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"nsw-blue-carbon-generation-from-existing-mangroves-and-saltmarsh",
            
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  "notes": "Generation is defined as the capacity for existing 
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  "notes": "Generation is defined as the capacity for existing 
            
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mangrove forests and saltmarshes to contribute to carbon additionality 
29
mangrove forests and saltmarshes to contribute to carbon additionality 
            
30
from living biomass, dead organic material, and soil organic carbon. 
30
from living biomass, dead organic material, and soil organic carbon. 
            
31
Several studies indicate that carbon addition is greater in mangrove 
31
Several studies indicate that carbon addition is greater in mangrove 
            
32
forests than saltmarshes (Chmura et al., 2003; Pendleton et al., 
32
forests than saltmarshes (Chmura et al., 2003; Pendleton et al., 
            
33
2012), and this is likely due to greater height and biomass of 
33
2012), and this is likely due to greater height and biomass of 
            
34
mangroves compared to herbaceous saltmarsh vegetation. In NSW where 
34
mangroves compared to herbaceous saltmarsh vegetation. In NSW where 
            
35
both ecosystems occur, mangroves forests typically occupy lower 
35
both ecosystems occur, mangroves forests typically occupy lower 
            
36
positions within the tidal frame than saltmarshes, and their 
36
positions within the tidal frame than saltmarshes, and their 
            
37
distribution can be defined based on elevation and hydroperiod (Hughes 
37
distribution can be defined based on elevation and hydroperiod (Hughes 
            
38
et al., 2019). Additionally, preservation of soil organic carbon 
38
et al., 2019). Additionally, preservation of soil organic carbon 
            
39
within the contemporary range of mangroves has been found to be 
39
within the contemporary range of mangroves has been found to be 
            
40
greater within fine grained sediments of fluvial origin than sandy 
40
greater within fine grained sediments of fluvial origin than sandy 
            
41
coastal barrier sediments. \r\n\r\n\r\n_Chmura, G.L., Anisfeld, S.C., 
41
coastal barrier sediments. \r\n\r\n\r\n_Chmura, G.L., Anisfeld, S.C., 
            
42
Cahoon, D.R., and Lynch, J.C. (2003). Global carbon sequestration in 
42
Cahoon, D.R., and Lynch, J.C. (2003). Global carbon sequestration in 
            
43
tidal, saline wetland soils. Global Biogeochem. Cycles 17, 
43
tidal, saline wetland soils. Global Biogeochem. Cycles 17, 
            
44
1111._\r\n\r\n_Pendleton, L., Donato, D.C., Murray, B.C., Crooks, S., 
44
1111._\r\n\r\n_Pendleton, L., Donato, D.C., Murray, B.C., Crooks, S., 
            
45
Jenkins, W.A., Sifleet, S., Craft, C., Fourqurean, J.W., Kauffman, 
45
Jenkins, W.A., Sifleet, S., Craft, C., Fourqurean, J.W., Kauffman, 
            
46
J.B., Marb\u00e0, N., Megonigal, P., Pidgeon, E., Herr, D., Gordon, 
46
J.B., Marb\u00e0, N., Megonigal, P., Pidgeon, E., Herr, D., Gordon, 
            
47
D., and Baldera, A. (2012). Estimating Global \u201cBlue Carbon\u201d 
47
D., and Baldera, A. (2012). Estimating Global \u201cBlue Carbon\u201d 
            
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Emissions from Conversion and Degradation of Vegetated Coastal 
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Emissions from Conversion and Degradation of Vegetated Coastal 
            
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Ecosystems. PLoS ONE 7, e43542._\r\n",
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Ecosystems. PLoS ONE 7, e43542._\r\n",
            
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  "tags": [
            
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    {
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      "display_name": "Blue Carbon",
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  ],
            
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  "temporal_coverage_from": "2020-05-16",
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  "temporal_coverage_from": "2020-05-16",
            
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  "title": "NSW Blue Carbon Generation from existing mangroves and 
220
  "title": "NSW Blue Carbon Generation from existing mangroves and 
            
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saltmarsh",
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saltmarsh",
            
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}
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}