-
Peel-Harvey Estuary Water Quality Data
The dataset consists of water quality parameters that have been monitored on a weekly to monthly basis at three sites in Peel Inlet and central site in Harvey Estuary from... -
Peel-Harvey Estuary Rainfall Data
Rainfall data from 1889 to 1993 for areas near the Peel-Harvey Estuary collected by Bureau of Meteorology as part of their routine weather monitoring programme. -
Parent Record: Social monogamy in the fiddler crab Uca capricornis
Fiddler crabs are not generally considered subjects for the study of monogamy as they tend to live in dense mixed sex colonies with numerous neighbours and individually defended... -
Parent record: Owner advantage in the fiddler crab, Uca mjoebergi: Investigating why owners win more contests?
Resource owners generally win contests against intruders, a phenomenon referred to as the 'Owner Advantage' (OA). Uca mjoebergi is a typical fiddler crab that is highly... -
Parent record: Datasets relating to core MD032607 (off South Australia)
We must understand the natural cycles of the oceans to understand the evolution of our climate through geological time. Core MD 032607 was obtained in 2003 off the coast of... -
Parent record: Datasets relating to core MD002361 (shelf edge offshore Western Australia)
We must understand the natural cycles of the oceans to understand the evolution of our climate through geological time. Core MD 002361 was obtained in 2000 off the coast of... -
Parent record: Datasets relating to core GC-14, located in the Capricorn Channel at a depth of 2004 mbsl
Core GC14 (23o49' 52S 154o21' 67E) was collected from the Capricorn Channel at a depth of 2004 mbsl (metres below sea level). By investigating the properties and components of... -
Parent record: Datasets relating to core GC13, located in the Capricorn Channel at a depth of 1482 mbsl
Core GC13 (23o47' 30S 154o13' 56E) was collected from the Capricorn Channel at a depth of 1482 mbsl (metres below sea level). By investigating the properties and components of... -
Parent record: Datasets relating to core GC-12, located in the Capricorn Channel at a depth of 990.5 mbsl
Core GC12 (23o34' 37S 153o49' 94E) was collected from the Capricorn Channel at a depth of 990.5 mbsl (metres below sea level). By investigating the properties and components of... -
Parent record: Datasets relating to core GC-11, located in the Capricorn Channel at a depth of 502 mbsl
Core GC11 (23o23' 07S 153o22' 00E) was collected from the Capricorn Channel at a depth of 502 mbsl (metres below sea level). By investigating the properties and components of... -
Parent record: Datasets relating to core GC-10, located in the Capricorn Channel at a depth of 335 mbsl
Core GC10 (22o59 76S 152o48' 00E) was collected from the Capricorn Channel at a depth of 335 mbsl (metres below sea level). By investigating the properties and components of... -
Parent record: Datasets relating to core GC-09, located in the Capricorn Channel at a depth of 166 mbsl.
Core GC09 (22o53' 70S 152o38' 10E) was collected from the Capricorn Channel at a depth of 166 mbsl (metres below sea level). By investigating the properties and components of... -
Parent record: Datasets relating to core BAR9403 (off the coast of Sumatra)
We must understand the natural cycles of the oceans to understand the evolution of our climate through geological time. Core BAR 9403 was obtained in 1994 off the coast of... -
Parent Record: Colouration and Colour Changes of the Fiddler Crab, Uca capricornis
The purpose of this investigation was to quantitatively describe the colour patterns of the fiddler crab Uca capricornis and their ability to change on a socially significant... -
Oxygen-isotope records, age-model results and sedimentation rates of core MD88-787
Core MD88-787 was recovered during the French ASPARA IV cruise in 1988, aboard the Marion Dufresne. The core was located on the Tasman Fracture Zone of the Mid-Ocean Ridge,... -
Oxygen-isotope records, age-model results and sedimentation rates of core MD88-784
Core MD88-784 was recovered during the French ASPARA IV cruise in 1988, aboard the Marion Dufresne. The core was located on the Tasman Fracture Zone of the Mid-Ocean Ridge,... -
Oxygen-isotope records, age-model results and sedimentation rates of core MD88-779
Core MD88-779 was taken during the 1988 French ASPARA IV cruise in the South East Indian Ocean aboard the Marion DuFresne. The core was situated on the South Tasman Rise... -
Oxygen isotope (18-O) values for 5 different foraminiferal species down the core of GC12, collected from the Capricorn Channel
A gravity core (GC12) was collected from a depth of 990.5 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). The 18-O values of the different foraminiferal... -
Owner Advantage in the fiddler crab, Uca mjoebergi. Fight data between burrow owners and natural floaters
Resource owners generally win contests against intruders, a phenomenon referred to as the 'Owner Advantage' (OA). Uca mjoebergi is a typical fiddler crab that is highly... -
Owner Advantage in the fiddler crab, Uca mjoebergi. Do owners win more contests than floaters because they are superior fighters?
Resource owners generally win contests against intruders, a phenomenon referred to as the 'Owner Advantage' (OA). Uca mjoebergi is a typical fiddler crab that is highly...