{"dp_type": "Dataset", "free_text": "Mercury"}
[{"awards": "0739575 Emslie, Steven", "bounds_geometry": ["POLYGON((-57.3 -63.3,-57.22 -63.3,-57.14 -63.3,-57.06 -63.3,-56.98 -63.3,-56.9 -63.3,-56.82 -63.3,-56.74 -63.3,-56.66 -63.3,-56.58 -63.3,-56.5 -63.3,-56.5 -63.4,-56.5 -63.5,-56.5 -63.6,-56.5 -63.7,-56.5 -63.8,-56.5 -63.9,-56.5 -64,-56.5 -64.1,-56.5 -64.2,-56.5 -64.3,-56.58 -64.3,-56.66 -64.3,-56.74 -64.3,-56.82 -64.3,-56.9 -64.3,-56.98 -64.3,-57.06 -64.3,-57.14 -64.3,-57.22 -64.3,-57.3 -64.3,-57.3 -64.2,-57.3 -64.1,-57.3 -64,-57.3 -63.9,-57.3 -63.8,-57.3 -63.7,-57.3 -63.6,-57.3 -63.5,-57.3 -63.4,-57.3 -63.3))"], "date_created": "Wed, 30 Jun 2021 00:00:00 GMT", "description": "Total mercury concentrations and corrected stable isotope signatures quantified in Ad\u00e9lie Penguin eggshell membrane and feathers recovered from the breast of deceased fledglings. 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One such mechanistic question is how bromine (BrO and Br) enriched snow migrates or is formed through processes in sea-ice, prior to its subsequent mobilization as an aerosol fraction into the atmosphere by strong winds. Once aloft, it may react with ozone and other atmospheric species. Dartmouth researchers will collect snow from the surface of sea ice, from freely blowing snow and in sea-ice cores from Cape Byrd, Ross Sea. 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| Dataset Title/Abstract/Map | NSF Award(s) | Date Created | PIs / Scientists | Project Links | Abstract | Bounds Geometry | Geometry | Selected | Visible |
|---|---|---|---|---|---|---|---|---|---|
|
Egg membrane and chick feather THg concentration and stable isotope composition
|
0739575 |
2021-06-30 | McKenzie, Ashley |
Stable Isotope Analyses of Pygoscelid Penguin remains from Active and Abandoned Colonies in Antarctica |
Total mercury concentrations and corrected stable isotope signatures quantified in Adélie Penguin eggshell membrane and feathers recovered from the breast of deceased fledglings. Samples were collected in the austral summer of 2013/2014 in the northern Antarctic Peninsula region. | ["POLYGON((-57.3 -63.3,-57.22 -63.3,-57.14 -63.3,-57.06 -63.3,-56.98 -63.3,-56.9 -63.3,-56.82 -63.3,-56.74 -63.3,-56.66 -63.3,-56.58 -63.3,-56.5 -63.3,-56.5 -63.4,-56.5 -63.5,-56.5 -63.6,-56.5 -63.7,-56.5 -63.8,-56.5 -63.9,-56.5 -64,-56.5 -64.1,-56.5 -64.2,-56.5 -64.3,-56.58 -64.3,-56.66 -64.3,-56.74 -64.3,-56.82 -64.3,-56.9 -64.3,-56.98 -64.3,-57.06 -64.3,-57.14 -64.3,-57.22 -64.3,-57.3 -64.3,-57.3 -64.2,-57.3 -64.1,-57.3 -64,-57.3 -63.9,-57.3 -63.8,-57.3 -63.7,-57.3 -63.6,-57.3 -63.5,-57.3 -63.4,-57.3 -63.3))"] | ["POINT(-56.9 -63.8)"] | false | false |
|
16S rRNA gene libraries of krill gut microbial communities
|
1543412 |
2019-03-31 | Reinfelder, John |
Methylmercury in Antarctic Krill Microbiomes |
This dataset includes 16S rRNA gene libraries produced from DNA extracted from pooled digestive tracts of Antarctic krill (Euphausia superba) collected in coastal waters west of the Antarctic Peninsula in 2014. | ["POLYGON((-69.9043 -65.8708,-69.74203 -65.8708,-69.57976 -65.8708,-69.41749 -65.8708,-69.25522 -65.8708,-69.09295 -65.8708,-68.93068 -65.8708,-68.76841 -65.8708,-68.60614 -65.8708,-68.44387 -65.8708,-68.2816 -65.8708,-68.2816 -66.05698,-68.2816 -66.24316,-68.2816 -66.42934,-68.2816 -66.61552,-68.2816 -66.8017,-68.2816 -66.98788,-68.2816 -67.17406,-68.2816 -67.36024,-68.2816 -67.54642,-68.2816 -67.7326,-68.44387 -67.7326,-68.60614 -67.7326,-68.76841 -67.7326,-68.93068 -67.7326,-69.09295 -67.7326,-69.25522 -67.7326,-69.41749 -67.7326,-69.57976 -67.7326,-69.74203 -67.7326,-69.9043 -67.7326,-69.9043 -67.54642,-69.9043 -67.36024,-69.9043 -67.17406,-69.9043 -66.98788,-69.9043 -66.8017,-69.9043 -66.61552,-69.9043 -66.42934,-69.9043 -66.24316,-69.9043 -66.05698,-69.9043 -65.8708))"] | ["POINT(-69.09295 -66.8017)"] | false | false |
|
Bromide in Snow in the Sea Ice Zone
|
1043145 |
2016-01-01 | Obbard, Rachel |
Bromide in Snow in the Sea Ice Zone |
A range of chemical and microphysical pathways in polar latitudes, including spring time (tropospheric) ozone depletion, oxidative pathways for mercury, and cloud condensation nuclei (CCN) production leading to changes in the cloud cover and attendant surface energy budgets, have been invoked as being dependent upon the emission of halogen gases formed in sea-ice. The prospects for climate warming induced reductions in sea ice extent causing alteration of these incompletely known surface-atmospheric feedbacks and interactions requires confirmation of mechanistic details in both laboratory studies and field campaigns. One such mechanistic question is how bromine (BrO and Br) enriched snow migrates or is formed through processes in sea-ice, prior to its subsequent mobilization as an aerosol fraction into the atmosphere by strong winds. Once aloft, it may react with ozone and other atmospheric species. Dartmouth researchers will collect snow from the surface of sea ice, from freely blowing snow and in sea-ice cores from Cape Byrd, Ross Sea. A range of spectroscopic, microanalytic and and microstructural approaches will be subsequently used to determine the Br distribution gradients through sea-ice, in order to shed light on how sea-ice first forms and then releases bromine species into the polar atmospheric boundary layer. | ["POLYGON((164.1005 -77.1188,164.36443 -77.1188,164.62836 -77.1188,164.89229 -77.1188,165.15622 -77.1188,165.42015 -77.1188,165.68408 -77.1188,165.94801 -77.1188,166.21194 -77.1188,166.47587 -77.1188,166.7398 -77.1188,166.7398 -77.19337,166.7398 -77.26794,166.7398 -77.34251,166.7398 -77.41708,166.7398 -77.49165,166.7398 -77.56622,166.7398 -77.64079,166.7398 -77.71536,166.7398 -77.78993,166.7398 -77.8645,166.47587 -77.8645,166.21194 -77.8645,165.94801 -77.8645,165.68408 -77.8645,165.42015 -77.8645,165.15622 -77.8645,164.89229 -77.8645,164.62836 -77.8645,164.36443 -77.8645,164.1005 -77.8645,164.1005 -77.78993,164.1005 -77.71536,164.1005 -77.64079,164.1005 -77.56622,164.1005 -77.49165,164.1005 -77.41708,164.1005 -77.34251,164.1005 -77.26794,164.1005 -77.19337,164.1005 -77.1188))"] | ["POINT(165.42015 -77.49165)"] | false | false |
