Changes
On May 16, 2022 at 12:24:04 PM +1000, National Native Title Tribunal:
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Added resource NSW Blue Carbon Permanency in Belowground Sediments to NSW Blue Carbon Permanency in Belowground Sediments
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Added resource NSW Blue Carbon Permanency in Belowground Sediments to NSW Blue Carbon Permanency in Belowground Sediments
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Added resource WMS - NSW Blue Carbon Permanency in Belowground Sediments to NSW Blue Carbon Permanency in Belowground Sediments
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Added resource Metadata statement to NSW Blue Carbon Permanency in Belowground Sediments
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Deleted resource WMS - NSW Blue Carbon Permanency in Belowground Sediments from NSW Blue Carbon Permanency in Belowground Sediments
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Deleted resource NSW Blue Carbon Permanency in Belowground Sediments from NSW Blue Carbon Permanency in Belowground Sediments
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Deleted resource NSW Blue Carbon Permanency in Belowground Sediments from NSW Blue Carbon Permanency in Belowground Sediments
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Deleted resource Metadata statement from NSW Blue Carbon Permanency in Belowground Sediments
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25 | "name": "nsw-blue-carbon-permanency-in-belowground-sediments", | 25 | "name": "nsw-blue-carbon-permanency-in-belowground-sediments", | ||
26 | "notes": "Permanency is defined as the capacity for carbon to be | 26 | "notes": "Permanency is defined as the capacity for carbon to be | ||
27 | preserved and not reworked under conditions of higher hydrodynamic | 27 | preserved and not reworked under conditions of higher hydrodynamic | ||
28 | energy associated with storms and changes to tidal regimes. The | 28 | energy associated with storms and changes to tidal regimes. The | ||
29 | permanency of carbon within substrates has been questioned (DeLaune | 29 | permanency of carbon within substrates has been questioned (DeLaune | ||
30 | and White, 2012; Kirwan and Mudd, 2012), particularly in the context | 30 | and White, 2012; Kirwan and Mudd, 2012), particularly in the context | ||
31 | of increased storminess. This component does not specifically indicate | 31 | of increased storminess. This component does not specifically indicate | ||
32 | retreat pathways for coastal ecosystems as they respond to sea-level | 32 | retreat pathways for coastal ecosystems as they respond to sea-level | ||
33 | rise. Lower elevations on estuarine shorelines may be exposed to | 33 | rise. Lower elevations on estuarine shorelines may be exposed to | ||
34 | greater hydrodynamic energy due to fetch and wave-action, whilst | 34 | greater hydrodynamic energy due to fetch and wave-action, whilst | ||
35 | coastal barrier sediments are more exposed to high wave energy of the | 35 | coastal barrier sediments are more exposed to high wave energy of the | ||
36 | open ocean; the exposure of these sediments to higher hydrodynamic | 36 | open ocean; the exposure of these sediments to higher hydrodynamic | ||
37 | energy increases the probability of reworking and poses considerable | 37 | energy increases the probability of reworking and poses considerable | ||
38 | risk to carbon permanency. \r\n\r\n\r\n_DeLaune, R., and White, J. | 38 | risk to carbon permanency. \r\n\r\n\r\n_DeLaune, R., and White, J. | ||
39 | (2012). Will coastal wetlands continue to sequester carbon in response | 39 | (2012). Will coastal wetlands continue to sequester carbon in response | ||
40 | to an increase in global sea level?: a case study of the rapidly | 40 | to an increase in global sea level?: a case study of the rapidly | ||
41 | subsiding Mississippi river deltaic plain. Climatic Change 110, | 41 | subsiding Mississippi river deltaic plain. Climatic Change 110, | ||
42 | 297-314._\r\n\r\n_Kirwan, M.L., and Mudd, S.M. (2012). Response of | 42 | 297-314._\r\n\r\n_Kirwan, M.L., and Mudd, S.M. (2012). Response of | ||
43 | salt-marsh carbon accumulation to climate change. Nature 489, | 43 | salt-marsh carbon accumulation to climate change. Nature 489, | ||
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57 | Natural Resources, Strategy & Policy and Business | 57 | Natural Resources, Strategy & Policy and Business | ||
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174 | "state": "active", | 174 | "state": "active", | ||
175 | "tags": [ | 175 | "tags": [ | ||
176 | { | 176 | { | ||
177 | "display_name": "Blue Carbon", | 177 | "display_name": "Blue Carbon", | ||
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180 | "state": "active", | 180 | "state": "active", | ||
181 | "vocabulary_id": null | 181 | "vocabulary_id": null | ||
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188 | "vocabulary_id": null | 188 | "vocabulary_id": null | ||
189 | }, | 189 | }, | ||
190 | { | 190 | { | ||
191 | "display_name": "Permanency", | 191 | "display_name": "Permanency", | ||
192 | "id": "6d7e4f93-f422-45a3-a3d4-ab536331ff9a", | 192 | "id": "6d7e4f93-f422-45a3-a3d4-ab536331ff9a", | ||
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195 | "vocabulary_id": null | 195 | "vocabulary_id": null | ||
196 | }, | 196 | }, | ||
197 | { | 197 | { | ||
198 | "display_name": "mangroves", | 198 | "display_name": "mangroves", | ||
199 | "id": "e8d047d0-f9e1-4604-b9c8-81c2c7e9a7eb", | 199 | "id": "e8d047d0-f9e1-4604-b9c8-81c2c7e9a7eb", | ||
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203 | }, | 203 | }, | ||
204 | { | 204 | { | ||
205 | "display_name": "saltmarsh", | 205 | "display_name": "saltmarsh", | ||
206 | "id": "6e1f377b-31d3-4616-9e8a-104b8312d595", | 206 | "id": "6e1f377b-31d3-4616-9e8a-104b8312d595", | ||
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208 | "state": "active", | 208 | "state": "active", | ||
209 | "vocabulary_id": null | 209 | "vocabulary_id": null | ||
210 | } | 210 | } | ||
211 | ], | 211 | ], | ||
212 | "temporal_coverage_from": "2020-05-16", | 212 | "temporal_coverage_from": "2020-05-16", | ||
213 | "title": "NSW Blue Carbon Permanency in Belowground Sediments", | 213 | "title": "NSW Blue Carbon Permanency in Belowground Sediments", | ||
214 | "type": "dataset", | 214 | "type": "dataset", | ||
215 | "unpublished": "false", | 215 | "unpublished": "false", | ||
216 | "update_freq": "unknown", | 216 | "update_freq": "unknown", | ||
217 | "url": "", | 217 | "url": "", | ||
218 | "version": null | 218 | "version": null | ||
219 | } | 219 | } |