Citation
Yasuhara, Moriaki, et al. "Past and Future Decline of Tropical Pelagic Biodiversity." Proceedings of the National Academy of Sciences of the United States of America, vol. 117, no. 23, 2020, pp. 12891-12896.
Yasuhara M, Wei CL, Kucera M, et al. Past and future decline of tropical pelagic biodiversity. Proc Natl Acad Sci U S A. 2020;117(23):12891-12896.
Yasuhara, M., Wei, C. L., Kucera, M., Costello, M. J., Tittensor, D. P., Kiessling, W., Bonebrake, T. C., Tabor, C. R., Feng, R., Baselga, A., Kretschmer, K., Kusumoto, B., & Kubota, Y. (2020). Past and future decline of tropical pelagic biodiversity. Proceedings of the National Academy of Sciences of the United States of America, 117(23), 12891-12896. https://doi.org/10.1073/pnas.1916923117
Yasuhara M, et al. Past and Future Decline of Tropical Pelagic Biodiversity. Proc Natl Acad Sci U S A. 2020 06 9;117(23):12891-12896. PubMed PMID: 32457146.
TY - JOUR
T1 - Past and future decline of tropical pelagic biodiversity.
AU - Yasuhara,Moriaki,
AU - Wei,Chih-Lin,
AU - Kucera,Michal,
AU - Costello,Mark J,
AU - Tittensor,Derek P,
AU - Kiessling,Wolfgang,
AU - Bonebrake,Timothy C,
AU - Tabor,Clay R,
AU - Feng,Ran,
AU - Baselga,Andrés,
AU - Kretschmer,Kerstin,
AU - Kusumoto,Buntarou,
AU - Kubota,Yasuhiro,
Y1 - 2020/05/26/
PY - 2020/5/28/pubmed
PY - 2020/8/22/medline
PY - 2020/5/28/entrez
KW - Last Glacial Maximum
KW - climate change
KW - latitudinal diversity gradients
KW - planktonic foraminifera
KW - temperature
SP - 12891
EP - 12896
JF - Proceedings of the National Academy of Sciences of the United States of America
JO - Proc Natl Acad Sci U S A
VL - 117
IS - 23
N2 - A major research question concerning global pelagic biodiversity remains unanswered: when did the apparent tropical biodiversity depression (i.e., bimodality of latitudinal diversity gradient [LDG]) begin? The bimodal LDG may be a consequence of recent ocean warming or of deep-time evolutionary speciation and extinction processes. Using rich fossil datasets of planktonic foraminifers, we show here that a unimodal (or only weakly bimodal) diversity gradient, with a plateau in the tropics, occurred during the last ice age and has since then developed into a bimodal gradient through species distribution shifts driven by postglacial ocean warming. The bimodal LDG likely emerged before the Anthropocene and industrialization, and perhaps ∼15,000 y ago, indicating a strong environmental control of tropical diversity even before the start of anthropogenic warming. However, our model projections suggest that future anthropogenic warming further diminishes tropical pelagic diversity to a level not seen in millions of years.
SN - 1091-6490
UR - https://www.unboundmedicine.com/medline/citation/32457146/Past_and_future_decline_of_tropical_pelagic_biodiversity_
L2 - http://www.pnas.org/cgi/pmidlookup?view=long&pmid=32457146
DB - PRIME
DP - Unbound Medicine
ER -