ORCID Profile
0000-0002-6421-3166
Current Organisations
Smithsonian Institution
,
Macquarie University
,
Smithsonian Marine Station
,
Macquarie University Faculty of Science and Engineering
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Publisher: Springer Science and Business Media LLC
Date: 08-10-2019
Publisher: Springer Science and Business Media LLC
Date: 09-08-2023
Publisher: Chinese Society for Mineralogy, Petrology, and Geochemistry
Date: 2022
Publisher: Elsevier BV
Date: 07-2018
Publisher: Editorial Office of Earth Science
Date: 2014
Publisher: Proceedings of the National Academy of Sciences
Date: 26-10-2020
Abstract: Consumption transfers energy and materials through food chains and fundamentally influences ecosystem productivity. Therefore, mapping the distribution of consumer feeding intensity is key to understanding how environmental changes influence bio ersity, with consequent effects on trophic transfer and top–down impacts through food webs. Our global comparison of standardized bait consumption in shallow coastal habitats finds a peak in feeding intensity away from the equator that is better explained by the presence of particular consumer families than by latitude or temperature. This study complements recent demonstrations that changes in bio ersity can have similar or larger impacts on ecological processes than those of climate.
Publisher: Elsevier BV
Date: 04-2020
Publisher: Elsevier BV
Date: 09-2017
Publisher: Elsevier BV
Date: 03-2023
Publisher: Springer Science and Business Media LLC
Date: 22-07-2021
DOI: 10.1038/S41467-021-24750-0
Abstract: Remobilization of sedimentary carbonate in subduction zones modulates arc volcanism emissions and thus Earth’s climate over geological timescales. Although limestones (or chalk) are thought to be the major carbon reservoir subducted to subarc depths, their fate is still unclear. Here we present high-pressure reaction experiments between impure limestone (7.4 wt.% clay) and dunite at 1.3–2.7 GPa to constrain the melting behaviour of subducted natural limestone in contact with peridotite. The results show that although clay impurities significantly depress the solidus of limestone, melting will not occur whilst limestones are still part of the subducting slab. Buoyancy calculations suggest that most of these limestones would form solid-state diapirs intruding into the mantle wedge, resulting in limited carbon flux to the deep mantle ( ~10 Mt C y −1 ). Less than 20% melting within the mantle wedge indicates that most limestones remain stable and are stored in subarc lithosphere, resulting in massive carbon storage in convergent margins considering their high carbon flux (~21.4 Mt C y −1 ). Assimilation and outgassing of these carbonates during arc magma ascent may dominate the carbon flux in volcanic arcs.
Publisher: Geological Society of America
Date: 20-10-2016
DOI: 10.1130/G38365.1
Publisher: Geological Society of America
Date: 11-04-2017
DOI: 10.1130/G39077Y.1
Publisher: Springer Science and Business Media LLC
Date: 23-06-2021
Publisher: Elsevier BV
Date: 09-2021
Publisher: Mineralogical Society of America
Date: 02-2017
DOI: 10.2138/AM-2017-5721
Publisher: Elsevier BV
Date: 12-2020
Publisher: Elsevier BV
Date: 02-2020
Publisher: Elsevier BV
Date: 09-2017
Publisher: Elsevier BV
Date: 07-2020
Publisher: Elsevier BV
Date: 03-2019
Publisher: Elsevier BV
Date: 2023
Publisher: Elsevier BV
Date: 06-2020
Publisher: Elsevier BV
Date: 10-2018
Publisher: Elsevier BV
Date: 08-2017
Publisher: Elsevier BV
Date: 09-2021
Location: United States of America
Location: Australia
No related grants have been discovered for Chunfei Chen.