AndreaBozzo/ceres-open-data-index huggingface dataset:
AIMS Weather Station Data - AIMS Wharf Platform Historical Wind -  From 01 Nov 1983 To 30 May 1984

This data set was collected by weather sensors deployed on the AIMS Weather Station site AIMS Wharf WS.

Instrumentation was deployed for measuring Wind Speed from 01 Nov 1983 through to 30 May 1984, and the installation was located at/on AIMS Wharf Platform Historical Latitude:-19.277325 - Longitude:147.05854. 

Instrumentation was deployed for measuring Wind Direction from 01 Nov 1983 through to 30 May 1984, and the installation was located at/on AIMS Wharf Platform Historical Latitude:-19.277325 - Longitude:147.05854.

Tags: Atmosphere, Atmospheric Pressure, Atmospheric Pressure Measurements, Atmospheric Sciences, EARTH SCIENCES, Meteorology, Ocean Temperature, Ocean Winds, Oceans, Surface Winds, Water Temperature
Organization: Australian Institute of Marine Science
AIMS Weather Station Data - AIMS Wharf Platform Historical Light -  From 01 Nov 1983 To 30 May 1984

This data set was collected by weather sensors deployed on the AIMS Weather Station site AIMS Wharf WS.

Instrumentation was deployed for measuring PAR from 01 Nov 1983 through to 30 May 1984, and the installation was located at/on AIMS Wharf Platform Historical Latitude:-19.277325 - Longitude:147.05854.

Tags: Atmosphere, Atmospheric Pressure, Atmospheric Pressure Measurements, Atmospheric Sciences, EARTH SCIENCES, Meteorology, Ocean Temperature, Ocean Winds, Oceans, Surface Winds, Water Temperature
Organization: Australian Institute of Marine Science
AIMS Weather Station Data - AIMS Wharf Platform Historical Air Temperature -  From 01 Nov 1983 To 30 May 1984

This data set was collected by weather sensors deployed on the AIMS Weather Station site AIMS Wharf WS.

Instrumentation was deployed for measuring Air Temperature from 01 Nov 1983 through to 30 May 1984, and the installation was located at/on AIMS Wharf Platform Historical Latitude:-19.277325 - Longitude:147.05854.

Tags: Atmosphere, Atmospheric Pressure, Atmospheric Pressure Measurements, Atmospheric Sciences, EARTH SCIENCES, Meteorology, Ocean Temperature, Ocean Winds, Oceans, Surface Winds, Water Temperature
Organization: Australian Institute of Marine Science
AIMS Weather Station Data - AIMS Wharf Platform Historical Air Pressure -  From 01 Nov 1983 To 30 May 1984

This data set was collected by weather sensors deployed on the AIMS Weather Station site AIMS Wharf WS.

Instrumentation was deployed for measuring Air Pressure from 01 Nov 1983 through to 30 May 1984, and the installation was located at/on AIMS Wharf Platform Historical Latitude:-19.277325 - Longitude:147.05854.

Tags: Atmosphere, Atmospheric Pressure, Atmospheric Pressure Measurements, Atmospheric Sciences, EARTH SCIENCES, Meteorology, Ocean Temperature, Ocean Winds, Oceans, Surface Winds, Water Temperature
Organization: Australian Institute of Marine Science
AIMS Weather Station Data - Agincourt_Weather Light -  From 22 Feb 1991 To 03 Oct 2017

This data set was collected by weather sensors deployed on the AIMS Weather Station site Agincourt Reef Number 3.

There have been 4 deployments for the PAR data set.

Instrumentation was deployed for measuring PAR from 22 Feb 1991 through to 22 Mar 2013, and the installation was located at/on Agincourt_Weather Latitude:-15.98278 - Longitude:145.82251. 

Instrumentation was deployed for measuring PAR from 22 Feb 2013 through to 04 Mar 2015, and the installation was located at/on Agincourt_Weather Latitude:-15.98278 - Longitude:145.82251. Sensor deployed was a Licor LI-192SA Quantum Sensor (PAR Sensor) manufactured by LI-COR Inc., model LI-192SA. 

Instrumentation was deployed for measuring PAR from 03 Mar 2015 through to 06 Oct 2016, and the installation was located at/on Agincourt_Weather Latitude:-15.98278 - Longitude:145.82251. Sensor deployed was a Licor LI-192SA Quantum Sensor (PAR Sensor) manufactured by LI-COR Inc., model LI-192SA. 

Instrumentation was deployed for measuring PAR from 29 Sep 2016 through to 03 Oct 2017, and the installation was located at/on Agincourt_Weather Latitude:-15.98278 - Longitude:145.82251. Sensor deployed was a Licor LI-192SA Quantum Sensor (PAR Sensor) manufactured by LI-COR Inc., model LI-192SA.

Tags: Atmospheric Sciences, EARTH SCIENCES, Meteorology, Ocean Temperature, Oceans, Water Temperature
Organization: Australian Institute of Marine Science
AIMS Weather Station Data - Agincourt_Weather Humidity -  From 02 Jan 2000 To 03 Oct 2017

This data set was collected by weather sensors deployed on the AIMS Weather Station site Agincourt Reef Number 3.

There have been 4 deployments for the Humidity data set.

Instrumentation was deployed for measuring Humidity from 02 Jan 2000 through to 30 Dec 2005, and the installation was located at/on Agincourt_Weather Latitude:-15.98278 - Longitude:145.82251. 

Instrumentation was deployed for measuring Humidity from 20 Mar 2013 through to 04 Mar 2015, and the installation was located at/on Agincourt_Weather Latitude:-15.98278 - Longitude:145.82251. Sensor deployed was a Vaisala WXT520 Weather Transmitter manufactured by Vaisala, model WXT520. 

Instrumentation was deployed for measuring Humidity from 03 Mar 2015 through to 06 Oct 2016, and the installation was located at/on Agincourt_Weather Latitude:-15.98278 - Longitude:145.82251. Sensor deployed was a Vaisala WXT510/WXT520 Weather Transmitter manufactured by Vaisala, model WXT510. 

Instrumentation was deployed for measuring Humidity from 29 Sep 2016 through to 03 Oct 2017, and the installation was located at/on Agincourt_Weather Latitude:-15.98278 - Longitude:145.82251. Sensor deployed was a Vaisala WXT520 Weather Transmitter manufactured by Vaisala, model WXT520.

Tags: Atmospheric Sciences, EARTH SCIENCES, Meteorology, Ocean Temperature, Oceans, Water Temperature
Organization: Australian Institute of Marine Science
AIMS Weather Station Data - Agincourt_Weather Air Temperature -  From 22 Feb 1991 To 03 Oct 2017

This data set was collected by weather sensors deployed on the AIMS Weather Station site Agincourt Reef Number 3.

There have been 4 deployments for the Air Temperature data set.

Instrumentation was deployed for measuring Air Temperature from 22 Feb 1991 through to 22 Mar 2013, and the installation was located at/on Agincourt_Weather Latitude:-15.98278 - Longitude:145.82251. 

Instrumentation was deployed for measuring Air Temperature from 20 Mar 2013 through to 04 Mar 2015, and the installation was located at/on Agincourt_Weather Latitude:-15.98278 - Longitude:145.82251. Sensor deployed was a Vaisala WXT520 Weather Transmitter manufactured by Vaisala, model WXT520. 

Instrumentation was deployed for measuring Air Temperature from 03 Mar 2015 through to 06 Oct 2016, and the installation was located at/on Agincourt_Weather Latitude:-15.98278 - Longitude:145.82251. Sensor deployed was a Vaisala WXT510/WXT520 Weather Transmitter manufactured by Vaisala, model WXT510. 

Instrumentation was deployed for measuring Air Temperature from 29 Sep 2016 through to 03 Oct 2017, and the installation was located at/on Agincourt_Weather Latitude:-15.98278 - Longitude:145.82251. Sensor deployed was a Vaisala WXT520 Weather Transmitter manufactured by Vaisala, model WXT520.

Tags: Atmospheric Sciences, EARTH SCIENCES, Meteorology, Ocean Temperature, Oceans, Water Temperature
Organization: Australian Institute of Marine Science
AIMS Weather Station Data - Agincourt_Weather Air Pressure -  From 22 Feb 1991 To 03 Oct 2017

This data set was collected by weather sensors deployed on the AIMS Weather Station site Agincourt Reef Number 3.

There have been 4 deployments for the Air Pressure data set.

Instrumentation was deployed for measuring Air Pressure from 22 Feb 1991 through to 22 Feb 2013, and the installation was located at/on Agincourt_Weather Latitude:-15.98278 - Longitude:145.82251. 

Instrumentation was deployed for measuring Air Pressure from 20 Mar 2013 through to 04 Mar 2015, and the installation was located at/on Agincourt_Weather Latitude:-15.98278 - Longitude:145.82251. Sensor deployed was a Vaisala WXT520 Weather Transmitter manufactured by Vaisala, model WXT520. 

Instrumentation was deployed for measuring Air Pressure from 03 Mar 2015 through to 06 Oct 2016, and the installation was located at/on Agincourt_Weather Latitude:-15.98278 - Longitude:145.82251. Sensor deployed was a Vaisala WXT510/WXT520 Weather Transmitter manufactured by Vaisala, model WXT510. 

Instrumentation was deployed for measuring Air Pressure from 29 Sep 2016 through to 03 Oct 2017, and the installation was located at/on Agincourt_Weather Latitude:-15.98278 - Longitude:145.82251. Sensor deployed was a Vaisala WXT520 Weather Transmitter manufactured by Vaisala, model WXT520.

Tags: Atmospheric Sciences, EARTH SCIENCES, Meteorology, Ocean Temperature, Oceans, Water Temperature
Organization: Australian Institute of Marine Science
AIMS Water Quality Chlorophyll and Turbidity Time-series Data

The Reef Plan Marine Monitoring Program (MMP) at AIMS monitors inshore water quality of the Great Barrier Reef (GBR). This includes the deployment of sensors at fixed coral reef sites along the GBR since 2007, with some additional sites added near river mouths since 2015. Continuous in situ measurements of chlorophyll fluorescence and turbidity are performed at these inshore sites using WET Labs ECO FLNTUSB Combination Fluorometer and Turbidity Sensors. 

The sensors are deployed for periods of approximately 4 month duration before recovery, when another instrument is deployed in its place. The time series data is uploaded upon recovery. The instruments have calibration checks performed and battery changes in-house, as well as servicing on a regular basis.

Tags: Data Loggers, Fluorometers, Oceans, Thermistors, Turbulence Sensors, Water Quality
Organization: Australian Institute of Marine Science
AGSO Cruise Report: Cruise 210 : The "Sojourn 7" Swath-mapping Cruise of R.V. Melville off Eastern Tasmania and in the Gippsland Basin

From 10 to 17 April 1997, the Australian Geological Survey Organisation (AGSO) chartered the 85 m Research Vessel Melville from Scripps Institution of Oceanography on a cooperative scientific basis, to map the sea bed east and northeast of Tasmania including the deep water part of the Gippsland Basin. The vessel was equipped with the SeaBeam 2000 multibeam sonar system, capable of swath-mapping the morphology and roughness of the sea bed in a swath 3.5 times as wide as the water depth. The central beam gave a 12 kHz bathymetric profile. Other equipment employed included a magnetometer and gravity meter. Navigation, by military standard GPS using the P code, had an accuracy of about 5 m. Detailed ship's tracks for the survey, from south to north, are shown in Figures 2-5.

The aims of the cruise were to determine the morphology and sea bed character of selected areas, to aid in tectonic, basin and sedimentological studies, to aid the fishing industry, and to provide critical information for future seismic profiling and geological sampling. Satellite gravity images, and sparse bathymetric and seismic profiles, were used to plan the survey.

You can also purchase hard copies of Geoscience Australia data and other products at http://www.ga.gov.au/products-services/how-to-order-products/sales-centre.html

Tags: Earth Sciences, GA Publication, Record, marine, marine survey, seismics
Organization: Geoscience Australia
Agriculture land interface area

This layer is displayed on the Industry, community infrastructure and agriculture land interface area overlay map in City Plan version 7 as 'Agriculture land interface area'. The layer is also available in Council’s City Plan interactive mapping tool. For further information on City Plan, please visit http://www.goldcoast.qld.gov.au/planning-and-building/city-plan-2015-19859.html

Tags: Agriculture land interface area, City Plan, City of Gold Coast, CoGC, Planning and building, agricultural, agriculture, open data, planning
Organization: City of Gold Coast
Agriculture land

This layer is displayed on the Industry, community infrastructure and agriculture land interface area overlay map in City Plan version 7 as 'Agriculture land'. The layer is also available in Council’s City Plan interactive mapping tool. For further information on City Plan, please visit http://www.goldcoast.qld.gov.au/planning-and-building/city-plan-2015-19859.html

Tags: City Plan, City of Gold Coast, CoGC, agricultural land, agriculture, planning
Organization: City of Gold Coast
Aggregations of common holothurians on reef flats of Coral Bay, Ningaloo Reef, North Western Australia

The distribution of three sea cucumbers (H. whitmaei (Bell 1887), H. atra (Jaeger 1933) and S. chloronotus (Brandt 1835) in the vincinity of Coral Bay, Ningaloo Reef, Western Australia was measured.  There was an emphasis on factors that may contribute to the heterogeneous distribution of H. whitmaei within broadly defined habitats and reasons for variable density estimates reported in the literature.

Tags: 25 416003, 25 416033, 25 417001, Aquatic Habitat, Biosphere, Ecological Dynamics, Habitat selection, Holothuria whitmaei, Marine Biology, Marine Invertebrates, Oceans, Population Dynamics, Population density survey, Range Changes, Reef Habitat, Spatial distribution, Stichopus chloronotus, black teatfish, green fish, lolly fish
Organization: BMT Oceanica
Age vs Depth profile of core GC14, collected from the Capricorn Channel off the Eastern Australian Coast

A gravity core (GC14) was collected from a depth of 2004 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Isotopic values for 18-O and 13-C were obtained from : Globigerinoides ruber and correlated with the SPECMAP age-model. It appears that the core extends back to MIS 3 (Marine Isotope Stage). From limited depth matching with the Martinson et al. (1987) SPECMAP age-model it is extremely difficult to determine a sedimentation rate, however, it exhibits a relatively uniform rate throughout the core of ~4cm/kyr. This is a fairly high sedimentation rate for a core this distal and abyssal.

Tags: 51200000, Foraminifera, Foraminiferans, Foraminiferida, Marine Sediments, Oceans, Sedimentation
Organization: National Institute of Water and Atmosphere (NIWA)
Age vs Depth profile of core GC13, collected from the Capricorn Channel off the Eastern Australian Coast

A gravity core (GC13) was collected from a depth of 1482 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Isotopic values for 18-O and 13-C were obtained from Globigerinoides ruber and correlated with the SPECMAP age-model. The age-model that was produced plausibly extends back to Marine Isotope Stage (MIS) 6, with approximate sedimentation rates calculated according to this model. Sedimentation rates fluctuate from 5cm/kyr during the last transition and interglacial, to 1cm/kyr during the glacial maximum.

Tags: 51200000, Foraminfera, Foraminiferans, Foraminiferida, Marine Sediments, Oceans, Sedimentation
Organization: National Institute of Water and Atmosphere (NIWA)
Age vs Depth profile of core GC12, collected from the Capricorn Channel off the Eastern Australian Coast

A gravity core (GC12) was collected from a depth of 990.5 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Isotopic values for 18-O and 13-C were obtained from Globigerinoides ruber and correlated with the SPECMAP age-model. Radiocarbon dating of Globigerinoides sacculifer was also undertaken at nine sample depths, and then corrected and correlated with the curve. This yielded an age vs. depth profile from which it was possible to determine approximate sedimentation rates. From the age-model we see the evidence of MIS 1 through to 5a with sedimentation rates ranging from 2 cm/kyr to 20 cm/kyr, with an average of 10cm/kyr. This is a high sedimentation rate for a sedimentary basin, however the core is situated on the increased slope of the Capricorn Channel, therefore sediments scoured off the shallow gradient slope above may feasibly be focused at this depth on the slope. The sedimentation rate exhibits a unorthodox pattern, with a very high rate (25 cm/kyr) during the middle of MIS 3.

Tags: 51200000, Foraminifera, Foraminiferans, Foraminiferida, Isotopes, Marine Sediments, Oceans, Paleoclimate, Sedimentation
Organization: National Institute of Water and Atmosphere (NIWA)
Age vs Depth profile of core GC11, collected from the Capricorn Channel off the Eastern Australian Coast

A gravity core (GC11) was collected from a depth of 502 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Isotopic values for 18O and 13C were obtained from Gs. ruber and correlated with the SPECMAP age-model. The results highlight 4 glacial cycles, incorporating Marine Isotope Stage (MIS) 1 through to MIS 11. Isotopically heavier 18O values at ~460cm, ~345cm, 150cm, and 30cm correspond respectively to MIS 10 (359 kyr BP), MIS 8 (260 kyr BP), MIS 6 (140 kyr BP) and the LGM (20 kyr BP). Sedimentation rates are typically low, <1 cm/kyr to ~4 cm/kyr. The higher sedimentation rates are evident at glacial / interglacial terminations, but then drop off rapidly in the interglacials.

Tags: 51200000, Foraminifera, Foraminiferans, Foraminiferida, Marine Sediments, Oceans, Sedimentation
Organization: National Institute of Water and Atmosphere (NIWA)
Age vs Depth profile of core GC10, collected from the Capricorn Channel off the Eastern Australian Coast

A gravity core (GC10) was collected from a depth of 335 mbsl within the Capricorn Channel, southern Great Barrier Reef (GBR). Isotopic values for 18O and 13C were obtained from Gs. ruber and correlated with the SPECMAP age-model. Radiocarbon dating of G. sacculifer was also undertaken at three sample depths, and then corrected and correlated with the curve. This yielded an age vs. depth profile from which it was possible to determine approximate sedimentation rates. The results place the Last Glacial Maximum (LGM) date at 130cm and highlights a peak in sedimentation rate during the penultimate glacial / interglacial transition. Down the core the sedimentation rates vary considerably from a high of 12 cm/kyr down to <1 cm/kyr. This is probably the result of a considerable change in the sediment flux related to the sea level fluctuations.

Tags: 51200000, Foraminifera, Foraminiferans, Foraminiferida, Marine Sediments, Oceans, Paleoclimate, Radiocarbon, Sedimentation
Organization: National Institute of Water and Atmosphere (NIWA)
Age vs. Depth of core MD032607 (off South Australia). Age has been calculated through modelling based on oxygen isotope records from Globigerina bulloides

The age with depth of core MD032607 is calculated through 18O values, which are then correlated with the SPECMAP age-model. Based upon these measurements the age at the deepest part of the core (3270cm) is ~176,590yrs BP. The age vs. depth profile for this core indicates a major increase in the sedimentation rate during the initial phase of MIS 6, when the sedimentation rate is ~41cm/1000yrs. The average sedimentation rate over the length of the core is 18.7cm/1000yrs.

Tags: 51200000, Age vs. depth profile, Marine Sediments, Oceans, Oxygen Isotopes, Paleoclimate, Sedimentation
Organization: Australian National University
Age vs. depth of core MD002361 (shelf edge offshore Western Australia). Age has been calculated using radiocarbon dating and modelling based on oxygen isotope records.

Radiocarbon dating was used to construct an age model for the upper sections of core MD002361 to a depth of 205cm, after which the age-model was based on the chronology of Bassinot et al. as the core extends beyond the Marine Isotope Stages (MIS) of SPECMAP. The age versus depth profile for this core shows a step-like pattern with increased sedimentation rates during interglacial periods and decreased rates during glacial periods. The average sedimentation rate over the length of the core is 2.5cm/1000yrs, with a high sedimentation rate illustrated during the holocene (15cm/1000yrs). It appears that the sedimentation rate may be affected by river discharge, with an increase in red-brown sediment during the interglacial periods. This is shown with an increase in sedimentation rate during MIS 5 and MIS 11. The age at the deepest part of the core (1360cm) is ~549,058yrs BP.

Tags: Age vs. Depth Profile, Marine Sediments, Oceans, Sedimentation
Organization: Australian National University
Age vs. Depth of core BAR 9403 (located off the coast of Sumatra). Age has been calculated through modelling based on oxygen isotope records

The age with depth of core BAR9403 is calculated through 18O values, which are then correlated with the SPECMAP age-model. Based upon these measurements the age at the deepest part of the core (275cm) was calculated to be ~33,200yrs BP. The age vs. depth profile indicates a reasonably constant sedimentation rate, with an average deposition rate of ~8cm/1000yrs.

Tags: Age vs. Depth, Marine Sediments, Oceans, Sedimentation
Organization: Australian National University
Ages of insolvent debtors

AFSA publish statistics on the age of insolvent debtors at the time of their insolvency. Debtors supply their date of birth on the statement of affairs. AFSA calculate the age of debtors using date of birth from the statement of affairs and the date that their personal insolvency commenced.

Please refer to https://www.afsa.gov.au/resources/statistics/socio-economic-statistics/ages/guide-to-ages-of-insolvent-debtors for more information about the data.

Tags: Age, debtor, insolvent debtors
Organization: Australian Financial Security Authority
Nyssanthes impervia potential habitat grid


## **Abstract** 
The dataset was compiled by the Geological and Bioregional Assessment Program from source data referenced within the dataset and/or metadata. Nyssanthes impervia potential habitat grid


## **Attribution** 
Geological and Bioregional Assessment Program


## **History** 
This dataset was created by intersecting WildNet observations with the Queensland regional ecosystem layers. All REs intersecting with these points were considered potential habitat and burned into a 500 m reference grid.

Organization: Bioregional Assessment Program
Isa: Species (distribution and occurrence) by landscape classes


## **Abstract** 
The dataset was derived by the Geological and Bioregional Assessment Program from multiple source datasets. The source datasets are identified in the Lineage field in this metadata statement. The processes undertaken to produce this derived dataset are described in the History field in this metadata statement.


## **Attribution** 
Geological and Bioregional Assessments


## **History** 
Species occurrences and mapped distributions were clipped to the Isa assessment region and intersected with the landscape classes. The area of spatial distribution and count of occurrences were calculated for each species within each of the landscape classes.

Organization: Bioregional Assessment Program