Origination of the modern-style diversity gradient 15 million years ago

The latitudinal diversity gradient (LDG) is a prevalent feature of modern ecosystems across diverse clades. Recognized for well over a century, the causal mechanisms for LDGs remain disputed, in part because numerous putative drivers simultaneously covary with latitude. The past provides the opportu...

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Main Authors: Fenton, IS, Aze, T, Farnsworth, A, Valdes, P, Saupe, EE
Format: Article in Journal/Newspaper
Language:unknown
Published: Nature Research 2023
Subjects:
Online Access:https://eprints.whiterose.ac.uk/196724/
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spelling ftleedsuniv:oai:eprints.whiterose.ac.uk:196724 2023-05-15T18:00:25+02:00 Origination of the modern-style diversity gradient 15 million years ago Fenton, IS Aze, T Farnsworth, A Valdes, P Saupe, EE 2023-02-23 https://eprints.whiterose.ac.uk/196724/ unknown Nature Research Fenton, IS, Aze, T orcid.org/0000-0002-4201-7105 , Farnsworth, A et al. (2 more authors) (2023) Origination of the modern-style diversity gradient 15 million years ago. Nature, 614 (7949). pp. 708-712. ISSN 0028-0836 Article NonPeerReviewed 2023 ftleedsuniv 2023-03-23T23:17:15Z The latitudinal diversity gradient (LDG) is a prevalent feature of modern ecosystems across diverse clades. Recognized for well over a century, the causal mechanisms for LDGs remain disputed, in part because numerous putative drivers simultaneously covary with latitude. The past provides the opportunity to disentangle LDG mechanisms because the relationships among biodiversity, latitude and possible causal factors have varied over time. Here we quantify the emergence of the LDG in planktonic foraminifera at high spatiotemporal resolution over the past 40 million years, finding that a modern-style gradient arose only 15 million years ago. Spatial and temporal models suggest that LDGs for planktonic foraminifera may be controlled by the physical structure of the water column. Steepening of the latitudinal temperature gradient over 15 million years ago, associated with an increased vertical temperature gradient at low latitudes, may have enhanced niche partitioning and provided more opportunities for speciation at low latitudes. Supporting this hypothesis, we find that higher rates of low-latitude speciation steepened the diversity gradient, consistent with spatiotemporal patterns of depth partitioning by planktonic foraminifera. Extirpation of species from high latitudes also strengthened the LDG, but this effect tended to be weaker than speciation. Our results provide a step change in understanding the evolution of marine LDGs over long timescales. Article in Journal/Newspaper Planktonic foraminifera White Rose Research Online (Universities of Leeds, Sheffield & York)
institution Open Polar
collection White Rose Research Online (Universities of Leeds, Sheffield & York)
op_collection_id ftleedsuniv
language unknown
description The latitudinal diversity gradient (LDG) is a prevalent feature of modern ecosystems across diverse clades. Recognized for well over a century, the causal mechanisms for LDGs remain disputed, in part because numerous putative drivers simultaneously covary with latitude. The past provides the opportunity to disentangle LDG mechanisms because the relationships among biodiversity, latitude and possible causal factors have varied over time. Here we quantify the emergence of the LDG in planktonic foraminifera at high spatiotemporal resolution over the past 40 million years, finding that a modern-style gradient arose only 15 million years ago. Spatial and temporal models suggest that LDGs for planktonic foraminifera may be controlled by the physical structure of the water column. Steepening of the latitudinal temperature gradient over 15 million years ago, associated with an increased vertical temperature gradient at low latitudes, may have enhanced niche partitioning and provided more opportunities for speciation at low latitudes. Supporting this hypothesis, we find that higher rates of low-latitude speciation steepened the diversity gradient, consistent with spatiotemporal patterns of depth partitioning by planktonic foraminifera. Extirpation of species from high latitudes also strengthened the LDG, but this effect tended to be weaker than speciation. Our results provide a step change in understanding the evolution of marine LDGs over long timescales.
format Article in Journal/Newspaper
author Fenton, IS
Aze, T
Farnsworth, A
Valdes, P
Saupe, EE
spellingShingle Fenton, IS
Aze, T
Farnsworth, A
Valdes, P
Saupe, EE
Origination of the modern-style diversity gradient 15 million years ago
author_facet Fenton, IS
Aze, T
Farnsworth, A
Valdes, P
Saupe, EE
author_sort Fenton, IS
title Origination of the modern-style diversity gradient 15 million years ago
title_short Origination of the modern-style diversity gradient 15 million years ago
title_full Origination of the modern-style diversity gradient 15 million years ago
title_fullStr Origination of the modern-style diversity gradient 15 million years ago
title_full_unstemmed Origination of the modern-style diversity gradient 15 million years ago
title_sort origination of the modern-style diversity gradient 15 million years ago
publisher Nature Research
publishDate 2023
url https://eprints.whiterose.ac.uk/196724/
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_relation Fenton, IS, Aze, T orcid.org/0000-0002-4201-7105 , Farnsworth, A et al. (2 more authors) (2023) Origination of the modern-style diversity gradient 15 million years ago. Nature, 614 (7949). pp. 708-712. ISSN 0028-0836
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