Rhizocorallium形态结构分析及其古环境意义——以兴义地区中三叠统关岭组为例
		
        
        
        
        
        
	        - 收稿日期:
				2025-06-05
 
			- 网络出版日期:
				2025-11-03
 
			
 		
        
            
            摘要: 摘  要  【目的】研究兴义地区关岭组中大量的Rhizocorallium,分析其潜穴形态与结构特征,旨在揭示潜穴的形成机制、造迹生物的行为习性及其对古沉积环境的指示意义。【方法】测量RhizocoralliumU形潜穴的遗迹管横截面直径和两翼管间距,采用线性回归分析参数相关性,分析其形态结构和造迹过程;通过生物扰动指数(BI)评估扰动强度,并综合岩性等特征,揭示其沉积环境。【结果】(1)Rhizocorallium的基本结构由U形和线形潜穴组成,其形成机制为造迹生物觅食-爬行行为的相互转化;(2)U形遗迹管横截面直径(0.1~2.6 cm)与两翼管间距(0.5~11.9 cm)呈高度正相关(R2=0.92688),表明造迹生物从幼体到成体行为模式高度一致,符合机会种(r-选择)的生存策略特征;(3)关岭组下段生物碎屑灰岩和泥晶灰岩中,以高密度的Rhizocorallium(BI=3~5)为特征,主要分布在低能开阔台地;上段生物碎屑灰岩中,以稀疏的Rhizocorallium(BI=1~3)为特征,主要分布在高能潮间带。【结论】本研究对Rhizocorallium的形态识别与鉴定,揭示了其潜穴特征、形成机制、造迹生物个体发育的行为一致性(r-选择策略)及环境响应适应性,共同支持其作为重建古生态与古环境的可靠遗迹学标志。
             
    
    
 	
    
        Morphological Analysis and Palaeoenvironmental Significance of Rhizocorallium from the Middle Triassic Guanling Formation in the Xingyi Area
		
        
         
		
        
        
	        - Received Date:
				2025-06-05
 
			- Available Online:
				2025-11-03
 
			
        
        
        	
            Abstract: Abstract: [Objective] To study a large number of Rhizocorallium in Guanling Formation in Xingyi area, and analyze the morphological and structural characteristics of its burrows, so as to reveal the behavioral habits of trace-making organisms and their indicative significance to the ancient sedimentary environment. [Methods] The cross-sectional diameter of the relict tube and the distance between the two wing tubes of Rhizocorallium U-shaped burrows were measured. The correlation of parameters was analyzed by linear regression, and the morphological structure and trace-making process were analyzed. The disturbance intensity was evaluated by bioturbation index (BI), and the sedimentary environment was revealed by combining lithology and other characteristics. [Results](1) The basic structure of Rhizocorallium is composed of U-shaped and linear burrows, and its formation mechanism is the mutual transformation of foraging-crawling behavior of trace-making organisms. (2) The cross-sectional diameter (0.1~2.6 cm) of the U-shaped trace tube was highly positively correlated with the distance between the two wing tubes (0.5~11.9 cm) (R2=0.92688), indicating that the behavior patterns of trace-building organisms from larvae to adults were highly consistent, which was consistent with the survival strategy characteristics of opportunistic species (r-selected).The bioclastic limestone and micritic limestone in the lower Guanling Formation are characterized by high-density Rhizocorallium ( BI = 3 ~ 5 ), mainly distributed in low-energy open platforms. The bioclastic limestone in the upper section of the  is characterized by sparse Rhizocorallium ( BI = 1 ~ 3 ), which is mainly distributed in the high-energy intertidal zone. [ Conclusion ] In this study, the morphological identification and identification of Rhizocorallium revealed the characteristics and formation mechanism of its burrow structure, and further confirmed the consistency of behavior and its r-selection strategy in the process of individual development. More importantly, the study clarified the behavioral response and adaptive characteristics of Rhizocorallium to different sedimentary environments. These findings together indicate that Rhizocorallium can be used as a reliable ichnological marker for the reconstruction of paleoecology and paleosedimentary environment.
             
    
   		
			
					
						刘慧, 时国, 何冰琦, 陈星桯, 龚文君, 田钧文. Rhizocorallium形态结构分析及其古环境意义——以兴义地区中三叠统关岭组为例[J]. 沉积学报. doi: 10.14027/j.issn.1000-0550.2025.042
					
				 
			
					
						Morphological Analysis and Palaeoenvironmental Significance of Rhizocorallium from the Middle Triassic Guanling Formation in the Xingyi Area[J]. Acta Sedimentologica Sinica. doi: 10.14027/j.issn.1000-0550.2025.042
						
							
								| Citation: | 
								
									
																			Morphological Analysis and Palaeoenvironmental Significance of Rhizocorallium from the Middle Triassic Guanling Formation in the Xingyi Area[J]. Acta Sedimentologica Sinica. doi: 10.14027/j.issn.1000-0550.2025.042								
									
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