FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2810497634> ?p ?o ?g. }

• W2810497634 endingPage "4585" @default.
• W2810497634 startingPage "4573" @default.
• W2810497634 abstract "Abstract Merging the late Quaternary Arctic paleoceanography into the Earth's global climate history remains challenging due to the lack of robust marine chronostratigraphies. Over ridges notably, low and variable sedimentation rates, scarce biogenic remains ensuing from low productivity and/or poor preservation, and oxygen isotope and paleomagnetic records differing from global stacks represent major impediments. However, as illustrate here based on consistent records from Mendeleev‐Alpha and Lomonosov Ridges, disequilibria between U‐series isotopes can provide benchmark ages. In such settings, fluxes of the particle‐reactive U‐daughter isotopes 230 Th and 231 Pa from the water column, are not unequivocally linked to sedimentation rates, but rather to sea‐ice rafting and brine production histories, thus to the development of sea‐ice factories over shelves during intervals of high relative sea level. The excesses in 230 Th and 231 Pa over fractions supported by their parent U‐isotopes, collapse down sedimentary sequences, due to radioactive decay, and provide radiometric benchmark ages of approximately 300 and 140 ka, respectively. These “extinction ages” point to mean sedimentation rates of ∼4.3 and ∼1.7 mm/ka, respectively, over the Lomonosov and Mendeleev Ridges, which are significantly lower than assumed in most recent studies, thus highlighting the need for revisiting current interpretations of Arctic lithostratigraphies in relation to the global‐scale late Quaternary climatostratigraphy." @default.
• W2810497634 created "2018-07-10" @default.
• W2810497634 creator A5000158357 @default.
• W2810497634 creator A5040113322 @default.
• W2810497634 creator A5041679091 @default.
• W2810497634 creator A5051754197 @default.
• W2810497634 creator A5058162134 @default.
• W2810497634 creator A5079412095 @default.
• W2810497634 creator A5085781532 @default.
• W2810497634 creator A5091217378 @default.
• W2810497634 date "2017-12-01" @default.
• W2810497634 modified "2023-10-16" @default.
• W2810497634 title "A New Chronology of Late Quaternary Sequences From the Central Arctic Ocean Based on “Extinction Ages” of Their Excesses in²³¹Pa and²³⁰Th" @default.
• W2810497634 cites W102194089 @default.
• W2810497634 cites W1531040956 @default.
• W2810497634 cites W1541103785 @default.
• W2810497634 cites W1768407171 @default.
• W2810497634 cites W1796896116 @default.
• W2810497634 cites W1869673716 @default.
• W2810497634 cites W1918626762 @default.
• W2810497634 cites W1953061174 @default.
• W2810497634 cites W1965583373 @default.
• W2810497634 cites W1966529962 @default.
• W2810497634 cites W1975160151 @default.
• W2810497634 cites W1976436689 @default.
• W2810497634 cites W1977737528 @default.
• W2810497634 cites W1980275011 @default.
• W2810497634 cites W1983113742 @default.
• W2810497634 cites W1999027888 @default.
• W2810497634 cites W2002474080 @default.
• W2810497634 cites W2002816415 @default.
• W2810497634 cites W2005463144 @default.
• W2810497634 cites W2013270839 @default.
• W2810497634 cites W2018716537 @default.
• W2810497634 cites W2021844300 @default.
• W2810497634 cites W2025460335 @default.
• W2810497634 cites W2025546593 @default.
• W2810497634 cites W2027491183 @default.
• W2810497634 cites W2027649198 @default.
• W2810497634 cites W2030422110 @default.
• W2810497634 cites W2033165365 @default.
• W2810497634 cites W2035061771 @default.
• W2810497634 cites W2045702994 @default.
• W2810497634 cites W2047823789 @default.
• W2810497634 cites W2048405463 @default.
• W2810497634 cites W2049328342 @default.
• W2810497634 cites W2049953938 @default.
• W2810497634 cites W2060425250 @default.
• W2810497634 cites W2062769133 @default.
• W2810497634 cites W2065126231 @default.
• W2810497634 cites W2065282358 @default.
• W2810497634 cites W2068625916 @default.
• W2810497634 cites W2074096601 @default.
• W2810497634 cites W2076402709 @default.
• W2810497634 cites W2077267127 @default.
• W2810497634 cites W2086811338 @default.
• W2810497634 cites W2089454180 @default.
• W2810497634 cites W2090099239 @default.
• W2810497634 cites W2112625494 @default.
• W2810497634 cites W2117882799 @default.
• W2810497634 cites W2118146220 @default.
• W2810497634 cites W2121759554 @default.
• W2810497634 cites W2125047091 @default.
• W2810497634 cites W2127702288 @default.
• W2810497634 cites W2135039044 @default.
• W2810497634 cites W2138023539 @default.
• W2810497634 cites W2149075049 @default.
• W2810497634 cites W2157681159 @default.
• W2810497634 cites W2161107240 @default.
• W2810497634 cites W2163219804 @default.
• W2810497634 cites W2166222352 @default.
• W2810497634 cites W2168439910 @default.
• W2810497634 cites W2169053053 @default.
• W2810497634 cites W2172120032 @default.
• W2810497634 cites W2224436824 @default.
• W2810497634 cites W2402815629 @default.
• W2810497634 cites W2562473239 @default.
• W2810497634 cites W37457635 @default.
• W2810497634 cites W4205665943 @default.
• W2810497634 cites W4246027503 @default.
• W2810497634 doi "https://doi.org/10.1002/2017gc007050" @default.
• W2810497634 hasPublicationYear "2017" @default.
• W2810497634 type Work @default.
• W2810497634 sameAs 2810497634 @default.
• W2810497634 citedByCount "25" @default.
• W2810497634 countsByYear W28104976342018 @default.
• W2810497634 countsByYear W28104976342019 @default.
• W2810497634 countsByYear W28104976342020 @default.
• W2810497634 countsByYear W28104976342021 @default.
• W2810497634 countsByYear W28104976342022 @default.
• W2810497634 countsByYear W28104976342023 @default.
• W2810497634 crossrefType "journal-article" @default.
• W2810497634 hasAuthorship W2810497634A5000158357 @default.
• W2810497634 hasAuthorship W2810497634A5040113322 @default.
• W2810497634 hasAuthorship W2810497634A5041679091 @default.
• W2810497634 hasAuthorship W2810497634A5051754197 @default.
• W2810497634 hasAuthorship W2810497634A5058162134 @default.
• W2810497634 hasAuthorship W2810497634A5079412095 @default.

• next