Testing the deep‐sea glacial disturbance hypothesis as a cause of low, present‐day Norwegian Sea diversity and resulting steep latitudinal diversity gradient, using fossil records.

MLA

Jöst, Anna B., et al. “Testing the Deep‐sea Glacial Disturbance Hypothesis as a Cause of Low, Present‐day Norwegian Sea Diversity and Resulting Steep Latitudinal Diversity Gradient, Using Fossil Records.” Global Ecology & Biogeography, vol. 33, no. 7, July 2024, pp. 1–18. EBSCOhost, https://doi.org/10.1111/geb.13844.

APA

Jöst, A. B., Huang, H. M., Hong, Y., Wei, C., Bauch, H. A., Thibodeau, B., Cronin, T. M., Okahashi, H., & Yasuhara, M. (2024). Testing the deep‐sea glacial disturbance hypothesis as a cause of low, present‐day Norwegian Sea diversity and resulting steep latitudinal diversity gradient, using fossil records. Global Ecology & Biogeography, 33(7), 1–18. https://doi.org/10.1111/geb.13844

Chicago

Jöst, Anna B., Huai‐Hsuan M. Huang, Yuanyuan Hong, Chih‐Lin Wei, Henning A. Bauch, Benoit Thibodeau, Thomas M. Cronin, Hisayo Okahashi, and Moriaki Yasuhara. 2024. “Testing the Deep‐sea Glacial Disturbance Hypothesis as a Cause of Low, Present‐day Norwegian Sea Diversity and Resulting Steep Latitudinal Diversity Gradient, Using Fossil Records.” Global Ecology & Biogeography 33 (7): 1–18. doi:10.1111/geb.13844.