Figure - PMC

Skip to main content

An official website of the United States government

Here's how you know

Here's how you know

Official websites use .gov
A .gov website belongs to an official government organization in the United States.

Secure .gov websites use HTTPS
A lock ( ) or https:// means you've safely connected to the .gov website. Share sensitive information only on official, secure websites.

View full-text article in PMC

. 2022 Jul 13;607(7919):507–511. doi: 10.1038/s41586-022-04932-6

Search in PMC
Search in PubMed
View in NLM Catalog
Add to search

© The Author(s), under exclusive licence to Springer Nature Limited 2022

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

PMC Copyright notice

Extended Data Fig. 3 — a-c, Global diversity dynamics reconstructed by the exponential diversification model using two alternative palaeogeographic models^33,35. d-f, Effect of changing the sea level +/− 100 m compared to the original palaeo-digital elevation model of Scotese and Wright³³. g-i, Effect of changing the mean ocean phosphate concentration (x2 and x0.5 with respect to present day concentrations, i.e., default scenario). All simulations were run for each of the three mass extinction patterns, that is, Sepkoski²⁰ (a, d, g), Alroy²¹ (b, e, h), and Zaffos et al²². (c, f, i).