The Effect of Oxygen Deprivation on Inorganic Nitrogen Uptake in an Antarctic Macrolichen
Abstract Snow meltwater containing 36 ng ml −1 NO 3 − −N (raised here to between 95–101 ng ml −1 NO 3 − −N) and 112 ng ml −1 NH 4 + −N was sprayed onto illuminated Usnea sphacelata at 2°C in a 2−1 capacity transparent perspex chamber force-ventilated with either air or O 2 − (and CO 2 − ) free N 2 ....
| Published in: | The Lichenologist |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Cambridge University Press (CUP)
1996
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| Online Access: | http://dx.doi.org/10.1006/lich.1996.0032 http://api.elsevier.com/content/article/PII:S0024-2829(96)90032-8?httpAccept=text/xml http://api.elsevier.com/content/article/PII:S0024-2829(96)90032-8?httpAccept=text/plain https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002428299600045X |
| Summary: | Abstract Snow meltwater containing 36 ng ml −1 NO 3 − −N (raised here to between 95–101 ng ml −1 NO 3 − −N) and 112 ng ml −1 NH 4 + −N was sprayed onto illuminated Usnea sphacelata at 2°C in a 2−1 capacity transparent perspex chamber force-ventilated with either air or O 2 − (and CO 2 − ) free N 2 . The NO 3 -concentration in meltwater recirculated through a layer of U. sphacelata fell to c. 8 ng ml −1 after 1.25 h. Although the pattern of decline was broadly comparable in both air and N 2 , the initial rate of decline was lower in N 2 . When undepleted meltwater was continuously sprayed onto the lichen and the effluent collected for analysis, the lichen was found to retain 55% of the wet deposited NO 3 − in air but only 27% under N 2 . Up to 90%) of NH 4 + supplied in a continuous spray of meltwater was retained by the lichen but this was affected little by O 2 and CO 2 deprivation. |
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