu

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Lausch, Angela, Jussi Baade, Lutz Bannehr, et al. "Linking Remote Sensing and Geodiversity and Their Traits Relevant to Biodiversity—Part I: Soil Characteristics." Remote Sensing 11, no. 20 (2019): 2356. http://dx.doi.org/10.3390/rs11202356.

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In the face of rapid global change it is imperative to preserve geodiversity for the overall conservation of biodiversity. Geodiversity is important for understanding complex biogeochemical and physical processes and is directly and indirectly linked to biodiversity on all scales of ecosystem organization. Despite the great importance of geodiversity, there is a lack of suitable monitoring methods. Compared to conventional in-situ techniques, remote sensing (RS) techniques provide a pathway towards cost-effective, increasingly more available, comprehensive, and repeatable, as well as standardi

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Charette, Matthew A., Phoebe J. Lam, Maeve C. Lohan, et al. "Coastal ocean and shelf-sea biogeochemical cycling of trace elements and isotopes: lessons learned from GEOTRACES." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 374, no. 2081 (2016): 20160076. http://dx.doi.org/10.1098/rsta.2016.0076.

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Continental shelves and shelf seas play a central role in the global carbon cycle. However, their importance with respect to trace element and isotope (TEI) inputs to ocean basins is less well understood. Here, we present major findings on shelf TEI biogeochemistry from the GEOTRACES programme as well as a proof of concept for a new method to estimate shelf TEI fluxes. The case studies focus on advances in our understanding of TEI cycling in the Arctic, transformations within a major river estuary (Amazon), shelf sediment micronutrient fluxes and basin-scale estimates of submarine groundwater

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Anderson, Robert F. "GEOTRACES: Accelerating Research on the Marine Biogeochemical Cycles of Trace Elements and Their Isotopes." Annual Review of Marine Science 12, no. 1 (2020): 49–85. http://dx.doi.org/10.1146/annurev-marine-010318-095123.

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The biogeochemical cycles of trace elements and their isotopes (TEIs) constitute an active area of oceanographic research due to their role as essential nutrients for marine organisms and their use as tracers of oceanographic processes. Selected TEIs also provide diagnostic information about the physical, geological, and chemical processes that supply or remove solutes in the ocean. Many of these same TEIs provide information about ocean conditions in the past, as their imprint on marine sediments can be interpreted to reflect changes in ocean circulation, biological productivity, the ocean ca

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Sarthou, Géraldine, Pascale Lherminier, Eric P. Achterberg, et al. "Introduction to the French GEOTRACES North Atlantic Transect (GA01): GEOVIDE cruise." Biogeosciences 15, no. 23 (2018): 7097–109. http://dx.doi.org/10.5194/bg-15-7097-2018.

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Abstract. The GEOVIDE cruise, a collaborative project within the framework of the international GEOTRACES programme, was conducted along the French-led section in the North Atlantic Ocean (Section GA01), between 15 May and 30 June 2014. In this special issue (https://www.biogeosciences.net/special_issue900.html), results from GEOVIDE, including physical oceanography and trace element and isotope cyclings, are presented among 18 articles. Here, the scientific context, project objectives, and scientific strategy of GEOVIDE are provided, along with an overview of the main results from the article

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Menzel Barraqueta, Jan-Lukas, Jessica K. Klar, Martha Gledhill, et al. "Atmospheric deposition fluxes over the Atlantic Ocean: a GEOTRACES case study." Biogeosciences 16, no. 7 (2019): 1525–42. http://dx.doi.org/10.5194/bg-16-1525-2019.

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Abstract. Atmospheric deposition is an important source of micronutrients to the ocean, but atmospheric deposition fluxes remain poorly constrained in most ocean regions due to the limited number of field observations of wet and dry atmospheric inputs. Here we present the distribution of dissolved aluminium (dAl), as a tracer of atmospheric inputs, in surface waters of the Atlantic Ocean along GEOTRACES sections GA01, GA06, GA08, and GA10. We used the surface mixed-layer concentrations of dAl to calculate atmospheric deposition fluxes using a simple steady state model. We have optimized the Al

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Lam, Phoebe J., and Robert F. Anderson. "GEOTRACES: The Marine Biogeochemical Cycle of Trace Elements and Their Isotopes." Elements 14, no. 6 (2018): 377–78. http://dx.doi.org/10.2138/gselements.14.6.377.

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Frank, Martin, Catherine Jeandel, Robert F. Anderson, Gideon Henderson, Roger Francois, and Mukul Sharma. "GEOTRACES: Studying the global marine biogeochemistry of trace elements and isotopes." Eos, Transactions American Geophysical Union 84, no. 34 (2003): 327. http://dx.doi.org/10.1029/2003eo340006.

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Jenkins, W. J., W. M. Smethie, E. A. Boyle, and G. A. Cutter. "Water mass analysis for the U.S. GEOTRACES (GA03) North Atlantic sections." Deep Sea Research Part II: Topical Studies in Oceanography 116 (June 2015): 6–20. http://dx.doi.org/10.1016/j.dsr2.2014.11.018.

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Oka, Akira, Hirofumi Tazoe, and Hajime Obata. "Simulation of global distribution of rare earth elements in the ocean using an ocean general circulation model." Journal of Oceanography 77, no. 3 (2021): 413–30. http://dx.doi.org/10.1007/s10872-021-00600-x.

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AbstractIn this study, we report our ocean general circulation model simulations of the global distribution of rare earth elements (REEs) in the ocean. As previously reported (Oka et al. in Glob Biogeochem Cycles 23:1–16, 2009), the vertical profiles of REEs in the North Pacific Ocean are strongly controlled by the reversible scavenging process, and the systematic differences between REEs can be reproduced in the model by selecting an appropriate model parameter which controls affinity to particles. We here demonstrate that the external REE input from the coastal regions also plays a role in c

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Tagliabue, Alessandro, and Thomas Weber. "Novel Insights into Ocean Trace Element Cycling from Biogeochemical Models." Oceanography 37, no. 2 (2024): 131–41. http://dx.doi.org/10.5670/oceanog.2024.418.

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Ocean biogeochemical models have become critical tools for interpreting trace element and isotope (TEI) distributions observed during the GEOTRACES program and understanding their driving processes. Models stimulate new research questions that cannot be addressed with observations alone, for instance, concerning processes that occur over vast spatial scales and linkages between TEIs and other elemental cycles. A spectrum of modeling approaches has been applied to date, including (1) fully prognostic models that couple TEIs to broader biogeochemical frameworks, (2) simpler element-specific mech

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