Bone surface modifications recorded.

Bone surface modifications recorded.

<p>Distribution of abrasion based on total (A) and NISP assemblage <b>(B)</b>. Distribution of weathered bones in the site K2 assemblage based on total assemblage.</p>

محفوظ في:

التفاصيل البيبلوغرافية
المؤلف الرئيسي:	Gábor Botfalvai (9426371) (author)
مؤلفون آخرون:	Zoltán Csiki-Sava (12058818) (author), János Magyar (13257123) (author), Barna Páll-Gergely (4961539) (author), Levente Koczó (22593484) (author), Daniel Ţabără (22593487) (author), Gergő Konecsni (22593490) (author), Soma Budai (22593493) (author)
منشور في:	2025
الموضوعات:	Evolutionary Biology Ecology Environmental Sciences not elsewhere classified Biological Sciences not elsewhere classified younger vertebrate assemblages related delta due recent extensive fieldwork multidominant mixed assemblage lacustrine depositional environment ha &# 355 good starting point 800 vertebrate fossils similar sites across scale faunal stability different depositional processes site k2 represents site k2 representing vertebrate paleontological investigations several important high div >< p changed significantly among 2 </ sup entire haţeg basin site k2 site among faunal composition different taxa maastrichtian sites haţeg island haţeg basin western romania transport energy thus provides sudden drop stratigraphical position remarkable large local fauna higher taxa former paleoenvironment excavated locations eg basin dominant elements dominance spectrum detailed sedimentological biostratigraphic comparisons approximately 4 already present
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مواد مشابهة

Skeletal completeness in the K2 assemblage: %TC – represents the percentage of total skeletal completeness; A – the actual number of skeletal elements recorded from site K2; E– the expected number of elements in a complete skeleton; %R – recovered element percentage of a certain skeletal element.
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Recovery rate of the different skeletal elements in the K2 assemblage.
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

NISP and MNI values as well as fragmentation rate associated with taxa in the K2 assemblage.
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Skeletal parts and taxon representation in the site K2 vertebrate assemblage.
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Results of the geochemical analyses (TOC, TS and n-alkanes) on sample 6B, site K2, Vălioara, Densuș-Ciula Formation.
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Stratigraphic position of site K2 (Neagului Valley, Vălioara – red star), Middle Member of the Densuș-Ciula Formation, relative to other important uppermost Cretaceous Transylvanian vertebrate sites (grey stars), including those mentioned/discussed specifically in the text (stars outlined in red), from the Hațeg (A – Sibișel Valley section, B – Râul Mare section, and C – Pui section) and southwestern Transylvanian basins (updated and modified from [3,20]); note that, as already acknowledged by [3], the relative positions of the sites within the different lithostratigraphic units is reliable, albeit not always precisely established,
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Reconstruction of the depositional processes producing the studied fossiliferous sedimentary sequence at site K2, Vălioara (Densuș–Ciula Formation).
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Fracture patterns of skeletal elements.
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Bone representation by size in the K2 assemblage.
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Relative abundances of the skeletal elements in the K2 vertebrate assemblage.
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Relative abundances of the vertebrate taxa in site K2, Vălioara (Densuș–Ciula Formation).
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Generalized skeletal reconstruction of the ‘K2 titanosaur’, Vălioara (Densuș–Ciula Formation).
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Generalized cranial and skeletal reconstruction of the ‘K2 rhabdodontid’, Vălioara (Densuș–Ciula Formation).
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Isolated crocodyliform teeth, site K2, Vălioara (Densuș–Ciula Formation).
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Isolated vertebrate remains, site K2, Vălioara (Densuș–Ciula Formation).
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Shells of terrestrial gastropods and freshwater bivalves from site K2, Vălioara (Densuș–Ciula Formation).
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Shells of the terrestrial and freshwater gastropods from site K2, Vălioara (Densuș–Ciula Formation).
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Gas chromatogram–mass spectrometry spectra from sample 6B, site K2, Vălioara (Densuş–Ciula Formation) (A), and diverse cross-plots: C, D. phytane/n-C18 versus pristane/n-C17 indicating the type of organic matter and depositional environment.
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Selected terrestrial palynomorphs, freshwater algae, and typical constituents of organic matter recognized at site K2, Vălioara (Densuș–Ciula Formation).
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Geological background and sedimentology of site K2.
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Site K2, Vălioara (Densuș-Ciula Formation).
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Geological maps.
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Geological and paleontological data for different uppermost Cretaceous vertebrate sites of Haţeg Island, discussed in the text.
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Character matrix of the taphonomic features recorded in the K2 vertebrate assemblage.
حسب: Gábor Botfalvai (9426371)
منشور في: (2025)

Statistics of the CATPCA presented in this study. The factor loadings are represented by the bulb of percussion (BP), flake termination (FT), sharp edges (SE), central crest/ridge (CC), platform preparation/trimming (PP), and ripples (R).
حسب: Dalila De Caro (21627189)
منشور في: (2025)

Statistics of the PCA presented in this study. The factor loadings are represented by length (L), width (W), thickness (T), platform depth (PD), platform width (PW).
حسب: Dalila De Caro (21627189)
منشور في: (2025)

Comparison of archaeological flakes and chips (≥10 mm) attributed to bipolar-on-anvil and freehand techniques.
حسب: Dalila De Caro (21627189)
منشور في: (2025)

Attribute Definitions and Scoring Criteria for Flake Analysis.
حسب: Dalila De Caro (21627189)
منشور في: (2025)

Marathousa 1, refits and conjoins.
حسب: Dalila De Caro (21627189)
منشور في: (2025)

CATPCA based on qualitative flake attributes.
حسب: Dalila De Caro (21627189)
منشور في: (2025)

PCA based on linear metric data.
حسب: Dalila De Caro (21627189)
منشور في: (2025)

Examples of radiolarite cores.
حسب: Dalila De Caro (21627189)
منشور في: (2025)

Cortical flakes and debris.
حسب: Dalila De Caro (21627189)
منشور في: (2025)

Expedient tools on debris and natural blanks.
حسب: Dalila De Caro (21627189)
منشور في: (2025)

Retouched tools.
حسب: Dalila De Caro (21627189)
منشور في: (2025)

Naturally backed knives and core edge elements (1-6).
حسب: Dalila De Caro (21627189)
منشور في: (2025)

Flakes in other raw materials.
حسب: Dalila De Caro (21627189)
منشور في: (2025)

Target flakes in radiolarite.
حسب: Dalila De Caro (21627189)
منشور في: (2025)

Scatter plot comparing the median values of exterior platform angle (EPA) and platform width (based on data published in [76]; see link to open access data below).
حسب: Dalila De Caro (21627189)
منشور في: (2025)

Boxplot showing the differences in length (mm), when comparing artefacts made on radiolarite to those made on other raw materials.
حسب: Dalila De Caro (21627189)
منشور في: (2025)