<?xml version="1.0" encoding="UTF-8"?>
<!DOCTYPE article PUBLIC "-//NLM//DTD JATS (Z39.96) Article Authoring DTD with MathML3 v1.4 20241031//EN" "https://jats.nlm.nih.gov/articleauthoring/1.4/JATS-articleauthoring1-4-mathml3.dtd">
<article xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mml="http://www.w3.org/1998/Math/MathML" article-type="data-paper" dtd-version="1.4" xml:lang="en">
<front>
<article-meta>
  <title-group>
    <article-title>[Article 201 - FAKE ARTICLE — DO NOT PUBLISH] Lorem Ipsum Sedimentation in the Dolor Sit Estuary: A Placeholder Dataset for Import-Pipeline Testing</article-title>
  </title-group>
  <contrib-group>
    <contrib contrib-type="author" corresp="yes">
      <contrib-id contrib-id-type="orcid">0000-0002-1825-0097</contrib-id>
      <name>
        <surname>Lorenzo</surname>
        <given-names>Ipsum A.</given-names>
      </name>
      <role vocab="credit" vocab-identifier="https://credit.niso.org/" vocab-term="Conceptualization" vocab-term-identifier="https://credit.niso.org/contributor-roles/conceptualization/">Conceptualization</role>
      <aff>
        <institution>Department of Placeholder Geosciences, Testus University, Testville, XX 29401, USA</institution>
      </aff>
      <email>i.lorenzo@example.edu</email>
    </contrib>
    <contrib contrib-type="author">
      <name>
        <surname>Harris</surname>
        <given-names>M. Scott</given-names>
      </name>
      <role vocab="earth-access" vocab-identifier="https://earthaccess.us/vocab/contributor-roles/" vocab-term="Research Advisor" vocab-term-identifier="https://earthaccess.us/vocab/contributor-roles/research-advisor/">Research Advisor</role>
      <role vocab="credit" vocab-identifier="https://credit.niso.org/" vocab-term="Conceptualization" vocab-term-identifier="https://credit.niso.org/contributor-roles/conceptualization/">Conceptualization</role>
      <email>scottharrisgeo@gmail.com</email>
    </contrib>
  </contrib-group>
  <permissions>
    <copyright-statement>© 2026 The Author(s).</copyright-statement>
    <copyright-year>2026</copyright-year>
    <license license-type="open-access" xlink:href="https://creativecommons.org/licenses/by/4.0/">
      <license-p>This work is licensed under a Creative Commons Attribution 4.0 International License (CC BY 4.0). The submitting author agreed to this license on behalf of all authors on 2026-08-02.</license-p>
    </license>
  </permissions>
  <abstract>
    <p>THIS IS A FAKE ARTICLE CREATED SOLELY TO TEST THE EARTH ACCESS IMPORT PIPELINE; IT CONTAINS NO REAL DATA AND MUST NOT BE PUBLISHED. Lorem ipsum dolor sit amet, we report a synthetic 14-day record of water level, along-channel velocity, and suspended-sediment concentration from the entirely fictional Placeholder Estuary. Consectetur adipiscing elit: five invented core sites (PC-01 through PC-05) and one invented ground-penetrating radar transect (T-01) were fabricated with a random-number generator on 2026-07-29. Sed do eiusmod tempor, net flux reverses between the synthetic spring and neap phases, with a fabricated landward transport of 0.42 ± 0.08 kg m⁻¹ s⁻¹ during the placeholder neap and a fabricated seaward transport of 1.13 ± 0.21 kg m⁻¹ s⁻¹ during the placeholder spring. Ut enim ad minim veniam, the dummy grain-size distributions fine landward from 2.1 φ to 6.8 φ. Duis aute irure dolor, none of these numbers mean anything; they exist so that figures, tables, equations, citations, and location data all travel through the JATS export and the OJS galley handoff at once. Excepteur sint occaecat cupidatat non proident, sunt in culpa qui officia deserunt mollit anim id est laborum.</p>
  </abstract>
  <kwd-group>
    <kwd>lorem ipsum</kwd>
    <kwd>placeholder sedimentology</kwd>
    <kwd>synthetic dataset</kwd>
    <kwd>pipeline testing</kwd>
    <kwd>JATS</kwd>
    <kwd>ground-penetrating radar</kwd>
    <kwd>fake data</kwd>
    <kwd>Placeholder Estuary</kwd>
  </kwd-group>
  <kwd-group kwd-group-type="gcmd-science-keywords" vocab="NASA GCMD Science Keywords" vocab-identifier="https://gcmd.earthdata.nasa.gov/kms/concepts/concept_scheme/sciencekeywords">
    <kwd vocab-term-identifier="c58320e6-3f1d-4c36-9bee-6bad73404c21">COASTAL LANDFORMS</kwd>
  </kwd-group>
  <kwd-group kwd-group-type="agu-index-terms" vocab="AGU Index Terms" vocab-identifier="https://www.agu.org/publications/authors/journals/index-terms">
    <kwd vocab-term-identifier="3002">Continental shelf and slope processes (4219)</kwd>
  </kwd-group>
</article-meta>
</front>
<body>
<sec id="sec809">
  <title>INTRODUCTION</title>
  <p>Lorem ipsum dolor sit amet, estuarine sediment transport is the placeholder problem this fake article pretends to address<xref ref-type="bibr" rid="ref172">(Jasiewicz &amp; Stepinski, 2013)</xref>. Consectetur adipiscing elit, terrain-pattern methods have been applied to comparable invented settings<xref ref-type="bibr" rid="ref173">(Jasiewicz et al., 2014)</xref>, and toolbox implementations exist for the same imaginary purpose<xref ref-type="bibr" rid="ref174">(Jasiewicz et al., 2015)</xref>. None of that is relevant here, because the data below were produced by a random-number generator.</p>
  <p>Sed do eiusmod tempor incididunt ut labore, machine-learning classification of synthetic surfaces has been demonstrated at planetary scale<xref ref-type="bibr" rid="ref175">(Stepinski &amp; Vilalta, 2010)</xref>, extended to pattern analysis workflows<xref ref-type="bibr" rid="ref176">(Stepinski et al., 2015)</xref>, and reimplemented in several statistical environments<xref ref-type="bibr" rid="ref177">(GmbH &amp; Sänger, n.d.)</xref>. We adopt none of these methods and simply assert our results.</p>
  <p>The three objectives of this fake study are stated below so that the importer has a list to carry through to JATS.</p>
  <list list-type="order">
    <list-item>
      <p>Quantify the fabricated net sediment flux at five invented core sites.</p>
    </list-item>
    <list-item>
      <p>Compare the fabricated flux against a placeholder tidal asymmetry index.</p>
    </list-item>
    <list-item>
      <p>Demonstrate that figures, tables, equations, citations, and location data survive the import.</p>
    </list-item>
  </list>
</sec>
<sec id="sec814">
  <title>METHODS</title>
  <sec id="sec815">
    <title>Study Area</title>
    <p>The Placeholder Estuary does not exist. Its invented centroid lies at 32.7963° N, 79.9401° W (WGS 84), and the fabricated tidal range is 1.6 m. The sampling design is shown in the figure below, following the mapping conventions of<xref ref-type="bibr" rid="ref178">(Wilson et al., 2007)</xref>.</p>
    <fig id="fig149" position="float">
      <caption>
        <p>Placeholder Estuary sampling design. Red circles mark the five invented core sites (PC-01 to PC-05); the blue line is the invented ground-penetrating radar transect T-01. Coordinates are WGS 84 decimal degrees. All features are fabricated.</p>
      </caption>
      <alt-text>Placeholder Estuary sampling design. Red circles mark the five invented core sites (PC-01 to PC-05); the blue line is the invented ground-penetrating radar transect T-01. Coordinates are WGS 84 decimal degrees. All features are fabricated.</alt-text>
      <graphic xlink:href="fig149-figure1-study-area.png"/>
    </fig>
  </sec>
  <sec id="sec817">
    <title>Data Collection</title>
    <p>No data were collected. For the purposes of this fixture we describe the following imaginary instrumentation, after the acquisition practice summarised by<xref ref-type="bibr" rid="ref179">(Ostrowski et al., 2017)</xref>:</p>
    <list list-type="bullet">
      <list-item>
        <p>One nonexistent acoustic Doppler current profiler at 1 Hz.</p>
        <list list-type="bullet">
          <list-item>
            <p>Mounted on an imaginary bottom frame.</p>
          </list-item>
          <list-item>
            <p>Logged to a hard drive that was never purchased.</p>
          </list-item>
        </list>
      </list-item>
      <list-item>
        <p>One nonexistent optical backscatter sensor at 1 m above bed.</p>
      </list-item>
      <list-item>
        <p>One nonexistent 400 MHz ground-penetrating radar antenna.</p>
      </list-item>
      <list-item>
        <p>Five nonexistent vibracores, each 3 m long.</p>
      </list-item>
    </list>
    <p>Sampling ran from 2026-03-01 to 2026-03-15 in an imaginary calendar. Positional accuracy was asserted to be ±0.03 m, and elevations are referenced to a datum we made up.</p>
  </sec>
  <sec id="sec821">
    <title>Data Analysis</title>
    <p>Instantaneous depth-integrated suspended-sediment flux (<italic>q</italic><sub>s</sub>) was computed as the product of concentration and velocity:</p>
    <disp-formula id="eq156">
      <label>(1)</label>
      <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" display="block">
        <mml:semantics>
          <mml:mrow><mml:msub><mml:mi>q</mml:mi><mml:mi>s</mml:mi></mml:msub><mml:mo>=</mml:mo><mml:msubsup><mml:mo>∫</mml:mo><mml:mn>0</mml:mn><mml:mi>h</mml:mi></mml:msubsup><mml:mi>C</mml:mi><mml:mrow><mml:mo>(</mml:mo><mml:mi>z</mml:mi><mml:mo>)</mml:mo></mml:mrow><mml:mi>u</mml:mi><mml:mrow><mml:mo>(</mml:mo><mml:mi>z</mml:mi><mml:mo>)</mml:mo></mml:mrow><mml:mi>d</mml:mi><mml:mi>z</mml:mi></mml:mrow>
          <mml:annotation encoding="application/x-tex"><![CDATA[{q}_{s}=\int_{0}^{h} C\left(z\right)u\left(z\right)dz]]></mml:annotation>
        </mml:semantics>
      </mml:math>
    </disp-formula>
    <p>Here (<italic>C</italic>) is the fabricated concentration, (<italic>u</italic>) the fabricated along-channel velocity, and (<italic>h</italic>) the fabricated water depth. The tidal asymmetry index follows a made-up ratio of peak velocities, and the result is<bold>entirely without physical meaning</bold>:</p>
    <disp-formula id="eq157">
      <label>(2)</label>
      <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" display="block">
        <mml:semantics>
          <mml:mrow><mml:msub><mml:mi>A</mml:mi><mml:mi>t</mml:mi></mml:msub><mml:mo>=</mml:mo><mml:mfrac><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mi>flood</mml:mi></mml:msub><mml:mo>-</mml:mo><mml:msub><mml:mi>u</mml:mi><mml:mi>ebb</mml:mi></mml:msub></mml:mrow><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mi>flood</mml:mi></mml:msub><mml:mo>+</mml:mo><mml:msub><mml:mi>u</mml:mi><mml:mi>ebb</mml:mi></mml:msub></mml:mrow></mml:mfrac></mml:mrow>
          <mml:annotation encoding="application/x-tex"><![CDATA[{A}_{t}=\frac{{u}_{flood}-{u}_{ebb}}{{u}_{flood}+{u}_{ebb}}]]></mml:annotation>
        </mml:semantics>
      </mml:math>
    </disp-formula>
    <p>Settling velocity was taken from an invented Stokes-type relation, with a root term included so the OMML-to-LaTeX conversion has something to chew on:</p>
    <disp-formula id="eq158">
      <label>(3)</label>
      <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" display="block">
        <mml:semantics>
          <mml:mrow><mml:msub><mml:mi>w</mml:mi><mml:mi>s</mml:mi></mml:msub><mml:mo>=</mml:mo><mml:mfrac><mml:mrow><mml:mrow><mml:mo>(</mml:mo><mml:msub><mml:mi>ρ</mml:mi><mml:mi>s</mml:mi></mml:msub><mml:mo>-</mml:mo><mml:mi>ρ</mml:mi><mml:mo>)</mml:mo></mml:mrow><mml:mi>g</mml:mi><mml:msup><mml:mi>d</mml:mi><mml:mn>2</mml:mn></mml:msup></mml:mrow><mml:mrow><mml:mn>18</mml:mn><mml:mi>μ</mml:mi></mml:mrow></mml:mfrac><mml:mo>+</mml:mo><mml:msqrt><mml:mfrac><mml:mi>τ</mml:mi><mml:mi>ρ</mml:mi></mml:mfrac></mml:msqrt></mml:mrow>
          <mml:annotation encoding="application/x-tex"><![CDATA[{w}_{s}=\frac{\left({\rho }_{s}-\rho \right)g{d}^{2}}{18\mu }+\sqrt{\frac{\tau }{\rho }}]]></mml:annotation>
        </mml:semantics>
      </mml:math>
    </disp-formula>
    <p>All processing was performed with software that we did not write, on data that do not exist, following a workflow we have not read<xref ref-type="bibr" rid="ref180">(Stepinski &amp; Vilalta, n.d.)</xref>.</p>
  </sec>
</sec>
<sec id="sec826">
  <title>RESULTS</title>
  <p>The synthetic record shows a clear spring–neap modulation, because that is how the generator was written.</p>
  <fig id="fig150" position="float">
    <caption>
      <p>Synthetic 14-day record at invented station PC-03. (A) Water level relative to a made-up MLLW datum. (B) Along-channel velocity, positive toward flood. (C) Suspended-sediment concentration at 1 m above bed. Values are generated, not measured.</p>
    </caption>
    <alt-text>Synthetic 14-day record at invented station PC-03. (A) Water level relative to a made-up MLLW datum. (B) Along-channel velocity, positive toward flood. (C) Suspended-sediment concentration at 1 m above bed. Values are generated, not measured.</alt-text>
    <graphic xlink:href="fig150-figure2-time-series.png"/>
  </fig>
  <p>Fabricated summary statistics for the five invented core sites are given in the table below. The reported uncertainties are also fabricated.</p>
  <p>Note that the numbers below were chosen to look plausible and to include a range of decimal precisions, negative values, and a non-ASCII degree sign.</p>
  <table-wrap id="tbl154" position="float">
    <caption>
      <p>Fabricated summary statistics for the five invented core sites. Positive net flux is seaward. Coordinates are WGS 84. Uncertainties are one standard error of a distribution that does not exist.</p>
    </caption>
    <table frame="hsides" rules="groups">
<thead>
<tr>
  <th>Site</th>
  <th>Latitude (°N)</th>
  <th>Longitude (°W)</th>
  <th>Mean d₅₀ (φ)</th>
  <th>Net flux (kg m⁻¹ s⁻¹)</th>
</tr>
</thead>
<tbody>
<tr>
  <td>PC-01</td>
  <td>32.7920</td>
  <td>−80.0550</td>
  <td>2.1</td>
  <td>+1.13 ± 0.21</td>
</tr>
<tr>
  <td>PC-02</td>
  <td>32.7860</td>
  <td>−79.9860</td>
  <td>3.4</td>
  <td>+0.64 ± 0.14</td>
</tr>
<tr>
  <td>PC-03</td>
  <td>32.8120</td>
  <td>−79.9020</td>
  <td>4.4</td>
  <td>−0.08 ± 0.05</td>
</tr>
<tr>
  <td>PC-04</td>
  <td>32.7550</td>
  <td>−79.9410</td>
  <td>5.9</td>
  <td>−0.31 ± 0.09</td>
</tr>
<tr>
  <td>PC-05</td>
  <td>32.7410</td>
  <td>−80.0210</td>
  <td>6.8</td>
  <td>−0.42 ± 0.08</td>
</tr>
</tbody>
    </table>
  </table-wrap>
  <p>Grain size fines landward across the invented transect, which is the pattern we asked the generator to produce.</p>
  <p>The distributions are unimodal by construction and should not be interpreted.</p>
  <fig id="fig151" position="float">
    <caption>
      <p>Placeholder grain-size distributions at three invented core sites, expressed in phi units. Curves are Gaussian by construction.</p>
    </caption>
    <alt-text>Placeholder grain-size distributions at three invented core sites, expressed in phi units. Curves are Gaussian by construction.</alt-text>
    <graphic xlink:href="fig151-figure3-grain-size.png"/>
  </fig>
  <p>The invented radar transect is presented next, mainly so that a wide raster figure travels through the pipeline.</p>
  <fig id="fig152" position="float">
    <caption>
      <p>Synthetic 400 MHz radargram along invented transect T-01. Three fabricated reflectors are visible at approximately 19, 60, and 120 ns two-way travel time. No survey was conducted.</p>
    </caption>
    <alt-text>Synthetic 400 MHz radargram along invented transect T-01. Three fabricated reflectors are visible at approximately 19, 60, and 120 ns two-way travel time. No survey was conducted.</alt-text>
    <graphic xlink:href="fig152-figure5-radargram.png"/>
  </fig>
  <p>Reflector picks and their fabricated depth conversions are summarised below, using an assumed velocity of 0.06 m ns⁻¹.</p>
  <p>The final column is intentionally text rather than numeric, to check mixed-type table handling.</p>
  <table-wrap id="tbl155" position="float">
    <caption>
      <p>Fabricated ground-penetrating radar reflector picks along invented transect T-01. Depths assume a constant velocity of 0.06 m ns⁻¹.</p>
    </caption>
    <table frame="hsides" rules="groups">
<thead>
<tr>
  <th>Reflector</th>
  <th>TWT (ns)</th>
  <th>Depth (m)</th>
  <th>Continuity</th>
  <th>Interpretation</th>
</tr>
</thead>
<tbody>
<tr>
  <td>R1</td>
  <td>19.2</td>
  <td>0.58</td>
  <td>continuous</td>
  <td>invented modern surface</td>
</tr>
<tr>
  <td>R2</td>
  <td>60.4</td>
  <td>1.81</td>
  <td>semi-continuous</td>
  <td>invented ravinement</td>
</tr>
<tr>
  <td>R3</td>
  <td>120.7</td>
  <td>3.62</td>
  <td>discontinuous</td>
  <td>invented Pleistocene top</td>
</tr>
</tbody>
    </table>
  </table-wrap>
</sec>
<sec id="sec835">
  <title>DISCUSSION</title>
  <p>Ut enim ad minim veniam, the fabricated reversal in net flux between spring and neap is consistent with the fabricated asymmetry index, which is unsurprising because both were drawn from the same generator. Comparable synthetic exercises have been described in the multiscale terrain literature<xref ref-type="bibr" rid="ref178">(Wilson et al., 2007)</xref>, in prominence and isolation computation<xref ref-type="bibr" rid="ref181">(Kirmse &amp; de Ferranti, 2017)</xref>, and in pockmark characterisation<xref ref-type="bibr" rid="ref182">(Gafeira et al., 2018)</xref>.</p>
  <sec id="sec837">
    <title>Limitations of the Fabricated Dataset</title>
    <p>The principal limitation is that none of this happened. A second limitation is that the hillshade conventions we did not use are nonetheless cited<xref ref-type="bibr" rid="ref183">(Horn, 1981)</xref>, as are recent reviews of terrain identification<xref ref-type="bibr" rid="ref184">(Nampoothiri et al., 2021)</xref>and deep-learning applications to elevation models<xref ref-type="bibr" rid="ref185">(Ruiz-Lendínez et al., 2023)</xref>.</p>
    <sec id="sec839">
      <title>Implications for the Import Pipeline</title>
      <p>If this document imports cleanly, the pipeline handles three heading levels, five figures, two tables, three display equations, two list types, inline marks, and fourteen Zotero citations in a single pass.</p>
      <fig id="fig153" position="float">
        <caption>
          <p>Schematic conceptual model of fabricated flux pathways in the Placeholder Estuary. Arrow width indicates invented relative magnitude. ETM denotes the imaginary estuarine turbidity maximum.</p>
        </caption>
        <alt-text>Schematic conceptual model of fabricated flux pathways in the Placeholder Estuary. Arrow width indicates invented relative magnitude. ETM denotes the imaginary estuarine turbidity maximum.</alt-text>
        <graphic xlink:href="fig153-figure4-flux-model.png"/>
      </fig>
      <p>Every number in this article is fabricated. Any resemblance to a real estuary, real sediment, or real science is coincidental and unintended.</p>
    </sec>
  </sec>
</sec>
<sec id="sec842">
  <title>CONCLUSIONS</title>
  <p>A fake dataset was fabricated, described, plotted, tabulated, and cited. The purpose of this article is to be imported, not read. If you are reading it in a published journal, something has gone wrong and it should be withdrawn immediately. Excepteur sint occaecat cupidatat non proident.</p>
</sec>
<sec id="sec844">
  <title>CONFLICT OF INTEREST</title>
  <p>The authors of this fake article are also fake and therefore declare no competing interests, financial or otherwise.</p>
</sec>
<sec id="sec846">
  <title>DATA AVAILABILITY</title>
  <p>All placeholder data described in this fake article are fabricated and are not deposited anywhere. In a real submission this statement would carry a repository DOI, for example https://doi.org/10.5281/zenodo.0000000, together with the licence under which the dataset is released. The synthetic files accompanying this fixture (locations CSV, supplementary workbook) are part of the test bundle only.</p>
</sec>
<sec sec-type="data-availability" id="sec-data-availability">
  <title>Data Availability</title>
  <p>In the appendix</p>
</sec>
<sec sec-type="conflict-of-interest" id="sec-conflict-of-interest">
  <title>Competing Interests</title>
  <p>The authors declare no competing interests.</p>
</sec>
</body>
<back>
<ack>
  <title>Contributions and Acknowledgments</title>
  <p>Ipsum A. Lorenzo: Conceptualization.</p>
  <p>M. Scott Harris: Research Advisor, Conceptualization.</p>
  <p>Jane Doe: Investigation, Lab operations support — lab.</p>
  <p>John Doe: Investigation — field.</p>
  <p>Jim Doe: Resources.</p>
  <p>This fake article was generated on 2026-07-29 to exercise the Earth Access import pipeline. No funding supported it because it does not exist. In a real submission this paragraph would name the grant, for example Award No. PLACEHOLDER-000000 from the Fictional Science Foundation, and would thank the invented field crew of the R/V Nonexistent for their imaginary assistance.</p>
  <p>Subject terms (NASA GCMD Science Keywords): EARTH SCIENCE &gt; SOLID EARTH &gt; GEOMORPHIC LANDFORMS/PROCESSES &gt; COASTAL LANDFORMS.</p>
  <p>Subject terms (AGU Index Terms): MARINE GEOLOGY AND GEOPHYSICS &gt; Continental shelf and slope processes.</p>
</ack>
<ref-list>
  <title>References</title>
  <ref id="ref172">
    <element-citation publication-type="journal">
      <person-group person-group-type="author">
        <name>
          <surname>Jasiewicz</surname>
          <given-names>Jarosław</given-names>
        </name>
        <name>
          <surname>Stepinski</surname>
          <given-names>Tomasz F.</given-names>
        </name>
      </person-group>
      <year>2013</year>
      <article-title>Geomorphons — a pattern recognition approach to classification and mapping of landforms</article-title>
      <source>Geomorphology</source>
      <volume>182</volume>
      <fpage>147</fpage>
      <lpage>156</lpage>
      <pub-id pub-id-type="doi">10.1016/j.geomorph.2012.11.005</pub-id>
      <uri>http://www.sciencedirect.com/science/article/pii/S0169555X12005028</uri>
    </element-citation>
  </ref>
  <ref id="ref173">
    <element-citation publication-type="journal">
      <person-group person-group-type="author">
        <name>
          <surname>Jasiewicz</surname>
          <given-names>Jaroslaw</given-names>
        </name>
        <name>
          <surname>Netzel</surname>
          <given-names>Pawel</given-names>
        </name>
        <name>
          <surname>Stepinski</surname>
          <given-names>Tomasz F.</given-names>
        </name>
      </person-group>
      <year>2014</year>
      <article-title>Landscape similarity, retrieval, and machine mapping of physiographic units</article-title>
      <source>Geomorphology</source>
      <volume>221</volume>
      <fpage>104</fpage>
      <lpage>112</lpage>
      <pub-id pub-id-type="doi">10.1016/j.geomorph.2014.06.011</pub-id>
      <uri>http://dx.doi.org/10.1016/j.geomorph.2014.06.011</uri>
    </element-citation>
  </ref>
  <ref id="ref174">
    <element-citation publication-type="journal">
      <person-group person-group-type="author">
        <name>
          <surname>Jasiewicz</surname>
          <given-names>Jarosław</given-names>
        </name>
        <name>
          <surname>Netzel</surname>
          <given-names>Paweł</given-names>
        </name>
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