Estuarine carbon export_Reithmaier et al._figshare.xlsx

This dataset forms the basis for the findings presented in Reithmaier, G. M., Maher, D. T., Holloway, C., Correa, R. E., &amp; Santos, I. R. (2024). Small wetland‐fringed estuaries deliver disproportionately large carbon loads to the ocean. <i>Limnology and Oceanography</i>.The dataset includes estuary name, season, date, latitude, longitude, salinity, pH, dissolved oxygen (DO), temperature, dissolved inorganic carbon (DIC), dissolved organic carbon (DOC), total alkalinity (TA), and pCO2. Out of the 713 samples collected during the 37 surveys, 307 represent original data while the remaining were published in different contexts. Partially published datasets were used in earlier greenhouse gas and carbon cycle investigations in Johnstone, Constant, and Fitzroy (Rosentreter et al. 2018); Caboolture (Adiyanti et al. 2016); Coffs, Boambee, Bonville, and Pine (Looman et al. 2019); Korogoro (Sadat-Noori et al. 2016); and Yarra (Santos et al. 2012).Rosentreter, J. A., D. Maher, D. Erler, R. Murray, and B. Eyre. 2018. Factors controlling seasonal CO₂ and CH₄ emissions in three tropical mangrove-dominated estuaries in Australia. Estuar. Coast. Shelf Sci. <b>215: </b>69-82. doi: 10.1016/j.ecss.2018.10.003Adiyanti, S., B. D. Eyre, D. T. Maher, I. Santos, L. Golsby-Smith, P. Mangion, and M. R. Hipsey. 2016. Stable isotopes reduce parameter uncertainty of an estuarine carbon cycling model. Environ. Model. Software <b>79: </b>233-255. doi: 10.1016/j.envsoft.2016.02.011Looman, A., I. R. Santos, D. R. Tait, J. Webb, C. Holloway, and D. T. Maher. 2019. Dissolved carbon, greenhouse gases, and δ¹³C dynamics in four estuaries across a land use gradient. Aquat. Sci. <b>81: </b>22. doi: 10.1007/s00027-018-0617-9Sadat-Noori, M., D. T. Maher, and I. R. Santos. 2016. Groundwater Discharge as a Source of Dissolved Carbon and Greenhouse Gases in a Subtropical Estuary. Estuaries and Coasts <b>39: </b>639-656. doi: 10.1007/s12237-015-0042-4Santos, I. R., P. L. Cook, L. Rogers, J. d. Weys, and B. D. Eyre. 2012a. The “salt wedge pump”: Convection‐driven pore‐water exchange as a source of dissolved organic and inorganic carbon and nitrogen to an estuary. Limnol. Oceanogr. <b>57: </b>1415-1426. doi: 10.4319/lo.2012.57.5.1415