• journal_title：PALAIOS
• Contributor：KATARZYNA FRANKOWIAK ; MACIEJ MAZUR ; ANNE M. GOTHMANN ; JAROSŁAW STOLARSKI
• Publisher：SEPM Society for Sedimentary Geology
• Date：2013-06-01
• Format：text/html
• Language：en
• Identifier：10.2110/palo.2012.p12-116r
• journal_abbrev：PALAIOS
• issn：0883-1351
• volume：28
• issue：6
• firstpage：333
• section：RESEARCH ARTICLES

Skeletons of Norian corals from the aragonite Konservat-Lagerstätte in Alakir Çay, Turkey are commonly considered to be exceptionally preserved. However, one example of Pachysolenia cylindrica shows that although aragonite is the dominant mineral phase (about 86.2%), the distribution of microscale diagenetic features in the skeleton complicate its usage as a paleoenvironmental archive. We used a density separation technique to isolate aragonite-enriched powders of skeletal material, which compared to powders of bulk skeleton (∼8.3% more calcite than aragonite-enriched powders), exhibit higher Sr/Ca (by an average of 0.27 mmol/mol), lower Mg/Ca (by an average of 1.34 mmol/mol), and lower δ¹⁸O (by an average of 0.28‰). In addition, paleo-sea surface temperatures calculated using values from bulk measurements are 1.1–3.4 °C colder (3.3–3.4 °C for Sr/Ca and 1.1–2.0 °C for δ¹⁸O) than temperatures calculated from the density-separated, aragonite-enriched powders. These data suggest that the presence of about 13.8% of secondary calcite can influence the robustness of geochemical proxies and that density separation is an effective tool for recovering the original geochemical signal from diagenetically altered samples.