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A 1100-year multi-proxy palaeoenvironmental record from Lake Höglwörth, Bavaria, Germany
Published 2023-11-01“…This period was followed by enhanced deforestation that led to a more open landscape and soil erosion, visible in increased allochthonous input from <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M5" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mn mathvariant="normal">1240</mn><mrow><mo>-</mo><mn mathvariant="normal">120</mn></mrow><mrow><mo>+</mo><mn mathvariant="normal">110</mn></mrow></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="45pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="0864c09116df22be3e6e3052404dfadd"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="egqsj-72-219-2023-ie00004.svg" width="45pt" height="17pt" src="egqsj-72-219-2023-ie00004.png"/></svg:svg></span></span> to <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M6" display="inline" overflow="scroll" dspmath="mathml"><mrow><msubsup><mn mathvariant="normal">1380</mn><mrow><mo>-</mo><mn mathvariant="normal">110</mn></mrow><mrow><mo>+</mo><mn mathvariant="normal">90</mn></mrow></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="45pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="d8ba1a1009a04f576c1ccaa884746c17"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="egqsj-72-219-2023-ie00005.svg" width="45pt" height="17pt" src="egqsj-72-219-2023-ie00005.png"/></svg:svg></span></span> CE. …”
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Chronological and sedimentological investigations of the Late Pleistocene succession in Osterbylund (Schleswig-Holstein, Germany)
Published 2023-03-01“…Optically stimulated luminescence and <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msup><mi/><mn mathvariant="normal">230</mn></msup><mi mathvariant="normal">Th</mi><mo>/</mo><mi mathvariant="normal">U</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="43pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="86ea54c90efe5652b6f4857723d472ce"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="egqsj-72-57-2023-ie00001.svg" width="43pt" height="15pt" src="egqsj-72-57-2023-ie00001.png"/></svg:svg></span></span> dating, as well as pollen analyses, were undertaken with the aim to correlate the soils OBL 1 to OBL 4 to interglacials and interstadials. …”
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What do dust sinks tell us about their sources and past environmental dynamics? A case study for oxygen isotope stages 3–2 in the Middle Rhine Valley, Germany
Published 2023-08-01“…</p> <p>Distinct shifts in several proxy data supported by changes in isotope composition (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M4" display="inline" overflow="scroll" dspmath="mathml"><mrow class="chem"><msup><mi/><mn mathvariant="normal">87</mn></msup><mi mathvariant="normal">Sr</mi><msup><mo>/</mo><mn mathvariant="normal">86</mn></msup><mi mathvariant="normal">Sr</mi></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="49pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="3e742fac50d9344ff94fdf71fe05f27c"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="egqsj-72-163-2023-ie00001.svg" width="49pt" height="15pt" src="egqsj-72-163-2023-ie00001.png"/></svg:svg></span></span> and <span class="inline-formula"><i>ε</i></span>Nd) within the lower section are interpreted as changes in provenance and decreasing weathering simultaneously with an overall cooling and aridification towards the end of OIS 3 (after <span class="inline-formula">∼</span> 35 ka) and enhanced wind activity with significant input of coarse-grained material recycled from local sources related to increased landscape instability (after <span class="inline-formula">∼</span> 31.5 ka). …”
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