Nonlinear increase in seawater <sup>87</sup>Sr ∕ <sup>86</sup>Sr in the Oligocene to early Miocene and implications for climate-sensitive weathering
<p>The <span class="inline-formula"><sup>87</sup></span>Sr <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M8" display="inline" overflow="scroll" dspmath="mathml&...
| Main Authors: | , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2024-01-01
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| Series: | Climate of the Past |
| Online Access: | https://cp.copernicus.org/articles/20/25/2024/cp-20-25-2024.pdf |
| Summary: | <p>The <span class="inline-formula"><sup>87</sup></span>Sr <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M8" display="inline" overflow="scroll" dspmath="mathml"><mo>/</mo></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="fb147fccdcf98a9911cf3d26a8f6dc33"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="cp-20-25-2024-ie00004.svg" width="8pt" height="14pt" src="cp-20-25-2024-ie00004.png"/></svg:svg></span></span> <span class="inline-formula"><sup>86</sup></span>Sr of marine carbonates provides a key constraint on the balance of continental weathering and hydrothermal Sr fluxes to the ocean, and the mid-Oligocene to mid-Miocene period features the most rapid rates of increase in the <span class="inline-formula"><sup>87</sup></span>Sr <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M11" display="inline" overflow="scroll" dspmath="mathml"><mo>/</mo></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="165b352473919034209a9d51d0eaf41d"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="cp-20-25-2024-ie00005.svg" width="8pt" height="14pt" src="cp-20-25-2024-ie00005.png"/></svg:svg></span></span> <span class="inline-formula"><sup>86</sup></span>Sr of the Cenozoic. Because previous records of the <span class="inline-formula"><sup>87</sup></span>Sr <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M14" display="inline" overflow="scroll" dspmath="mathml"><mo>/</mo></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="539a58614ea8688159b8effbc6d3da8d"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="cp-20-25-2024-ie00006.svg" width="8pt" height="14pt" src="cp-20-25-2024-ie00006.png"/></svg:svg></span></span> <span class="inline-formula"><sup>86</sup></span>Sr increase with time were based on biostratigraphically defined age models in diverse locations, it was difficult to unambiguously distinguish million-year-scale variations in the rate of <span class="inline-formula"><sup>87</sup></span>Sr <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M17" display="inline" overflow="scroll" dspmath="mathml"><mo>/</mo></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="a3a809672b156f3719eee3cbaf593ee5"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="cp-20-25-2024-ie00007.svg" width="8pt" height="14pt" src="cp-20-25-2024-ie00007.png"/></svg:svg></span></span> <span class="inline-formula"><sup>86</sup></span>Sr change from variations in sedimentation rate. In this study, we produce the first <span class="inline-formula"><sup>87</sup></span>Sr <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M20" display="inline" overflow="scroll" dspmath="mathml"><mo>/</mo></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="78c74280a32911099c6aadbec3864e34"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="cp-20-25-2024-ie00008.svg" width="8pt" height="14pt" src="cp-20-25-2024-ie00008.png"/></svg:svg></span></span> <span class="inline-formula"><sup>86</sup></span>Sr results from an Oligocene to early Miocene site with a precise age-model-derived orbital tuning of high-resolution benthic <span class="inline-formula"><i>δ</i><sup>18</sup></span>O at Equatorial Pacific Ocean Drilling Program (ODP) Site 1218. Our new dataset resolves transient decreases in <span class="inline-formula"><sup>87</sup></span>Sr <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M24" display="inline" overflow="scroll" dspmath="mathml"><mo>/</mo></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="cdb097d754d0791f99b194a2a037445d"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="cp-20-25-2024-ie00009.svg" width="8pt" height="14pt" src="cp-20-25-2024-ie00009.png"/></svg:svg></span></span> <span class="inline-formula"><sup>86</sup></span>Sr, as well as periods of relative stasis. These changes can be directly compared with the high-resolution benthic <span class="inline-formula"><i>δ</i><sup>18</sup></span>O at the same site. We find that slowing of the rate of <span class="inline-formula"><sup>87</sup></span>Sr <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M28" display="inline" overflow="scroll" dspmath="mathml"><mo>/</mo></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="6e9042c80619a800f49fe8d9da77f107"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="cp-20-25-2024-ie00010.svg" width="8pt" height="14pt" src="cp-20-25-2024-ie00010.png"/></svg:svg></span></span> <span class="inline-formula"><sup>86</sup></span>Sr increase coincides with the onset of Antarctic ice expansion at the beginning of the mid-Oligocene glacial interval, and a rapid steeping in the <span class="inline-formula"><sup>87</sup></span>Sr <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M31" display="inline" overflow="scroll" dspmath="mathml"><mo>/</mo></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="cde794723cf5af95a282a8ea7937b694"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="cp-20-25-2024-ie00011.svg" width="8pt" height="14pt" src="cp-20-25-2024-ie00011.png"/></svg:svg></span></span> <span class="inline-formula"><sup>86</sup></span>Sr increase coincides with the benthic <span class="inline-formula"><i>δ</i><sup>18</sup></span>O evidence for rapid ice retreat. This pattern may reflect either northward shifts in the Intertropical Convergence Zone precipitation to areas of nonradiogenic bedrock and/or lowered weathering fluxes from highly radiogenic glacial flours on Antarctica. We additionally generate the first <span class="inline-formula"><sup>87</sup></span>Sr <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M35" display="inline" overflow="scroll" dspmath="mathml"><mo>/</mo></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="07d7a1dd05fd1823c5d4d7644fe5a26c"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="cp-20-25-2024-ie00012.svg" width="8pt" height="14pt" src="cp-20-25-2024-ie00012.png"/></svg:svg></span></span> <span class="inline-formula"><sup>86</sup></span>Sr data from ODP Site 1168 on the Tasman Rise and Integrated Ocean Drilling Program (IODP) Site 1406 of the Newfoundland Margin during the Oligocene to early Miocene to improve the precision of age correlation of these Northern Hemisphere and Southern Hemisphere midlatitude sites and to better estimate the duration of early Miocene hiatus and condensed sedimentation.</p> |
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| ISSN: | 1814-9324 1814-9332 |