Articles | Volume 13, issue 5
https://doi.org/10.5194/cp-13-533-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-13-533-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
A 21 000-year record of fluorescent organic matter markers in the WAIS Divide ice core
Dept. Chemical and Biological Engineering, Montana State University,
Bozeman, MT 59717, USA
Center for Biofilm Engineering, Montana State University, Bozeman,
MT 59717, USA
Christine M. Foreman
Dept. Chemical and Biological Engineering, Montana State University,
Bozeman, MT 59717, USA
Center for Biofilm Engineering, Montana State University, Bozeman,
MT 59717, USA
Michael Sigl
Division of Hydrologic Science, Desert Research Institute, Reno,
NV 89512, USA
John C. Priscu
Dept. of Land Resources & Environmental Sciences, Montana State
University, Bozeman, MT 59717, USA
Joseph R. McConnell
Division of Hydrologic Science, Desert Research Institute, Reno,
NV 89512, USA
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- Organic matter distribution in the icy environments of Taylor Valley, Antarctica B. Guo et al. 10.1016/j.scitotenv.2022.156639
- Dynamic changes, cycling and downward fate of dissolved carbon and nitrogen photosynthetically-derived from glaciers in upper Indus river basin M. Bhat et al. 10.1016/j.envres.2024.120117
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37 citations as recorded by crossref.
- Aerosol-Climate Interactions During the Last Glacial Maximum S. Albani et al. 10.1007/s40641-018-0100-7
- Inferring Ecosystem Function from Dissolved Organic Matter Optical Properties: A Critical Review J. D’Andrilli et al. 10.1021/acs.est.2c04240
- Augmentation of field fluorescence measures for improved in situ contaminant detection M. Rincón Remolina & N. Peleato 10.1007/s10661-022-10652-1
- Application of machine learning methods for rapid fluorescence-based detection of naphthenic acids and phenol in natural surface waters M. Remolina et al. 10.1016/j.jhazmat.2022.128491
- Supraglacial Soils and Soil-Like Bodies: Diversity, Genesis, Functioning (Review) N. Mergelov et al. 10.1134/S1064229323602330
- Biogeochemical Connectivity Between Freshwater Ecosystems beneath the West Antarctic Ice Sheet and the Sub‐Ice Marine Environment T. Vick‐Majors et al. 10.1029/2019GB006446
- Qualitative variability of dissolved organic matter in the Baltic Sea sediments apparent from fluxes and optical properties A. Loginova et al. 10.3389/fmars.2024.1433199
- Biochar-derived dissolved organic matter enhanced the release of residual ciprofloxacin from the soil solid phase G. Chen et al. 10.1016/j.chemosphere.2024.142193
- Dissolved organic matter evolution and straw decomposition rate characterization under different water and fertilizer conditions based on three-dimensional fluorescence spectrum and deep learning G. Yang et al. 10.1016/j.jenvman.2023.118537
- Enhanced hydrolysis/acidogenesis and potential mechanism in thermal-alkali-biofilm synergistic pretreatment of high-solid and low-organic-content sludge S. Shi et al. 10.1016/j.biortech.2023.128988
- Compositions, sources, and bioavailability of colloidal organic matter in Lake Taihu Y. Ding et al. 10.1016/j.jglr.2024.102400
- Geospatial Variability of Fluorescent Dissolved Organic Matter in Urban Watersheds: Relationships with Land Cover and Wastewater Infrastructure J. Batista-Andrade et al. 10.1021/acs.est.3c07925
- Biogeochemical evolution of ponded meltwater in a High Arctic subglacial tunnel A. Dubnick et al. 10.5194/tc-17-2993-2023
- Sorption of colored vs. noncolored organic matter by tidal marsh soils P. Neale et al. 10.5194/bg-21-2599-2024
- Do early diagenetic processes affect the applicability of commonly-used organic matter source tracking tools? An assessment through controlled degradation end-member mixing experiments M. Derrien et al. 10.1016/j.watres.2020.115588
- Effects of FeSO4 dosage on nitrogen loss and humification during the composting of cow dung and corn straw J. Mei et al. 10.1016/j.biortech.2021.125867
- Experimental evaluation of the role of inorganic phosphorus for terrestrial carbon degradation in stream hyporheic zones K. Attermeyer et al. 10.1111/fwb.13980
- Optical and molecular characteristics of urban wastewater dissolved organic matter: insights into their correlations J. Chu & Z. Liao 10.1039/D4EW00519H
- Supraglacial Soils and Soil-Like Bodies: Diversity, Genesis, Functioning (Review) N. Mergelov et al. 10.31857/S0032180X23601494
- Water extractable organic matter and iron in relation to land use and seasonal changes S. Praise et al. 10.1016/j.scitotenv.2019.136070
- Explore variations of DOM components in different landcover areas of riparian zone by EEM-PARAFAC and partial least squares structural equation model X. Zhang et al. 10.1016/j.saa.2022.122300
- Bulk optical characterization of dissolved organic matter from semiarid wheat-based cropping systems C. Romero et al. 10.1016/j.geoderma.2017.06.029
- The migration and transformation processes of dissolved organic matter in rainwater- drip water- phreatic water of a typical karst spring catchment, in South China J. Shi et al. 10.1016/j.jhydrol.2023.130077
- WATSON:In SituOrganic Detection in Subsurface Ice Using Deep-UV Fluorescence Spectroscopy E. Eshelman et al. 10.1089/ast.2018.1925
- In-lake processing counteracts the effect of allochthonous input on the composition of color dissolved organic matter in a deep lake S. An et al. 10.1016/j.scitotenv.2022.158970
- Composition of dissolved organic matter controls interactions with La and Al ions: Implications for phosphorus immobilization in eutrophic lakes Y. Du et al. 10.1016/j.envpol.2019.02.002
- Biodegradation-induced signatures in sediment pore water dissolved organic matter: Implications from artificial sediments composed of two contrasting sources M. Derrien et al. 10.1016/j.scitotenv.2019.133714
- Response of bacterial community in composition and function to the various DOM at river confluences in the urban area Y. Li et al. 10.1016/j.watres.2019.115293
- Polar ice core organic matter signatures reveal past atmospheric carbon composition and spatial trends across ancient and modern timescales J. D'Andrilli & J. McConnell 10.1017/jog.2021.51
- Optical properties of dissolved organic matter highlight peatland-like properties in a constructed wetland M. Clark et al. 10.1016/j.scitotenv.2021.149770
- The Process of Soil Carbon Sequestration in Different Ecological Zones of Qingtu Lake in the Arid–Semi-Arid Region of Western China T. Wang et al. 10.3390/microorganisms12112122
- Applying EEM-PARAFAC combined with moving-window 2DCOS and structural equation modeling to characterize binding properties of Cu (II) with DOM from different sources in an urbanized river D. Liu et al. 10.1016/j.watres.2022.119317
- Subsurface In Situ Detection of Microbes and Diverse Organic Matter Hotspots in the Greenland Ice Sheet M. Malaska et al. 10.1089/ast.2020.2241
- Roles of magnetic coagulation in black-odor water restoration: An insight into dissolved organic matters L. Zheng et al. 10.1016/j.watcyc.2022.11.002
- Organic matter distribution in the icy environments of Taylor Valley, Antarctica B. Guo et al. 10.1016/j.scitotenv.2022.156639
- Dynamic changes, cycling and downward fate of dissolved carbon and nitrogen photosynthetically-derived from glaciers in upper Indus river basin M. Bhat et al. 10.1016/j.envres.2024.120117
- Tracking the evolution of particulate organic matter sources during summer storm events via end-member mixing analysis based on spectroscopic proxies M. Derrien et al. 10.1016/j.chemosphere.2020.126445
Latest update: 02 Nov 2024
Short summary
Climate-driven trends in fluorescent organic matter (OM) markers from Antarctic ice cores revealed fluctuations over 21.0 kyr, reflecting environmental shifts as a result of global ecosystem response in a warming climate. Precursors of lignin-like fluorescent chemical species were detected as OM markers from the Last Glacial Maximum to the mid-Holocene. Holocene ice contained the most complex lignin-like fluorescent OM markers. Thus, ice cores contain paleoecological OM markers of Earth’s past.
Climate-driven trends in fluorescent organic matter (OM) markers from Antarctic ice cores...