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527 results for “Mesozoic.”

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dryad28/100

Data from: Pelvis morphology suggests that early Mesozoic birds were too heavy to contact incubate their eggs

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publicMar 2018View details →
dryad28/100

Data from: The Muensterelloidea: phylogeny and character evolution of Mesozoic stem octopods

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publicJun 2019View details →
zenodo24/100

Dataset:Slab rollback versus delamination: contrasting fates of flat subduction and implications for South China evolution in Mesozoic

<p>This dataset contains simulation results used for visualizing Figures in&nbsp;<br> &ldquo;Slab rollback versus delamination: contrasting fates of flat subduction and implications for South China evolution in Mesozoic&rdquo;</p>

opencc-by-4.0Dec 2019View details →
zenodo24/100

An inclination-shallowing-corrected Early Triassic paleomagnetic pole for the North China Craton: Implication for the Mesozoic Geography of Proto-Asia

<p>This is a Supplementary Table for a manuscript submitted to JGR: Solid Earth entitled &quot;An inclination-shallowing-corrected Early Triassic paleomagnetic pole for the North China Craton: Implication for the Mesozoic Geography of Proto-Asia&quot;.</p>

opencc-by-4.0Jun 2020View details →
dryad24/100

Data from:Inferring flight parameters of Mesozoic avians through multivariate analyses of forelimb elements in their living relatives

Our knowledge of the diversity, ecology, and phylogeny of Mesozoic birds has increased significantly during recent decades, yet our understanding of their flight competence remains poor. Wing loading (WL) and aspect ratio (AR) are two aerodynamically relevant parameters, as they relate to energy costs of aerial locomotion and flight maneuverability. They can be calculated in living birds (i.e., Neornithes) from body mass (BM), wingspan (B) and lift surface (SL). However, the estimates for extinct birds can be subject to biases from statistical issues, phylogeny, locomotor adaptations, and diagenetic compaction. Here we develop a sequential approach for generating reliable multivariate models that allow estimating measurements necessary to determine WL and AR in the main clades of non-neornithine Mesozoic birds. The strength of our predictions is supported by the use of those variables that show similar scaling patterns in modern and stem taxa (i.e., non-neornithine birds), and the similarity of our predictions with measurements obtained from fossils preserving wing outlines. In addition, although our WL and AR values are based on estimates (BM, B, and SL) that have an associated error, there is no cumulative error in their calculation, and both parameters show low prediction errors. Therefore we present the first taxonomically broad, error-calibrated estimation of these two important aerodynamic parameters in non-neornithine birds. Such estimates show that the WL and AR of the non-neornithine birds here analyzed fall within the range of variation of modern birds (i.e., Neornithes). Our results indicate that most modern flight modes (e.g., continuous flapping, flap and gliding, flap and bounding, thermal soaring) were possible for the wide range of non-neornithine avian taxa; we found no evidence for the presence of dynamic soaring among these early birds.

opencc-zeroDec 2015View details →
dryad24/100

Data from: A new specimen of large-bodied basal enantiornithine Bohaiornis from the early Cretaceous of China and the inference of feeding ecology in Mesozoic birds

A new specimen of Bohaiornis guoi from the Jiufotang Formation, comprising a nearly complete skeleton, sheds light on enantiornithine morphological variation and ecological specialization. The new specimen was collected from near Lamadong Village in Liaoning Province, which is the same area where the sub-adult holotype specimen was reported. It provides new information on the cranial and pectoral girdle anatomy of the species, e.g., broad nasal, strikingly robust acromion, medially curved acrocoracoid process. In contrast to the holotype, the newly referred specimen has small rounded stones in the thoracic region that in other extinct taxa has been interpreted as direct evidence of diet. Direct evidence of diet is so far unknown in other Enantiornithes. Specifically the lack of "stomach stones" or gastroliths in enantiornithines despite their excellent fossil record has been proposed to be related to their insectivorous diet as well as to their arboreal ecology. We hypothesize that cranial morphology as well as the number and shape of the preserved stones in Bohaiornis may be most consistent with a raptorial ecology previously unknown for Enantiornithes and considered rare for Avialae. While rostrum shape has a strong relationship to feeding ecology in living birds, in basal avialan birds most diversity is in dental morphology, number, and distribution of the teeth.

opencc-zeroDec 2012View details →
zenodo24/100

Figs 18–22 in The longest-nosed Mesozoic Fulgoroidea (Homoptera): a new family from mid-Cretaceous Burmese amber

Figs 18–22. Dorytocus ornithorhynchus sp. n.: 18 – holotype instar V nymph, body,

opencc-by-4.0Feb 2018View details →
zenodo24/100

Figure 1 from: Zheng Y, Chen J, Wang X (2016) A new genus and species of Tettigarctidae from the Mesozoic of northeastern China (Insecta, Hemiptera, Cicadoidea). ZooKeys 632: 47-55. https://doi.org/10.3897/zookeys.632.10076

Figure 1 - Holotype of Maculaprosbole zhengi gen. et sp. n. A Photograph B Line drawing.

opencc-by-4.0Nov 2016View details →
zenodo24/100

FIG. 1 in Structure and genesis of the Taukha Mesozoic accretionary prism (southern Sikhote-Alin, Russia)

FIG. 1. — Regional tectonic map for the southeastern part of the southern Sikhote-Alin region.

opencc-zeroDec 2000View details →
dryad24/100

Data from: A new specimen of large-bodied basal enantiornithine Bohaiornis from the early Cretaceous of China and the inference of feeding ecology in Mesozoic birds

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publicOct 2013View details →
dryad24/100

Data from:Inferring flight parameters of Mesozoic avians through multivariate analyses of forelimb elements in their living relatives

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publicAug 2016View details →
zenodo20/100

FIGURE 6 in Review of Mesozoic Perissommatidae (Insecta: Diptera)

FIGURE 6. Collessomma mongolica gen. et sp. nov. (Bon-Tsagan, K1). A, B. Holotype PIN No. 3559/10039, total view and head. C. Paratype PIN No. 3559/4154, wing. Scale bars 500 μm (A, C), 200 μm (B).

opennotspecifiedJan 2020View details →
zenodo20/100

FIGURE 8. Mesozoic Perissommatinae. A, B in Review of Mesozoic Perissommatidae (Insecta: Diptera)

FIGURE 8. Mesozoic Perissommatinae. A, B. Head and total view of Palaeoperissomma collessi Kovalev in Kalugina &amp; Kovalev, 1985, PIN No. 1255/1341 (Kubekovo, J2). C, D. Head and total view of?Palaeoperissomma demetrii Kovalev, 1990, holotype PIN No. 1742/667 (Turga, K1). E, F. Head and total view of Gurvaniella hosbayari Kovalev, 1986, holotype PIN No. 3149/1789 (Gurvan, K1). Scale bars 200 μm (A, C, E), 1 mm (B, D, F). Abbreviations: e, eye; f, vein-like fold; o, ocelli.

opennotspecifiedJan 2020View details →
zenodo20/100

FIGURE 4. Collessomma gen. nov. A–C. C in Review of Mesozoic Perissommatidae (Insecta: Diptera)

FIGURE 4. Collessomma gen. nov. A–C. C. sibirica gen. et sp. nov. A, B. Male? PIN No. 5026/206, wing and tarsus. C. Holotype PIN No. 5340/1681, male terminalia. D, E. C. gnoma gen. et sp. nov. Holotype PIN No. 5026/201, wing and male terminalia. F, G. C. mongolica gen. et sp. nov. F. Paratype PIN No. 3559/4154, wing. G. Holotype PIN No. 3559/10039, female terminalia. Abbreviations: aed, aedeagus; cerc, cerci; gst, gonostylus; gx, gonocoxite; TG6–9, tergites 6–9; ST6-8, sternites 6–8. Scale bars 1 mm (A, F), 500 μm (D), 200 μm (C, E, G), 100 μm (B).

opennotspecifiedJan 2020View details →
zenodo20/100

FIGURE 5. C in Review of Mesozoic Perissommatidae (Insecta: Diptera)

FIGURE 5. C.gnoma gen. et sp. nov. A–C. Paratype PIN No. 5340/2982, male. A, B. Ventral and dorsal view of head (part and counterpart). C. Leg. D, E. Holotype PIN No. 5026/201, male, total view and terminalia. F–H. Paratype PIN No. 5340/2981, female. F. Antenna. G. Cerci. H. Total view. Scale bars 200 μm (A, B, C, E, F, G), 1 mm (D, H).

opennotspecifiedJan 2020View details →
zenodo20/100

Mesozoic–Cenozoic thermochronology of the Tarim–Southern Tianshan system, NW China: Implications for hydrocarbon accumulation

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opencc-by-4.0Apr 2020View details →
zenodo20/100

Figure 3 in Evidence from mitochondrial genomics supports the lower Mesozoic of South Asia as the time and place of basal divergence of cypriniform fishes (Actinopterygii: Ostariophysi)

Figure 3. Ancestral distribution ranges inferred by dispersal-vicariance analysis (DIVA) of 18 lineages at the subfamilial rank. Arrays of presence (1) or absence (0) state shown at each branch are in the order Africa, South Asia, East Asia, Europe, Siberia, western North America, and eastern North America (also see the inset). A number of arrays at some branches indicate equally optimal ancestral patterns. There were 1753 equally optimal combinations of these patterns given by DIVA.

opennotspecifiedFeb 2011View details →
zenodo20/100

Figure 4 in Evidence from mitochondrial genomics supports the lower Mesozoic of South Asia as the time and place of basal divergence of cypriniform fishes (Actinopterygii: Ostariophysi)

Figure 4. Ancestral distribution ranges reconstructed parsimoniously using PAUP*. Two representative character state (see legend for Fig. 3) optimizations are shown on the upper (delayed transition) and lower (accelerated transition) rows. Minimum F optimization was the same as delayed transition. The parsimonious reconstruction of character states allows an unrealistic all zero state. It does not give the character state at the root. In such cases the character state was manually optimized (asterisks).

opennotspecifiedFeb 2011View details →
zenodo20/100

Figure 5 in Wanted, tracked down and identified: Mesozoic non-biting midges of the subfamily Chironominae (Chironomidae, Diptera)

Figure 5. Palaeocentron krzeminskii, adult male, MP/4020 (ISEZ PAN); mid-Cretaceous, probably Albian–Cenomanian; Hukawng Valley, Kachin State, Myanmar. A, habitus. B, head and antenna (arrowheads indicate borders between flagellomeres fm 1–14).

opennotspecifiedJun 2021View details →
zenodo20/100

Fig. 12 in New fossil data and phylogenetic inferences shed light on the morphological disparity of Mesozoic Sinoalidae (Hemiptera, Cicadomorpha)

Fig. 12 Fifty percent majority-rule consensus tree of Sinoalidae inferred from Bayesian inference analysis based on 34 morphological characters, with representatives of fore- and hind wings illustrated. Numbers above the nodes indicate posterior probabilities. Numbers above branches

opennotspecifiedMar 2019View details →

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