hdl:10013/epic.32749
      
      
      
      Late glacial and Holocene variations of aeolian influx over the northeastern Tibetan Plateau recorded by laminated sediments of a saline meromictic lake
          
  
	Mischke, S., Zhang, C., Börner, A. and Herzschuh, Ulrike 
ORCID: https://orcid.org/0000-0003-0999-1261		
		
			;
			
        
      
      
ORCID: https://orcid.org/0000-0003-0999-1261		
		
			;
			
        
              Contact
            
            
              Ulrike.Herzschuh [ at ] awi.de
            
          
        
        Abstract
      
      
          Item Type
        
        
          Article
          
          
          
        
      
      
        
          Authors
        
        
          
  
	Mischke, S., Zhang, C., Börner, A. and Herzschuh, Ulrike 
ORCID: https://orcid.org/0000-0003-0999-1261		
		
			;
			
        
      
      
        
ORCID: https://orcid.org/0000-0003-0999-1261		
		
			;
			
        
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          Programs
        
        
          Helmholtz Research Programs > PACES I (2009-2013) > TOPIC 3: Lessons from the Past
Helmholtz Research Programs > PACES I (2009-2013) > TOPIC 3: Lessons from the Past > WP 3.1: Past Polar Climate and inter-hemispheric Coupling
      
      
      
      
      
      
      
        Helmholtz Research Programs > PACES I (2009-2013) > TOPIC 3: Lessons from the Past > WP 3.1: Past Polar Climate and inter-hemispheric Coupling
          Publication Status
        
        
          Published
        
      
      
      
        
          Eprint ID
        
        
          20249
        
      
    
        Cite as
      
      
        
 
	   
		
Mischke, S. 			
		,		
Zhang, C. 			
		,		
Börner, A. 			
		
				
					and
				
					
Herzschuh, U. 			
		
				
					
		
	
	
  
	(2009):	
	Late glacial and Holocene variations of aeolian influx over the northeastern Tibetan Plateau recorded by laminated sediments of a saline meromictic lake
		
	,	
 
		Journal of Quaternary Science.
	    
		
		
		
				
		.
	  
	
      
      
      
        
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