FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4385311384> ?p ?o ?g. }

• W4385311384 endingPage "111751" @default.
• W4385311384 startingPage "111751" @default.
• W4385311384 abstract "The Late Devonian Kellwasser Events are two major biodiversity crises recorded at and just below the Frasnian-Famennian stage boundary for which the ultimate cause or causes of diversity depletion remain unclear. The discovery of anomalous mercury (Hg) enrichments in Upper Kellwasser Event (UKE) strata has led to increased interest in a potential volcanic trigger for one or both events. However, UKE Hg anomalies are found mainly on the continental shelves of the Paleotethys Ocean, and Hg isotope values from at least one distal basin indicate a non-volcanic Hg source. These findings suggest volcanism during the UKE may have had regional rather than global impacts. In comparison to the UKE, few works have investigated the sedimentary Hg record of the Lower Kellwasser Event (LKE). Here, we contribute new Hg data from the LKE of the Appalachian Basin and compare this to a compilation of global Hg data from both events. The Appalachian Basin contains no sedimentary Hg enrichments consistent with massive volcanism during the LKE, and Hg concentrations are strongly correlated with total organic carbon. We argue that organic matter drawdown exerted a primary control upon Hg concentration in the Appalachian Basin. While basins more proximal to the Paleotethys Ocean preserve potentially volcanogenic LKE Hg anomalies, the absence of such anomalies here reflects volcanism during the LKE that was at most only regionally significant, as hypothesized for the UKE. Volcanism is therefore an unlikely trigger of the global Kellwasser diversity depletions. Broader sampling of the Kellwasser record will assist in the development of an extinction model that accounts for variations in global Hg concentrations, as the depressed origination rates, prolonged background environmental stress, and variations in intra-basinal expression that characterize both events may indicate that the trigger of diversity loss in this interval is unique among the “Big Five” mass extinctions." @default.
• W4385311384 created "2023-07-28" @default.
• W4385311384 creator A5000745389 @default.
• W4385311384 creator A5004811514 @default.
• W4385311384 creator A5011277833 @default.
• W4385311384 creator A5021497988 @default.
• W4385311384 date "2023-10-01" @default.
• W4385311384 modified "2023-09-26" @default.
• W4385311384 title "Appalachian Basin mercury enrichments during the Late Devonian Kellwasser Events and comparison to global records" @default.
• W4385311384 cites W1501195950 @default.
• W4385311384 cites W1581571809 @default.
• W4385311384 cites W1582303660 @default.
• W4385311384 cites W1770113505 @default.
• W4385311384 cites W1976721572 @default.
• W4385311384 cites W1986516591 @default.
• W4385311384 cites W1992369998 @default.
• W4385311384 cites W1997469183 @default.
• W4385311384 cites W1998963014 @default.
• W4385311384 cites W2005004394 @default.
• W4385311384 cites W2006478853 @default.
• W4385311384 cites W2009076574 @default.
• W4385311384 cites W2011611047 @default.
• W4385311384 cites W2015486378 @default.
• W4385311384 cites W2019839279 @default.
• W4385311384 cites W2024624559 @default.
• W4385311384 cites W2030150536 @default.
• W4385311384 cites W2052902538 @default.
• W4385311384 cites W2053080100 @default.
• W4385311384 cites W2056204989 @default.
• W4385311384 cites W2059075068 @default.
• W4385311384 cites W2077116437 @default.
• W4385311384 cites W2079852953 @default.
• W4385311384 cites W2083546661 @default.
• W4385311384 cites W2084341057 @default.
• W4385311384 cites W2086667596 @default.
• W4385311384 cites W2096478882 @default.
• W4385311384 cites W2109379209 @default.
• W4385311384 cites W2109920192 @default.
• W4385311384 cites W2118691770 @default.
• W4385311384 cites W2118709509 @default.
• W4385311384 cites W2123767734 @default.
• W4385311384 cites W2128652714 @default.
• W4385311384 cites W2128870723 @default.
• W4385311384 cites W2150209488 @default.
• W4385311384 cites W2154305513 @default.
• W4385311384 cites W2154984426 @default.
• W4385311384 cites W2162402178 @default.
• W4385311384 cites W2165736936 @default.
• W4385311384 cites W2206804843 @default.
• W4385311384 cites W2224212289 @default.
• W4385311384 cites W2295656484 @default.
• W4385311384 cites W2312960404 @default.
• W4385311384 cites W2316952183 @default.
• W4385311384 cites W2477272335 @default.
• W4385311384 cites W2550194864 @default.
• W4385311384 cites W2560595811 @default.
• W4385311384 cites W2567656277 @default.
• W4385311384 cites W2593173378 @default.
• W4385311384 cites W2594503416 @default.
• W4385311384 cites W2743442732 @default.
• W4385311384 cites W2765950902 @default.
• W4385311384 cites W2769305873 @default.
• W4385311384 cites W2779472444 @default.
• W4385311384 cites W2794301357 @default.
• W4385311384 cites W2801345300 @default.
• W4385311384 cites W2804398341 @default.
• W4385311384 cites W2885063737 @default.
• W4385311384 cites W2892551230 @default.
• W4385311384 cites W2893607070 @default.
• W4385311384 cites W2896903886 @default.
• W4385311384 cites W2905112325 @default.
• W4385311384 cites W2911755519 @default.
• W4385311384 cites W2913368254 @default.
• W4385311384 cites W2924150740 @default.
• W4385311384 cites W2929626496 @default.
• W4385311384 cites W2944752667 @default.
• W4385311384 cites W2947224750 @default.
• W4385311384 cites W2994764300 @default.
• W4385311384 cites W2995518230 @default.
• W4385311384 cites W2997493598 @default.
• W4385311384 cites W3004969637 @default.
• W4385311384 cites W3009641280 @default.
• W4385311384 cites W3011326703 @default.
• W4385311384 cites W3026130405 @default.
• W4385311384 cites W3095662282 @default.
• W4385311384 cites W3111957921 @default.
• W4385311384 cites W3131973622 @default.
• W4385311384 cites W3135337128 @default.
• W4385311384 cites W4213134767 @default.
• W4385311384 cites W4220811251 @default.
• W4385311384 cites W424978307 @default.
• W4385311384 cites W4295308633 @default.
• W4385311384 cites W4367042815 @default.
• W4385311384 doi "https://doi.org/10.1016/j.palaeo.2023.111751" @default.
• W4385311384 hasPublicationYear "2023" @default.
• W4385311384 type Work @default.
• W4385311384 citedByCount "0" @default.
• W4385311384 crossrefType "journal-article" @default.

• next