The Toarcian oceanic anoxic event disrupted terrestrial ecosystems as well as the marine realm, according to analyses of microfossils derived from land plants. Changes in diversity and composition were initially more rapid in terrestrial ecosystems.
This is a preview of subscription content, access via your institution
Access options
Access Nature and 54 other Nature Portfolio journals
Get Nature+, our best-value online-access subscription
$29.99 / 30 days
cancel any time
Subscribe to this journal
Receive 12 print issues and online access
$259.00 per year
only $21.58 per issue
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
References
Slater, S. M., Twitchett, R. J., Danise, S. & Vajda, V. Nat. Geosci. https://doi.org/10.1038/s41561-019-0349-z (2019).
Mander, L. & Punyasena, S. W. Int. J. Plant Sci. 175, 931–945 (2014).
Haworth, M. & McElwain, J. C. Palaeogeog. Palaeoclim. Palaeoecol. 262, 79–90 (2008).
Mander, L. & Punyasena, S. W. Methods in Paleoecology 215–234 (Springer, 2018).
McElwain, J. C. & Steinthorsdottir, M. Plant Physiol. 174, 650–664 (2017).
Wilson, J. P. et al. New Phyt. 215, 1333–1353 (2017).
Percival, L. M. et al. Am. J. Sci. 318, 799–860 (2018).
Patra, M. & Sharma, A. Bot. Rev. 66, 379–422 (2000).
Otto, S. P. Cell 131, 452–462 (2007).
Author information
Authors and Affiliations
Corresponding authors
Rights and permissions
About this article
Cite this article
Mander, L., McElwain, J.C. Toarcian land vegetation loss. Nat. Geosci. 12, 405–406 (2019). https://doi.org/10.1038/s41561-019-0366-y
Published:
Issue Date:
DOI: https://doi.org/10.1038/s41561-019-0366-y