Global subterranean estuaries modify groundwater nutrient loading to the ocean

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2024-05-16
Authors
Wilson, Stephanie J.
Moody, Amy
McKenzie, Tristan
Cardenas, M. Bayani
Luijendijk, Elco
Sawyer, Audrey H.
Wilson, Alicia
Michael, Holly A.
Xu, Bochao
Knee, Karen L.
Cho, Hyung-Mi
Weinstein, Yishai
Paytan, Adina
Moosdorf, Nils
Chen, Chen-Tung Aurthur
Beck, Melanie
Lopez, Cody
Murgulet, Dorina
Kim, Guebuem
Charette, Mathew A.
Waska, Hannelore
Ibanhez, J. Severino P.
Chaillou, Gwenaelle
Oehler, Till
Onodera, Shin-ichi
Saito, Mitsuyo
Rodellas, Valenti
Dimova, Natasha T.
Montiel, Daniel
Dulai, Henrietta
Richardson, Christina
Du, Jinzhou
Petermann, Eric
Chen, Xiaogang
Davis, Kay L.
Lamontagne, Sebastien
Sugimoto, Ryo
Wang, Guizhi
Li, Hailong
Torres, Americo I.
Demir, Cansu
Bristol, Emily
Connolly, Craig T.
McClelland, James W.
Silva, Brenno J.
Tait, Douglas
Kumar, Busala Siva Kiran
Viswanadham, Rongali
Sarma, V. V. S. S.
Silva-Filho, Emmanoel
Shiller, Alan M.
Lecher, Alanna
Tamborski, Joseph
Bokuniewicz, Henry J.
Rocha, Carlos
Reckhardt, Anja
Bottcher, Michael Ernst
Jiang, Shan
Stieglitz, Thomas
Gbewezoun, Houegnon Geraud Vinel
Charbonnier, Celine
Anschutz, Pierre
Hernandez-Terrones, Laura M.
Babu, Suresh
Szymczycha, Beata
Sadat-Noori, Mahmood
Niencheski, Felipe
Null, Kimberly
Tobias, Craig
Song, Bongkeun
Anderson, Iris C.
Santos, Isaac R.
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DOI
10.1002/lol2.10390
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Abstract
Terrestrial groundwater travels through subterranean estuaries before reaching the sea. Groundwater-derived nutrients drive coastal water quality, primary production, and eutrophication. We determined how dissolved inorganic nitrogen (DIN), dissolved inorganic phosphorus (DIP), and dissolved organic nitrogen (DON) are transformed within subterranean estuaries and estimated submarine groundwater discharge (SGD) nutrient loads compiling > 10,000 groundwater samples from 216 sites worldwide. Nutrients exhibited complex, nonconservative behavior in subterranean estuaries. Fresh groundwater DIN and DIP are usually produced, and DON is consumed during transport. Median total SGD (saline and fresh) fluxes globally were 5.4, 2.6, and 0.18 Tmol yr−1 for DIN, DON, and DIP, respectively. Despite large natural variability, total SGD fluxes likely exceed global riverine nutrient export. Fresh SGD is a small source of new nutrients, but saline SGD is an important source of mostly recycled nutrients. Nutrients exported via SGD via subterranean estuaries are critical to coastal biogeochemistry and a significant nutrient source to the oceans.
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© The Author(s), 2024. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Wilson, S., Moody, A., McKenzie, T., Cardenas, M., Luijendijk, E., Sawyer, A., Wilson, A., Michael, H., Xu, B., Knee, K., Cho, H., Weinstein, Y., Paytan, A., Moosdorf, N., Chen, C., Beck, M., Lopez, C., Murgulet, D., Kim, G., Charette, M. A., Waska, H., Ibanhez, J. S. P., Chaillou, G., Oehler, T., Onodera, S., Saito, M., Rodellas, V., Dimova, N., Montiel, D., Dulai, H., Richardson, C., Du, J., Petermann, E., Chen, X., Davis, K. L., Lamontagne, S., Sugimoto, R., Wang, G., Li, H., Torres, A. I., Demir, C., Bristol, E., Connolly, C. T., McClelland, J. W., Silva, B. J., Tait, D., Kumar, BSK, Viswanadham, R., Sarma, VVSS, Silva-Filho, E., Shiller, A., Lecher, A., Tamborski, J., Bokuniewicz, H., Rocha, C., Reckhart, A., Bottcher, M. E., Jiang, S., Stieglitz, T., Gbewezoun, H. G. V., Charbonnier, C., Anschutz, P., Hernandez-Terrones, L. M., Babu, S., Szymczycha, B., Sadat-Noori, M., Niencheski, F., Null, K., Tobias, C., Song, B., Anderson, I. C., & Santos, I. (2024). Global subterranean estuaries modify groundwater nutrient loading to the ocean. Limnology and Oceanography Letters, https://doi.org/10.1002/lol2.10390.
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Wilson, S., Moody, A., McKenzie, T., Cardenas, M., Luijendijk, E., Sawyer, A., Wilson, A., Michael, H., Xu, B., Knee, K., Cho, H., Weinstein, Y., Paytan, A., Moosdorf, N., Chen, C., Beck, M., Lopez, C., Murgulet, D., Kim, G., Charette, M. A., Waska, H., Ibanhez, J. S. P., Chaillou, G., Oehler, T., Onodera, S., Saito, M., Rodellas, V., Dimova, N., Montiel, D., Dulai, H., Richardson, C., Du, J., Petermann, E., Chen, X., Davis, K. L., Lamontagne, S., Sugimoto, R., Wang, G., Li, H., Torres, A. I., Demir, C., Bristol, E., Connolly, C. T., McClelland, J. W., Silva, B. J., Tait, D., Kumar, BSK, Viswanadham, R., Sarma, VVSS, Silva-Filho, E., Shiller, A., Lecher, A., Tamborski, J., Bokuniewicz, H., Rocha, C., Reckhart, A., Bottcher, M. E., Jiang, S., Stieglitz, T., Gbewezoun, H. G. V., Charbonnier, C., Anschutz, P., Hernandez-Terrones, L. M., Babu, S., Szymczycha, B., Sadat-Noori, M., Niencheski, F., Null, K., Tobias, C., Song, B., Anderson, I. C., & Santos, I. (2024). Global subterranean estuaries modify groundwater nutrient loading to the ocean. Limnology and Oceanography Letters.
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