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21 results on '"Yu Haitian"'

7. Yield Adaptability and Stability in Field Pea Genotypes Using AMMI, GGE, and GYT Biplot Analyses

Author

Yang, Xin, primary, Soliman, Alaa A., additional, Hu, Chaoqin, additional, Yang, Feng, additional, Lv, Meiyuan, additional, Yu, Haitian, additional, Wang, Yubao, additional, Zheng, Aiqing, additional, Dai, Zhengming, additional, Li, Qiong, additional, Tang, Yongsheng, additional, Yang, Jiangu, additional, Zhang, Yurong, additional, Niu, Wenwu, additional, Wang, Liping, additional, and He, Yuhua, additional

Published
2023
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11. Complete mitochondrial genome of the important phytopathogenic fungus Macrophomina phaseolina (Botryosphaeriales, Ascomycota)

Author

Yu Haitian, Wang Liping, He Yuhua, Yang Feng, and Lv Meiyuan

Subjects
Mitochondrial DNA, Ascomycota, biology, fungi, food and beverages, Fungus, biology.organism_classification, Botryosphaeriales, Crop production, Macrophomina phaseolina, mitochondrial genome, Botany, Genetics, phylogenetic analyses, Molecular Biology, Pathogen, Mitogenome Announcement, Research Article
Abstract

Macrophomina phaseolina is a Catastrophic plant pathogen, which can cause serious reduction in crop production. In the current study, the mitochondrial genome of M. phaseolina is assembled and annotated. The mitogenome of M. phaseolina is a circular molecule of 101,198 bp. The overall nucleotide content is 34.95% A, 35.25% T, 13.30% C, 16.50% G, with a CG content of 29.80%. The mitogenome contains 42 genes, including 14 protein coding genes (PCGs), 2 ribosomal RNA (rRNA) genes and 26 transfer RNA (tRNA) genes. Phylogenetic analyses based on concatenated protein sequences from 15 taxa of five orders in Ascomycota indicated that M. phaseolina is clustered in the order Botryosphaeriales. This study would have a positive impact on the molecular biology research and biological control of Macrophomina fungi in the future.

Published
2021

18. Response of provenance transition of Middle Jurassic–Early Cretaceous sediments to tectonic domain transformation in the North Yellow Sea Basin, Eastern North China Craton.

Author

Yu, Haitian, Xu, Zhongjie, Cheng, Rihui, Gao, Dan, and Zhang, Zhen

Subjects
*PROVENANCE (Geology), *SEDIMENTS, *FELSIC rocks, *IGNEOUS rocks, *OROGENIC belts, *MODAL analysis
Abstract

In the Late Mesozoic, the Eastern North China Craton changed from being controlled by the Palaeo‐Asian tectonic domain to the marginal Pacific tectonic domain. The Eastern North China Craton transformed the E–W compression to NNE–SSW extensional tectonics under the influence of two tectonic domain transformations. However, the timing of the transformation of the tectonic domains remains controversial. The North Yellow Sea Basin is located in an important position in the Eastern North China Craton at the junction of the Pacific and Eurasian plates and is controlled by two tectonic domains. Therefore, the sediments in the basin are faithful records of the transformation of the two tectonic domains. Based on the latest and high‐precision detrital zircon U–Pb dating data, sandstone modal analysis, and elemental geochemical analysis in the North Yellow Sea Basin combined with regional tectonic, palaeontological, and palaeoclimatic evidence, this paper discusses the provenance from the Middle Jurassic to Early Cretaceous, which responds to the Late Mesozoic tectonic domain transformation in the Eastern North China Craton, and provides important evidence of provenance in the North Yellow Sea Basin to determine the time of tectonic domain transformation. These results suggest that the source rocks of sediments in the North Yellow Sea Basin have changed from ancient sediments (ancient craton/recycle orogenic belt) in the Middle Jurassic to Late Jurassic, to felsic igneous rocks in the Early Cretaceous. The peak of zircon U–Pb ages changed from 234, 1,842, and 2,429 Ma in the Late Jurassic to 217 and 1,871 Ma in the Early Cretaceous. The provenance changed from the Sulu Orogenic Belt and Precambrian basement of the Jiaodong Peninsula in the Late Jurassic, to the igneous rocks and Precambrian basement of the Liaodong Peninsula and Korean Peninsula in the Early Cretaceous. The provenance direction of the sediments changed from south‐west in the Late Jurassic to the north and south‐east in the Early Cretaceous. The tectonic setting of the basin changed from compression to extension. The changes in the peaks of zircon U–Pb age, characteristics of the source rocks, provenance direction, and basin tectonic setting in the Middle Jurassic to Early Cretaceous in the North Yellow Sea Basin are a response to the change from E–W compression to NNE–SSW extensional tectonics caused by the transformation of two tectonic domains. In the Early Cretaceous, the Eastern North China Craton completed the transformation of two tectonic domains that were influenced and controlled by the marginal Pacific tectonic domain. [ABSTRACT FROM AUTHOR]

Published
2022
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