FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1991144030> ?p ?o ?g. }

• W1991144030 endingPage "205" @default.
• W1991144030 startingPage "194" @default.
• W1991144030 abstract "Multiple dinosaur tracksites are known from the red beds (sandstones and siltstones) of the Hekou Group in the Lanzhou-Minhe Basin in Gansu Province, China. Among these, the most famous is the Yanguoxia No. 1 & 2 tracksite, which has an abundance of tracks from a diverse ichnofauna. Here, we describe natural casts from six new tracksites including three located near the Yanguoxia No. 1 & 2 tracksites and three from more distant tracksites (located up to 40 km from Yanguoxia). The new tracksites have all yielded isolated, large dinosaur track casts, two of which are tridactyl tracks of ornithopod and/or theropod affinity, while another eight casts are pes and manus tracks of medium-to large-sized sauropods. The predominance of sauropod track casts may reflect the fact that, by simple virtue of their large size, sauropods tracks resist weathering and are easy to find. Notably, the sauropod track casts are deep natural tracks left in soft and moist substrates with a relatively high cohesiveness. They offer a glimpse into the three-dimensional foot morphology of the sauropod trackmakers and their foot movement (locomotion), and thus are an important complement to the tracks preserved as (shallow) impressions and the trackways of the Yanguoxia No. 1 & 2 tracksite. The new tracksites suggest a lower ecological diversity than would be inferred from the Yanguoxia No. 1 & 2 tracksite. However, it is assumed that this apparent low diversity is an artifact resulting from the small sample area and the fact that all the outcrops are cross-sections where bedding planes – that could reveal small tracks and more abundant tracks and trackways – are scarce and limited to small surfaces. These new sites suggest that the distribution and frequency of dinosaur tracks within the Lanzhou-Minhe Basin is much wider than previously assumed and that many more dinosaur tracksites are likely to be discovered within the basin in the future." @default.
• W1991144030 created "2016-06-24" @default.
• W1991144030 creator A5007417772 @default.
• W1991144030 creator A5017991749 @default.
• W1991144030 creator A5032706216 @default.
• W1991144030 creator A5040432736 @default.
• W1991144030 creator A5059015378 @default.
• W1991144030 creator A5063816185 @default.
• W1991144030 creator A5069271704 @default.
• W1991144030 creator A5076374858 @default.
• W1991144030 creator A5090834341 @default.
• W1991144030 date "2015-01-01" @default.
• W1991144030 modified "2023-09-30" @default.
• W1991144030 title "Dinosaur natural track casts from the Lower Cretaceous Hekou Group in the Lanzhou-Minhe Basin, Gansu, Northwest China: Ichnology, track formation, and distribution" @default.
• W1991144030 cites W1585179859 @default.
• W1991144030 cites W1880620305 @default.
• W1991144030 cites W1966518809 @default.
• W1991144030 cites W1968591108 @default.
• W1991144030 cites W1970598126 @default.
• W1991144030 cites W1976093627 @default.
• W1991144030 cites W1982568697 @default.
• W1991144030 cites W2004554861 @default.
• W1991144030 cites W2011010913 @default.
• W1991144030 cites W2014197839 @default.
• W1991144030 cites W2030068229 @default.
• W1991144030 cites W2030598013 @default.
• W1991144030 cites W2039592722 @default.
• W1991144030 cites W2053597338 @default.
• W1991144030 cites W2065845231 @default.
• W1991144030 cites W2077322127 @default.
• W1991144030 cites W2078270382 @default.
• W1991144030 cites W2089282094 @default.
• W1991144030 cites W2103008101 @default.
• W1991144030 cites W2109570175 @default.
• W1991144030 cites W2141285642 @default.
• W1991144030 cites W2152301519 @default.
• W1991144030 cites W2157461079 @default.
• W1991144030 cites W2165573263 @default.
• W1991144030 cites W2176003244 @default.
• W1991144030 cites W2179599488 @default.
• W1991144030 cites W3120422152 @default.
• W1991144030 doi "https://doi.org/10.1016/j.cretres.2014.10.001" @default.
• W1991144030 hasPublicationYear "2015" @default.
• W1991144030 type Work @default.
• W1991144030 sameAs 1991144030 @default.
• W1991144030 citedByCount "28" @default.
• W1991144030 countsByYear W19911440302015 @default.
• W1991144030 countsByYear W19911440302016 @default.
• W1991144030 countsByYear W19911440302017 @default.
• W1991144030 countsByYear W19911440302018 @default.
• W1991144030 countsByYear W19911440302019 @default.
• W1991144030 countsByYear W19911440302020 @default.
• W1991144030 countsByYear W19911440302021 @default.
• W1991144030 countsByYear W19911440302022 @default.
• W1991144030 crossrefType "journal-article" @default.
• W1991144030 hasAuthorship W1991144030A5007417772 @default.
• W1991144030 hasAuthorship W1991144030A5017991749 @default.
• W1991144030 hasAuthorship W1991144030A5032706216 @default.
• W1991144030 hasAuthorship W1991144030A5040432736 @default.
• W1991144030 hasAuthorship W1991144030A5059015378 @default.
• W1991144030 hasAuthorship W1991144030A5063816185 @default.
• W1991144030 hasAuthorship W1991144030A5069271704 @default.
• W1991144030 hasAuthorship W1991144030A5076374858 @default.
• W1991144030 hasAuthorship W1991144030A5090834341 @default.
• W1991144030 hasConcept C109007969 @default.
• W1991144030 hasConcept C12294951 @default.
• W1991144030 hasConcept C127313418 @default.
• W1991144030 hasConcept C138170599 @default.
• W1991144030 hasConcept C151730666 @default.
• W1991144030 hasConcept C160937034 @default.
• W1991144030 hasConcept C169212394 @default.
• W1991144030 hasConcept C178790620 @default.
• W1991144030 hasConcept C185592680 @default.
• W1991144030 hasConcept C186847809 @default.
• W1991144030 hasConcept C2776608160 @default.
• W1991144030 hasConcept C2777014788 @default.
• W1991144030 hasConcept C2781311116 @default.
• W1991144030 hasConcept C41440632 @default.
• W1991144030 hasConcept C42498943 @default.
• W1991144030 hasConceptScore W1991144030C109007969 @default.
• W1991144030 hasConceptScore W1991144030C12294951 @default.
• W1991144030 hasConceptScore W1991144030C127313418 @default.
• W1991144030 hasConceptScore W1991144030C138170599 @default.
• W1991144030 hasConceptScore W1991144030C151730666 @default.
• W1991144030 hasConceptScore W1991144030C160937034 @default.
• W1991144030 hasConceptScore W1991144030C169212394 @default.
• W1991144030 hasConceptScore W1991144030C178790620 @default.
• W1991144030 hasConceptScore W1991144030C185592680 @default.
• W1991144030 hasConceptScore W1991144030C186847809 @default.
• W1991144030 hasConceptScore W1991144030C2776608160 @default.
• W1991144030 hasConceptScore W1991144030C2777014788 @default.
• W1991144030 hasConceptScore W1991144030C2781311116 @default.
• W1991144030 hasConceptScore W1991144030C41440632 @default.
• W1991144030 hasConceptScore W1991144030C42498943 @default.
• W1991144030 hasLocation W19911440301 @default.
• W1991144030 hasOpenAccess W1991144030 @default.
• W1991144030 hasPrimaryLocation W19911440301 @default.
• W1991144030 hasRelatedWork W1916724119 @default.

• next