FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2887179914> ?p ?o ?g. }

• W2887179914 endingPage "19" @default.
• W2887179914 startingPage "1" @default.
• W2887179914 abstract "We study the sedimentology, palaeontology and palaeomagnetism of the 500 m thick sedimentary sequence in the Gorna Sushitsa gorge in the Sandanski Basin (southwest Bulgaria), which is exceptionally rich in fossil mammals of Pikermian type. Magnetostratigraphy indicates that this section was deposited within 2 myrs, between 8.5 Ma and 6.5 Ma (late Tortonian to early Messinian). Our investigations reveal that the Sandanski Basin infill represents two stacking synrift phases (Delcevo and Kalimantsi formations), with an intervening tectonic quiescence package (Sandanski Formation). Kalimantsi Formation deposition ends with the cessation of slip on basin-bounding faults at 6.9 Ma, probably caused by a switch from regional E-W to NS extension between 7 and 6.5 Ma. High slip rates compared to hanging wall sedimentation rates induced the development of mega-breccia dominated substantial fault scarps during the younger synrift phase (8.2 to 6.9 Ma). Tectonic changes are superimposed by several climatic changes. Moderately humid conditions prevail from 8.5–8.2 Ma, followed by relatively dry period from 8.2 to 7.8 Ma. A second humid interval from 7.74–7.56 Ma, which may be responsible for the Maeotian transgression in the Eastern Paratethys lake, is followed by a significant trend in local and supra-regional aridization, indicated by the onset of orbital driven aeolian dust deposition at 7.42 Ma. Our new data expand the Northern Mediterranean Sahara-born dust record at the Tortonian-Messinian transition to at least 600 kyrs (7.42 to 6.85–6.8 Ma). Coeval with the onset of dust deposition we observed evolutionary changes in the large mammal record, leading to the classical Pikermian association dated to between 7.42 and 7.27 Ma. We interpret faunal changes at the Tortonian-Messinian transition in the Eastern Mediterranean as driven by global cooling and mid-latitudinal desertification." @default.
• W2887179914 created "2018-08-22" @default.
• W2887179914 creator A5005587883 @default.
• W2887179914 creator A5007690646 @default.
• W2887179914 creator A5042645740 @default.
• W2887179914 creator A5067000979 @default.
• W2887179914 creator A5069436287 @default.
• W2887179914 date "2018-11-01" @default.
• W2887179914 modified "2023-10-18" @default.
• W2887179914 title "Late Miocene stratigraphy, palaeoclimate and evolution of the Sandanski Basin (Bulgaria) and the chronology of the Pikermian faunal changes" @default.
• W2887179914 cites W1593718805 @default.
• W2887179914 cites W1972303070 @default.
• W2887179914 cites W1975827797 @default.
• W2887179914 cites W1979536803 @default.
• W2887179914 cites W1989793143 @default.
• W2887179914 cites W1999138593 @default.
• W2887179914 cites W1999956578 @default.
• W2887179914 cites W2003352687 @default.
• W2887179914 cites W2003488081 @default.
• W2887179914 cites W2009301766 @default.
• W2887179914 cites W2017853264 @default.
• W2887179914 cites W2023137424 @default.
• W2887179914 cites W2028082051 @default.
• W2887179914 cites W2034649511 @default.
• W2887179914 cites W2036840075 @default.
• W2887179914 cites W2042800623 @default.
• W2887179914 cites W2043918289 @default.
• W2887179914 cites W2050049637 @default.
• W2887179914 cites W2057138816 @default.
• W2887179914 cites W2057874266 @default.
• W2887179914 cites W2064279268 @default.
• W2887179914 cites W2067084800 @default.
• W2887179914 cites W2070203063 @default.
• W2887179914 cites W2073224371 @default.
• W2887179914 cites W2092050977 @default.
• W2887179914 cites W2093080240 @default.
• W2887179914 cites W2104584561 @default.
• W2887179914 cites W2118336265 @default.
• W2887179914 cites W2124119288 @default.
• W2887179914 cites W2128670040 @default.
• W2887179914 cites W2129806013 @default.
• W2887179914 cites W2133732249 @default.
• W2887179914 cites W2140477756 @default.
• W2887179914 cites W2156901294 @default.
• W2887179914 cites W2169309664 @default.
• W2887179914 cites W2169575345 @default.
• W2887179914 cites W2176167820 @default.
• W2887179914 cites W2184943590 @default.
• W2887179914 cites W2405865015 @default.
• W2887179914 cites W2472477839 @default.
• W2887179914 cites W2511575715 @default.
• W2887179914 cites W2526517389 @default.
• W2887179914 cites W2549555987 @default.
• W2887179914 cites W2605792333 @default.
• W2887179914 cites W2617454850 @default.
• W2887179914 cites W2620485859 @default.
• W2887179914 cites W2746454103 @default.
• W2887179914 cites W3083730058 @default.
• W2887179914 cites W4232507027 @default.
• W2887179914 cites W4306293736 @default.
• W2887179914 cites W4316082669 @default.
• W2887179914 cites W4320473669 @default.
• W2887179914 doi "https://doi.org/10.1016/j.gloplacha.2018.07.019" @default.
• W2887179914 hasPublicationYear "2018" @default.
• W2887179914 type Work @default.
• W2887179914 sameAs 2887179914 @default.
• W2887179914 citedByCount "14" @default.
• W2887179914 countsByYear W28871799142019 @default.
• W2887179914 countsByYear W28871799142020 @default.
• W2887179914 countsByYear W28871799142021 @default.
• W2887179914 countsByYear W28871799142022 @default.
• W2887179914 countsByYear W28871799142023 @default.
• W2887179914 crossrefType "journal-article" @default.
• W2887179914 hasAuthorship W2887179914A5005587883 @default.
• W2887179914 hasAuthorship W2887179914A5007690646 @default.
• W2887179914 hasAuthorship W2887179914A5042645740 @default.
• W2887179914 hasAuthorship W2887179914A5067000979 @default.
• W2887179914 hasAuthorship W2887179914A5069436287 @default.
• W2887179914 hasConcept C109007969 @default.
• W2887179914 hasConcept C121332964 @default.
• W2887179914 hasConcept C127313418 @default.
• W2887179914 hasConcept C151730666 @default.
• W2887179914 hasConcept C181536285 @default.
• W2887179914 hasConcept C189479680 @default.
• W2887179914 hasConcept C193748577 @default.
• W2887179914 hasConcept C204330871 @default.
• W2887179914 hasConcept C24890656 @default.
• W2887179914 hasConcept C2779421809 @default.
• W2887179914 hasConcept C2781291010 @default.
• W2887179914 hasConcept C49015763 @default.
• W2887179914 hasConcept C6494504 @default.
• W2887179914 hasConcept C67422804 @default.
• W2887179914 hasConcept C77271252 @default.
• W2887179914 hasConceptScore W2887179914C109007969 @default.
• W2887179914 hasConceptScore W2887179914C121332964 @default.
• W2887179914 hasConceptScore W2887179914C127313418 @default.
• W2887179914 hasConceptScore W2887179914C151730666 @default.
• W2887179914 hasConceptScore W2887179914C181536285 @default.

• next