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RB 37/00136 Microfossils from Pleistocene to recent deposits, Lake Eyre South.
Published: 01 Jan 1956 Created: 04 Nov 2024 Revised: 04 Nov 2024
Author: Ludbrook, N.H.

Samples from sands, clays and limestones on the southern eastern corner of Lake Eyre were found to contain remains of fresh or brackish water microscopic plants and animals which inhabit inland and coastal lagoons, together with species of...

Samples from sands, clays and limestones on the southern eastern corner of Lake Eyre were found to contain remains of fresh or brackish water microscopic plants and animals which inhabit inland and coastal lagoons, together with species of brackish water foraminifera. Deposition probably took place during Pleistocene high sea levels.

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Record No rb3700136
Topic Geoscientific Information
Type of Resource Document
Category Type
Document Type Departmental Publication - Geological Survey Geoscience Publication
Contributor
Sponsor
Tenement
Tenement Holder
Operator
Geological Province
    Mine Name
    Stratigraphy
    Commodity
      Notes 
      Geographic Locality: Lake Eyre
Doc No: RB 37/00136 p: na
      Geographic Locality: Lake Eyre
Doc No: RB 37/00136 p: na
      Language English
      Metadata Standard ISO 19115-3

      Citations

      Use constraints License
      License Creative Commons Attribution 4.0
      Persistent identifier https://pid.sarig.sa.gov.au/document/rb3700136
      Citation Ludbrook, N.H. 1956. RB 37/00136 Microfossils from Pleistocene to recent deposits, Lake Eyre South. Departmental Publication - Geological Survey Geoscience Publication. Government of South Australia.
      https://pid.sarig.sa.gov.au/document/rb3700136

      Technical information

      Status
      Maintenance and Update Frequency
      Geographic Reference GDA2020 (EPSG:7844)
      Geo bounding box {"type":"Polygon","coordinates":[[[137.5,-29],[138,-29],[138,-28.5],[137.5,-28.5],[137.5,-29]]]}
      Purpose 
      
                    
                    
      
                    
                        		
                
      
              
                
                
      
                  
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