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  1. Book ; Online: UAV approaches for improved mapping of vegetation cover and estimation of carbon storage of small saltmarshes

    Hiles, William / Miller, Lucy C. / Smeaton, Craig / Austin, William E. N.

    eISSN: 1726-4189

    examples from Loch Fleet, northeast Scotland

    2024  

    Abstract: Saltmarsh environments are recognised as key components of many biophysical and biochemical processes at the local and global scale. Accurately mapping these environments, and understanding how they are changing over time, is crucial for better ... ...

    Abstract Saltmarsh environments are recognised as key components of many biophysical and biochemical processes at the local and global scale. Accurately mapping these environments, and understanding how they are changing over time, is crucial for better understanding these systems. However, traditional surveying techniques are time-consuming and are inadequate for understanding how these dynamic systems may be changing temporally and spatially. The development of uncrewed aerial vehicle (UAV) technology presents an opportunity for efficiently mapping saltmarsh extent. Here we develop a methodology which combines field vegetation surveys with multispectral UAV data collected at two scales to estimate saltmarsh area and organic carbon storage at three saltmarshes in Loch Fleet (Scotland). We find that the Normalised Difference Vegetation Index (NDVI) values for surveyed saltmarsh vegetation communities, in combination with local tidal data, can be used to reliably estimate saltmarsh area. Using these area estimates, together with known plant community and soil organic carbon relationships, saltmarsh soil organic carbon storage is modelled. Based on our most reliable UAV-derived saltmarsh area estimates, we find that organic carbon storage is 15 %–20 % lower than previous area estimates would indicate. The methodology presented here potentially provides a cheap, affordable, and rapid method for saltmarsh mapping which could be implemented more widely to test and refine existing estimates of saltmarsh extent and is particularly well-suited to the mapping of small areas of saltmarsh environments.
    Subject code 333
    Language English
    Publishing date 2024-02-20
    Publishing country de
    Document type Book ; Online
    Database BASE - Bielefeld Academic Search Engine (life sciences selection)

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  2. Article: Best practice for upscaling soil organic carbon stocks in salt marshes

    Ladd, Cai J.T. / Smeaton, Craig / Skov, Martin W. / Austin, William E.N.

    Geoderma. 2022 Sept. 20,

    2022  

    Abstract: Calculating the amount of soil organic carbon (SOC) stored in coastal environments, including salt marshes, is needed to determine their role in mitigating the Climate Crisis. Several techniques exist to calculate the SOC content of a unit of land from ... ...

    Abstract Calculating the amount of soil organic carbon (SOC) stored in coastal environments, including salt marshes, is needed to determine their role in mitigating the Climate Crisis. Several techniques exist to calculate the SOC content of a unit of land from the upscaling of soil cores. However, no comprehensive assessment has been made on the performance of commonly used SOC upscaling techniques until now. We measured the SOC content of soil cores gathered from two Scottish salt marshes. Two SOC values were used for upscaling; SOC content for a 1 m standardised depth (as recommended by the IPCC), and SOC content of the modern marsh deposit (identified in the stratigraphy as a transition from organic-rich (marsh) to mineral-rich (intertidal flat) soil. Twenty-two upscaling techniques were used (SOC content × area, interpolative, and regression-based extrapolative calculations). Leave-one-out cross-validation procedures and prediction interval widths were used to assess the accuracy of each technique. Digital Terrain Models and Normalized Difference Vegetation Indices were used as covariate surfaces in the regression models. We found that marsh-scale SOC stocks varied by as much as fifty-two times depending on which sampling depth and upscaling technique was used. The largest differences emerged when comparing SOC stocks upscaled from 1 m deep and modern marsh deposits. Using the IPCC recommended 1 m sampling depth inflated the SOC stocks of salt marshes, as intertidal flat environments were included in the calculation. Ensemble regression models from the weighted average of seven machine learning algorithm outputs produced the highest upscaling accuracies across marshes and sampling depths. Simple SOC content × area calculations produced marsh-scale SOC stocks that were comparable to stock values produced by more advanced ensemble regression models. However, regression models produced detailed maps of SOC distribution across a marsh, and the associated uncertainty in the SOC values. Our findings are broadly applicable for other environments where large-scale SOC stock assessments and uncertainty are needed.
    Keywords algorithms ; climate ; landscapes ; littoral zone ; marshes ; prediction ; soil ; soil organic carbon ; stratigraphy ; uncertainty
    Language English
    Dates of publication 2022-0920
    Publishing place Elsevier B.V.
    Document type Article
    Note Pre-press version
    ZDB-ID 281080-3
    ISSN 1872-6259 ; 0016-7061
    ISSN (online) 1872-6259
    ISSN 0016-7061
    DOI 10.1016/j.geoderma.2022.116188
    Database NAL-Catalogue (AGRICOLA)

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  3. Article ; Online: Organic carbon accumulation in British saltmarshes.

    Smeaton, Craig / Garrett, Ed / Koot, Martha B / Ladd, Cai J T / Miller, Lucy C / McMahon, Lucy / Foster, Bradley / Barlow, Natasha L M / Blake, William / Gehrels, W Roland / Skov, Martin W / Austin, William E N

    The Science of the total environment

    2024  Volume 926, Page(s) 172104

    Abstract: Saltmarshes are a crucial component of the coastal carbon (C) system and provide a natural climate regulation service through the accumulation and long-term storage of organic carbon (OC) in their soils. These coastal ecosystems are under growing ... ...

    Abstract Saltmarshes are a crucial component of the coastal carbon (C) system and provide a natural climate regulation service through the accumulation and long-term storage of organic carbon (OC) in their soils. These coastal ecosystems are under growing pressure from a changing climate and increasing anthropogenic disturbance. To manage and protect these ecosystems for C and to allow their inclusion in emissions and natural-capital accounting, as well as carbon markets, accurate and reliable estimates of OC accumulation are required. However, globally, such data are rare or of varying quality. Here, we quantify sedimentation rates and OC densities for 21 saltmarshes in Great Britain (GB). We estimate that, on average, saltmarshes accumulate OC at a rate of 110.88 ± 43.12 g C m
    Language English
    Publishing date 2024-03-29
    Publishing country Netherlands
    Document type Journal Article
    ZDB-ID 121506-1
    ISSN 1879-1026 ; 0048-9697
    ISSN (online) 1879-1026
    ISSN 0048-9697
    DOI 10.1016/j.scitotenv.2024.172104
    Database MEDical Literature Analysis and Retrieval System OnLINE

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  4. Article ; Online: Coring and compaction

    Smeaton, Craig / Barlow, Natasha L.M. / Austin, William E.N.

    best practice in blue carbon stock and burial estimations

    2020  

    Abstract: A comparison of gouge and hammer coring techniques in intertidal wetland soils highlights a significant effect of soil compaction of up to 28% associated with the widely applied hammer coring method employed in Blue Carbon research. Hammer coring reduces ...

    Abstract A comparison of gouge and hammer coring techniques in intertidal wetland soils highlights a significant effect of soil compaction of up to 28% associated with the widely applied hammer coring method employed in Blue Carbon research. Hammer coring reduces the thickness of the soil profile and increases the dry bulk density, which results in an overestimation of the soil OC stock of up to 22%. In saltmarshes with multiple different soil units, we show that hammer coring is unsuitable for the calculation of OC stocks and should be avoided in favour of Russian or gouge cores. Compaction changes both soil dry bulk density and porosity and we show that resultant radiometric chronologies are compromised, almost doubling mass accumulation rates. While we show that the OC (%) content of these sediments is largely unchanged by coring method, the implication for OC burial rates are profound because of the significant effect of hammer coring on the calculation of soil mass accumlation rates.
    Subject code 550
    Language English
    Publisher Elsevier
    Publishing country de
    Document type Article ; Online
    Database BASE - Bielefeld Academic Search Engine (life sciences selection)

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  5. Article: Coring and compaction: Best practice in blue carbon stock and burial estimations

    Smeaton, Craig / Austin, William E.N / Barlow, Natasha L.M

    Geoderma. 2020 Apr. 01, v. 364

    2020  

    Abstract: A comparison of gouge and hammer coring techniques in intertidal wetland soils highlights a significant effect of soil compaction of up to 28% associated with the widely applied hammer coring method employed in Blue Carbon research. Hammer coring reduces ...

    Abstract A comparison of gouge and hammer coring techniques in intertidal wetland soils highlights a significant effect of soil compaction of up to 28% associated with the widely applied hammer coring method employed in Blue Carbon research. Hammer coring reduces the thickness of the soil profile and increases the dry bulk density, which results in an overestimation of the soil OC stock of up to 22%. In saltmarshes with multiple different soil units, we show that hammer coring is unsuitable for the calculation of OC stocks and should be avoided in favour of Russian or gouge cores. Compaction changes both soil dry bulk density and porosity and we show that resultant radiometric chronologies are compromised, almost doubling mass accumulation rates. While we show that the OC (%) content of these sediments is largely unchanged by coring method, the implication for OC burial rates are profound because of the significant effect of hammer coring on the calculation of soil mass accumlation rates.
    Keywords blue carbon ; bulk density ; carbon sinks ; littoral zone ; porosity ; radiometry ; salt marshes ; sediments ; soil compaction ; soil profiles ; wetland soils
    Language English
    Dates of publication 2020-0401
    Publishing place Elsevier B.V.
    Document type Article
    ZDB-ID 281080-3
    ISSN 1872-6259 ; 0016-7061
    ISSN (online) 1872-6259
    ISSN 0016-7061
    DOI 10.1016/j.geoderma.2020.114180
    Database NAL-Catalogue (AGRICOLA)

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  6. Book ; Conference proceedings: Biogeochemical controls on palaeoceanographic environmental proxies

    Austin, William E. N

    (Geological Society special publication ; 303)

    2008  

    Event/congress Geological Society of London Meeting on Biogeochemical Controls on Palaeoceanographic Proxies (2005.10.03-04, London)
    Author's details ed. by W.E.N. Austin
    Series title Geological Society special publication ; 303
    Keywords Biogeochemical cycles ; Biomineralization ; Paleoceanography
    Language English
    Size 192 S., Ill., graph. Darst.
    Publisher Geological Soc
    Publishing place London
    Document type Book ; Conference proceedings
    ISBN 9781862392571 ; 1862392579
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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  7. Article ; Online: Impacts of ocean acidification on intertidal benthic foraminiferal growth and calcification.

    Guamán-Guevara, Fabricio / Austin, Heather / Hicks, Natalie / Streeter, Richard / Austin, William E N

    PloS one

    2019  Volume 14, Issue 8, Page(s) e0220046

    Abstract: Foraminifera are expected to be particularly susceptible to future changes in ocean carbonate chemistry as a function of increased atmospheric CO2. Studies in an experimental recirculating seawater system were performed with a dominant benthic ... ...

    Abstract Foraminifera are expected to be particularly susceptible to future changes in ocean carbonate chemistry as a function of increased atmospheric CO2. Studies in an experimental recirculating seawater system were performed with a dominant benthic foraminiferal species collected from intertidal mudflats. We investigated the experimental impacts of ocean acidification on survival, growth/calcification, morphology and the biometric features of a calcareous species Elphidium williamsoni. Foraminifera were exposed for 6 weeks to four different pH treatments that replicated future scenarios of a high CO2 atmosphere resulting in lower seawater pH. Results revealed that declining seawater pH caused a decline in foraminiferal survival rate and growth/calcification (mainly through test weight reduction). Scanning electron microscopy image analysis of live specimens at the end of the experimental period show changes in foraminiferal morphology with clear signs of corrosion and cracking on the test surface, septal bridges, sutures and feeding structures of specimens exposed to the lowest pH conditions. These findings suggest that the morphological changes observed in shell feeding structures may serve to alter: (1) foraminiferal feeding efficiency and their long-term ecological competitiveness, (2) the energy transferred within the benthic food web with a subsequent shift in benthic community structures and (3) carbon cycling and total CaCO3 production, both highly significant processes in coastal waters. These experimental results open-up the possibility of modelling future impacts of ocean acidification on both calcification and dissolution in benthic foraminifera within mid-latitude intertidal environments, with potential implications for understanding the changing marine carbon cycle.
    MeSH term(s) Calcification, Physiologic/drug effects ; Carbonates/analysis ; Carbonates/pharmacology ; Foraminifera/drug effects ; Foraminifera/growth & development ; Foraminifera/physiology ; Hydrogen-Ion Concentration ; Seawater/chemistry ; Survival Analysis ; Time Factors
    Chemical Substances Carbonates
    Language English
    Publishing date 2019-08-21
    Publishing country United States
    Document type Journal Article ; Research Support, Non-U.S. Gov't
    ISSN 1932-6203
    ISSN (online) 1932-6203
    DOI 10.1371/journal.pone.0220046
    Database MEDical Literature Analysis and Retrieval System OnLINE

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  8. Book ; Conference proceedings: Quaternary shelf sea palaeoceanography

    Austin, William E. N

    recent developments in Europe ; a collection of papers arising from the Geoscience 2000 meeting, organized by the Geological Society of London at the University of Manchester, 17 - 20 April 2000

    (Marine geology : Special issue ; 191.2002,3/4)

    2002  

    Institution Geological Society
    Event/congress Geoscience 2000 (2000.04.17-20, Manchester)
    Author's details ed. by William E. N. Austin
    Series title Marine geology : Special issue ; 191.2002,3/4
    Language English
    Size S. 88-188, graph. Darst., Kt
    Publisher Elsevier
    Publishing place Amsterdam u.a.
    Document type Book ; Conference proceedings
    Note Literaturangaben
    Database Library catalogue of the German National Library of Science and Technology (TIB), Hannover

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  9. Article: Fjords as Aquatic Critical Zones (ACZs)

    Bianchi, Thomas S / Arndt, Sandra / Austin, William E.N / Benn, Douglas I / Bertrand, Sebastien / Cui, Xingqian / Faust, Johan C / Koziorowska-Makuch, Katarzyna / Moy, Christopher M / Savage, Candida / Smeaton, Craig / Smith, Richard W / Syvitski, Jaia

    Earth-science reviews. 2020 Apr., v. 203

    2020  

    Abstract: In recent decades, the land-ocean aquatic continuum, commonly defined as the interface, or transition zone, between terrestrial ecosystems and the open ocean, has undergone dramatic changes. On-going work has stressed the importance of treating Aquatic ... ...

    Abstract In recent decades, the land-ocean aquatic continuum, commonly defined as the interface, or transition zone, between terrestrial ecosystems and the open ocean, has undergone dramatic changes. On-going work has stressed the importance of treating Aquatic Critical Zones (ACZs) as a sensitive system needing intensive investigation. Here, we discuss fjords as an ACZ in the context of sedimentological, geochemical, and climatic impacts. These diverse physical features of fjords are key in controlling the sources, transport, and burial of organic matter in the modern era and over the Holocene. High sediment accumulation rates in fjord sediments allow for high-resolution records of past climate and environmental change where multiple proxies can be applied to fjord sediments that focus on either marine or terrestrial-derived components.Humans through land-use change and climatic stressors are having an impact on the larger carbon stores in fjords. Sediment delivery whether from accelerating erosion (e.g. mining, deforestation, road building, agriculture) or from sequestration of fluvial sediment behind dams has been seriously altered in the Anthropocene. Climate change affecting rainfall and river discharge into fjords will impact the thickness and extent of the low-salinity layer in the upper reaches of the fjord, slowing the rate of the overturning circulation and deep-water renewal – thereby impacting bottom water oxygen concentrations.
    Keywords Anthropocene epoch ; Holocene epoch ; carbon sinks ; climate ; climate change ; deforestation ; land use change ; mining ; organic matter ; oxygen ; rain ; river flow ; sediments ; terrestrial ecosystems
    Language English
    Dates of publication 2020-04
    Publishing place Elsevier B.V.
    Document type Article
    ZDB-ID 1792-9
    ISSN 0012-8252
    ISSN 0012-8252
    DOI 10.1016/j.earscirev.2020.103145
    Database NAL-Catalogue (AGRICOLA)

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  10. Article ; Online: The impact of ocean acidification on the functional morphology of foraminifera.

    Khanna, Nikki / Godbold, Jasmin A / Austin, William E N / Paterson, David M

    PloS one

    2013  Volume 8, Issue 12, Page(s) e83118

    Abstract: Culturing experiments were performed on sediment samples from the Ythan Estuary, N. E. Scotland, to assess the impacts of ocean acidification on test surface ornamentation in the benthic foraminifer Haynesina germanica. Specimens were cultured for 36 ... ...

    Abstract Culturing experiments were performed on sediment samples from the Ythan Estuary, N. E. Scotland, to assess the impacts of ocean acidification on test surface ornamentation in the benthic foraminifer Haynesina germanica. Specimens were cultured for 36 weeks at either 380, 750 or 1000 ppm atmospheric CO2. Analysis of the test surface using SEM imaging reveals sensitivity of functionally important ornamentation associated with feeding to changing seawater CO2 levels. Specimens incubated at high CO2 levels displayed evidence of shell dissolution, a significant reduction and deformation of ornamentation. It is clear that these calcifying organisms are likely to be vulnerable to ocean acidification. A reduction in functionally important ornamentation could lead to a reduction in feeding efficiency with consequent impacts on this organism's survival and fitness.
    MeSH term(s) Acids/analysis ; Acids/pharmacology ; Animals ; Carbon Dioxide/chemistry ; Carbon Dioxide/pharmacology ; Dose-Response Relationship, Drug ; Ecosystem ; Foraminifera/cytology ; Foraminifera/drug effects ; Foraminifera/growth & development ; Foraminifera/ultrastructure ; Hydrogen-Ion Concentration ; Microscopy, Electron, Scanning ; Oceans and Seas ; Seawater/chemistry
    Chemical Substances Acids ; Carbon Dioxide (142M471B3J)
    Language English
    Publishing date 2013-12-17
    Publishing country United States
    Document type Journal Article ; Research Support, Non-U.S. Gov't
    ISSN 1932-6203
    ISSN (online) 1932-6203
    DOI 10.1371/journal.pone.0083118
    Database MEDical Literature Analysis and Retrieval System OnLINE

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