Evidence map›Paper›PMID 34237071›Full record

ArticlePloS one2021

Relationships between climate and phylogenetic community structure of fossil pollen assemblages are not constant during the last deglaciation.

Kavya Pradhan, Diego Nieto-Lugilde, Matthew C Fitzpatrick

Abstract read
In one paragraph

Article in PloS one, 2021. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

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0citing papers in PubMed
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1 · What the graph read from it

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The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

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3 · Its place in the literature

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4 · The record

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5 · Who and what money

Authors and funding

3 authors.

Kavya PradhanUniversity of Maryland Center for Environmental Science, Appalachian Lab, Frostburg, Maryland, United States of America.
Diego Nieto-LugildeUniversity of Maryland Center for Environmental Science, Appalachian Lab, Frostburg, Maryland, United States of America.ORCID 0000-0003-4135-2881
Matthew C FitzpatrickUniversity of Maryland Center for Environmental Science, Appalachian Lab, Frostburg, Maryland, United States of America.ORCID 0000-0003-1911-8407

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Disentangling the influence of environmental drivers on community assembly is important to understand how multiple processes influence biodiversity patterns and can inform understanding of ecological responses to climate change. Phylogenetic Community Structure (PCS) is increasingly used in community assembly studies to incorporate evolutionary perspectives and as a proxy for trait (dis)similarity within communities. Studies often assume a stationary relationship between PCS and climate, though few studies have tested this assumption over long time periods with concurrent community data. We estimated two PCS metrics-Nearest Taxon Index (NTI) and Net Relatedness index (NRI)-of fossil pollen assemblages of Angiosperms in eastern North America over the last 21 ka BP at 1 ka intervals. We analyzed spatiotemporal relationships between PCS and seven climate variables, evaluated the potential impact of deglaciation on PCS, and tested for the stability of climate-PCS relationships through time. The broad scale geographic patterns of PCS remained largely stable across time, with overdispersion tending to be most prominent in the central and southern portion of the study area and clustering dominating at the longitudinal extremes. Most importantly, we found that significant relationships between climate variables and PCS (slope) were not constant as climate changed during the last deglaciation and new ice-free regions were colonized. We also found weak, but significant relationships between both PCS metrics (i.e., NTI and NRI) and climate and time-since-deglaciation that also varied through time. Overall, our results suggest that (1) PCS of fossil Angiosperm assemblages during the last 21ka BP have had largely constant spatial patterns, but (2) temporal variability in the relationships between PCS and climate brings into question their usefulness in predictive modeling of community assembly.

Indexed as

Climate ChangeFossilsPhylogenyPollenBiodiversityClimateMagnoliopsidaNorth America

Identifiers

PMID34237071
PMCPMC8266067

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Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.