Figures & data
Figure 1. Location of the cryoconite holes used for in situ incubations, measurements, and sampling on the Greenland Ice Sheet at Point 660 (67.06000, −50.17000) on the ice sheet margins and at camp Black and Bloom (67.07482, −49.3586). Map is acquired as an image from Modis Satellite
![Figure 1. Location of the cryoconite holes used for in situ incubations, measurements, and sampling on the Greenland Ice Sheet at Point 660 (67.06000, −50.17000) on the ice sheet margins and at camp Black and Bloom (67.07482, −49.3586). Map is acquired as an image from Modis Satellite](/cms/asset/7d119203-5eba-4f83-b569-270d861a94e7/uaar_a_1420859_f0001_oc.jpg)
Figure 2. A custom-made incubation vessel, manufactured using 3D printing with sampling ports on the sides to enable measurement of oxygen, pH, and microbial community changes with depth
![Figure 2. A custom-made incubation vessel, manufactured using 3D printing with sampling ports on the sides to enable measurement of oxygen, pH, and microbial community changes with depth](/cms/asset/b609aca9-0add-4643-bf3d-11e6b533fd96/uaar_a_1420859_f0002_oc.jpg)
Figure 3. Microoptode positioned with a manual micromanipulator for in situ measurement of an oxygen profile in a cryoconite hole on the surface of the Greenland Ice Sheet
![Figure 3. Microoptode positioned with a manual micromanipulator for in situ measurement of an oxygen profile in a cryoconite hole on the surface of the Greenland Ice Sheet](/cms/asset/08b08960-9bb5-41a3-b96d-3ca53ab0fc25/uaar_a_1420859_f0003_oc.jpg)
Figure 4. In situ oxygen profiles of varying morphologies of cryoconite sediments measured with a microoptode in a variety of cryoconite sediment accumulations. Note the different vertical scale on the graphs. (A) A classic cryoconite hole, with a regular, semicircular shape. Water depth was approximately 11 cm and sediment depth was approximately 4 mm. (B) Cryoconite sediment in an irregularly shaped hole, with a water depth of 1–7 cm and sediment depth of 1 cm. (C) A thick layer of cryoconite material (1.5 cm) without a layer of water
![Figure 4. In situ oxygen profiles of varying morphologies of cryoconite sediments measured with a microoptode in a variety of cryoconite sediment accumulations. Note the different vertical scale on the graphs. (A) A classic cryoconite hole, with a regular, semicircular shape. Water depth was approximately 11 cm and sediment depth was approximately 4 mm. (B) Cryoconite sediment in an irregularly shaped hole, with a water depth of 1–7 cm and sediment depth of 1 cm. (C) A thick layer of cryoconite material (1.5 cm) without a layer of water](/cms/asset/037d3390-473c-4c6d-a927-a9be5f037700/uaar_a_1420859_f0004_oc.jpg)
Figure 5. Oxygen profile measured using a microsensor within a 4 mm wide, spherical cryoconite granule
![Figure 5. Oxygen profile measured using a microsensor within a 4 mm wide, spherical cryoconite granule](/cms/asset/0c6c37a3-7aaf-44ca-88f1-bebc8408f774/uaar_a_1420859_f0005_b.gif)
Figure 6. Temporal development of a characteristic oxygen profile in 10 mm thick cryoconite sediment after perturbation
![Figure 6. Temporal development of a characteristic oxygen profile in 10 mm thick cryoconite sediment after perturbation](/cms/asset/cda9820a-2948-45f3-be3b-175baa0b8725/uaar_a_1420859_f0006_b.gif)
Figure 7. Oxygen profiles of twenty-day open and closed cryoconite field incubations with calculated NEP. Error bars show standard deviation of triplicate bottle measurements of oxygen and standard error of NEP calculations
![Figure 7. Oxygen profiles of twenty-day open and closed cryoconite field incubations with calculated NEP. Error bars show standard deviation of triplicate bottle measurements of oxygen and standard error of NEP calculations](/cms/asset/a45f16fe-66e7-4156-9bf9-b3b4db1c5fa2/uaar_a_1420859_f0007_b.gif)