The latest spreading periods of the south china sea: new constraints from macrostructure analysis of IODP expedition 349 cores and geophysical data

Author Posting. © American Geophysical Union, 2019. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research-Solid Earth 124 (2019): 9980– 9998, doi:10.1029/2019JB017584.Macrostructures preserved in deformed rocks are essential for the understanding of their evolution, especially when the deformation is weak and hard to discriminate in regional scale or purely through geophysical data. In order to resolve the inconsistency between NS trending fracture zones and NE oriented spreading fabrics of the South China Sea during the latest spreading stage, we analyzed macrostructures identifiable from the basalt and consolidated sediment samples of the Integrated Ocean Drilling Program (IODP) Sites U1431 and U1433. These two sites are close to the East and Southwest relict spreading ridges and provide critical information on the latest spreading stages. The structures in the basalt of both sites suggest two dominant orientations of NS and NE. At U1431, sediments show mainly WNW trending slickensides, different from that of basalt. At U1433, no structures were found in postspreading sediment. Thus, NE and NS trending structures in basalt are most possibly formed by seafloor spreading. Crosscutting relationship suggests that NE trending structures formed first, followed by NS and finally WNW trending structures. These observations are consistent with geophysical features. Magnetic anomalies and ocean bottom seismometer velocity suggest that the latest relict ridge of the East Subbasin coincides with the EW trending seamount chain. Located between the relict ridges of East and Southwest Subbasins, NS trending Zhongnan‐Liyue Fracture Zone had acted as the latest transform fault. Based on the above evidences, we proposed that the South China Sea may have experienced a short period of NS oriented spreading after earlier SE spreading. These results resolve the previous inconsistencies.We appreciate Anne Replumaz and other anonymous reviewers for the constructive suggestions, which improve this paper to a great extent. This research was supported by Guangdong NSF research team project (2017A030312002), K. C. Wong Education Foundation (GJTD‐2018‐13), the IODP‐China Foundation, the NSFC Projects (91628301, 41376027, 41576070, 41576068, 41430962, 41674069, 91528302, and 20153410), U.S. National Science Foundation through Grant EAR‐1250444, the Guangdong Province Foundation (41576068), and the Joint Foundation of the Natural Science Foundation of China (NSFC) and Guangdong Province (U1301233). Fucheng Li is thanked for helping with the earthquake epicenter figure for the study area. All the sample photos can be accessed via web address (http://www.iodp.tamu.edu). The archive halves of samples are kept in the Kochi repository. The paleomag data will be published by Xixi Zhao separately. All the other geophysical data have been published; for example, the multichannel seismic could be referenced to Li et al. (2015a), and the gravity data and magnetic anomaly data are from Sandwell et al. (2014) and Ishihara and Kisimoto (1996).2020-02-2

1,1′-Bis(diisobutyl­phosphino)cobalto­cenium hexa­fluorido­phosphate

In the title compound, [Co(C13H22P)2]PF6, the CoIII atom is sandwiched between two (diisobutyl­phosphino)cyclo­penta­dienenyl ligands. The two diisobutyl­phophine units are trans to each other with respect to the CoIII metal center. The PF6 − anion links the cobaltocenium cations via weak C—H⋯F hydrogen bonds into a chain running along the b axis. The chains are further linked by C—H⋯F hydrogen bonds, forming a layer extending parallel to the (10) plane

Tris(1H-imidazole-κN 3)(7-oxabicyclo­[2.2.1]heptane-2,3-dicarboxyl­ato-κ3 O 2,O 3,O 7)cobalt(II) 3.35-hydrate

In the crystal structure of the title compound, [Co(C8H8O5)(C3H4N2)3]·3.35H2O, the central CoII ion is in a slightly distorted octa­hedral environment, coordinated by the bridg­ing O atom from the bicyclo­[2.2.1]heptane ligand, by two carboxyl­ate O atoms from two different carboxyl­ate groups and by three N atoms from imidazole ligands. Uncoordinated water mol­ecules, some of them disordered, are present in the crystal structure. In the crystal structure, mol­ecules are linked by O—H⋯O, N—H⋯O and O—H⋯N hydrogen-bonding inter­actions

Identify submitochondria and subchloroplast locations with pseudo amino acid composition: Approach from the strategy of discrete wavelet transform feature extraction

AbstractIt is very challenging and complicated to predict protein locations at the sub-subcellular level. The key to enhancing the prediction quality for protein sub-subcellular locations is to grasp the core features of a protein that can discriminate among proteins with different subcompartment locations. In this study, a different formulation of pseudoamino acid composition by the approach of discrete wavelet transform feature extraction was developed to predict submitochondria and subchloroplast locations. As a result of jackknife cross-validation, with our method, it can efficiently distinguish mitochondrial proteins from chloroplast proteins with total accuracy of 98.8% and obtained a promising total accuracy of 93.38% for predicting submitochondria locations. Especially the predictive accuracy for mitochondrial outer membrane and chloroplast thylakoid lumen were 82.93% and 82.22%, respectively, showing an improvement of 4.88% and 27.22% when other existing methods were compared. The results indicated that the proposed method might be employed as a useful assistant technique for identifying sub-subcellular locations. We have implemented our algorithm as an online service called SubIdent (http://bioinfo.ncu.edu.cn/services.aspx)