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621.
Controversies over the origin of globally distributed Cretaceous red beds have mainly focused on climate vs. weathering with potential hydrothermal influence. In comparison to Cretaceous Oceanic Red Beds, Cretaceous lacustrine red beds exhibit chronological inconsistencies and their diverse tectonic settings suggest differing genetic mechanisms. In this paper, Early Cretaceous red beds in the North Yellow Sea Basin, one of Mesozoic rift basins in eastern China that are associated with multi-phase magmatic activities, was chosen to document potential hydrothermal impact. Geological and geochemical analyses show that these red beds were syndepositional products developed in shallow to moderately deep lacustrine environments and that they were influenced by hydrothermal activity. Major and trace elements, including enhanced Al2O3-normalized Fe2O3 and Fe2O3 (total) values, Al/(Al + Fe + Mn) and (Fe + Mn)/Ti ratios, Ni-Co-Zn and Fe-Mn-(Ni + Co + Cu)*10, ∑REE-La/Yb, the concentrations of hydrothermally-related ions, invalid redox indicators of trace elements, abnormally high Fe2O3 (total) content, positive Eu anomaly, correlation of Fe2O3 (total) and Eu anomaly, and vitrinite reflectance (Ro) vs. total organic carbon (TOC), all show strong hydrothermal fluid influence and heating effects. By integrating and comparing data from previous studies, we propose a hydrothermally affected sedimentation model for Cretaceous red beds and associated sediments in magma-activated lacustrine basins, and conclude that the enriched metallic ions introduced by the hydrothermal fluids may be the most significant reason for the deposition of the red beds, and the flushed ferric ions, accompanied by hydrothermal fluid, are the main ions that are hosted inside hematite causing the red sediment. This model can be applied to similar lacustrine basins that experience strong magmatic activity. 相似文献
622.
Shengyi Mao Hongxiang Guan Lihua Liu Xiqiu Han Xueping Chen Juan Yu Yongge Sun Yejian Wang 《海洋学报(英文版)》2021,40(8):53-64
Hydrothermal venting has a profound effect on the chemical and biological properties of local and distal seawater and sediments. In this study, lipid biomarkers were analyzed to examine the potential influence of hydrothermal activity on the fate of organic matter(OM) in surface sediments around Tianxiu Hydrothermal Field in the Carlsberg Ridge(CR), Northwest Indian Ocean. By comparing the biomarker distributions of the samples with that of other typical hydrothermal sediments in the mid ocean ridge, it is shown that the location of the samples is not affected by the hydrothermal activity. The relatively low abundances of terrestrial n-alkyl lipids and riverine1,15-C32 diol suggested a minor contribution of terrigenous OM to the study area. The bacteria contributed predominantly to sedimentary marine OM; however, other marine source organisms, e.g., eukaryotes(i.e.,phytoplankton and fungi) could not be completely neglected. The marine-originated biomarkers showed significantly variable distributions between the two sediments, suggesting different dynamic physical and biogeochemical processes controlling the fate of marine OM. This study identified various diagnostic biomarkers(5,5-diethyl alkanes, diols and β-OH FAs), which may have significant environmental implications for future works in this region. 相似文献
623.
利用1980—1984年和2004—2020年锦州市农业气象观测站春玉米物候观测资料和气象观测资料,采用趋势系数、倾向率、相关分析和通径分析等方法,分析了锦州市春玉米生育期长度和水热条件的变化趋势,并探讨了锦州市春玉米生育期长度与水热条件的关系。结果表明:1980—1984年和2004—2020年锦州地区春玉米各生育期长度变化趋势不同,除抽雄期、成熟期和生殖生长期外,其他生育期长度均呈缩短的趋势。营养生长期长度极显著缩短,生殖生长期长度极显著延长,因此全生育期呈弱的延长趋势,变化不明显。春玉米各生育期水热条件变化趋势不同,热量条件变化显著,而水分条件变化不显著,多数生育期≥10℃活动积温(DT10)和生长度日(GDD)呈增加的趋势,其中抽雄期、成熟期和生殖生长期、全生育期热量条件呈极显著增加趋势,表明热量条件对春玉米生长发育影响最大。相关分析和通径分析表明,DT10和GDD对春玉米生育期长度影响最大,水分条件对春玉米生育期长度影响较小,其中出苗期、成熟期和全生育期长度与水分条件相关显著。可见,锦州地区水热因子之间相互制约、相互影响,共同影响春玉米的整个生育期。 相似文献