Editorial preface to special issue: Biocalcifier resilience and response during Phanerozoic global climate changes

Through the Phanerozoic, the Earth has experienced several environmental disturbances characterised by varied tempos and modes of ecosystem resilience and response, and organisms that secrete calcium carbonate skeletons (calcifiers) are especially vulnerable. These events have occasionally reached ecological tipping-points that triggering permanent changes in the abundance, biodiversity, ecological range and biomineralization processes of marine calcifiers. Today benthic and planktic marine calcifiers are the most impacted by these global perturbations; therefore, it is important to understand how calcifiers responded to global climatic and environmental perturbations in the recent and distant past in order to understand future resilience. This Virtual Special Issue (VSI), entitled Biocalcifier resilience and response during Phanerozoic global climate changes , comprises 17 papers that document the adaptative response of marine calcifiers to global stresses, dealing with examples from the geological record and from modern biota. Papers span from the Permian to the Recent, and consider pelagic organisms, benthic organisms, and integrated studies of pelagic and benthic ecosystems. Some of the main findings are as follows: (1) Planktic communities show a greater ecological resilience than benthic ones; (2) Most perturbations trigger ecological shifts rather than complete biotic turnovers, with the exceptions being the end-Permian and Triassic-Jurassic boundary crises which led to ecosystem collapse and extinctions; and (3) Benthic ecosystems often respond through reorganization into new community assemblages. It is important to emphasise that each event represents a unique case study, where different duration and environmental stressors are key factors in determining organismal survival and ecosystem restructuring. The papers presented will be of help in detecting the most vulnerable and/or highly tolerant and resilient taxa in order to quantify the most common responses and adaptive strategies to current climate changes. • We document the adaptative (or not) response of biocalcifiers to global stresses. • Planktic communities showed a greater ecological resilience than benthic ones. • Benthic ecosystems responded through reorganization into new community assemblages. • Each event is a unique case, with different duration and environmental stressors.

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Journal
Palaeogeography Palaeoclimatology Palaeoecology
Published
2025-06-22
DOI
https://doi.org/10.1016/j.palaeo.2025.113106
Primary Topic
Ocean Acidification Effects and Responses
Type
article
Field-Weighted Citation Impact
0.00

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article

Editorial preface to special issue: Biocalcifier resilience and response during Phanerozoic global climate changes

Gaia Crippa, Cinzia Bottini
Palaeogeography Palaeoclimatology Palaeoecology
Ocean Acidification Effects and Responses
article

Editorial preface to special issue: Biocalcifier resilience and response during Phanerozoic global climate changes

Gaia Crippa, Cinzia Bottini
article en

Abstract

Through the Phanerozoic, the Earth has experienced several environmental disturbances characterised by varied tempos and modes of ecosystem resilience and response, and organisms that secrete calcium carbonate skeletons (calcifiers) are especially vulnerable. These events have occasionally reached ecological tipping-points that triggering permanent changes in the abundance, biodiversity, ecological range and biomineralization processes of marine calcifiers. Today benthic and planktic marine calcifiers are the most impacted by these global perturbations; therefore, it is important to understand how calcifiers responded to global climatic and environmental perturbations in the recent and distant past in order to understand future resilience. This Virtual Special Issue (VSI), entitled Biocalcifier resilience and response during Phanerozoic global climate changes , comprises 17 papers that document the adaptative response of marine calcifiers to global stresses, dealing with examples from the geological record and from modern biota. Papers span from the Permian to the Recent, and consider pelagic organisms, benthic organisms, and integrated studies of pelagic and benthic ecosystems. Some of the main findings are as follows: (1) Planktic communities show a greater ecological resilience than benthic ones; (2) Most perturbations trigger ecological shifts rather than complete biotic turnovers, with the exceptions being the end-Permian and Triassic-Jurassic boundary crises which led to ecosystem collapse and extinctions; and (3) Benthic ecosystems often respond through reorganization into new community assemblages. It is important to emphasise that each event represents a unique case study, where different duration and environmental stressors are key factors in determining organismal survival and ecosystem restructuring. The papers presented will be of help in detecting the most vulnerable and/or highly tolerant and resilient taxa in order to quantify the most common responses and adaptive strategies to current climate changes. • We document the adaptative (or not) response of biocalcifiers to global stresses. • Planktic communities showed a greater ecological resilience than benthic ones. • Benthic ecosystems responded through reorganization into new community assemblages. • Each event is a unique case, with different duration and environmental stressors.

Palaeogeography Palaeoclimatology PalaeoecologyVol. 675
University of Milan (IT)
European Commission, Ministero dell’Istruzione, dell’Università e della Ricerca
Climate action
Openalex Percentile: Top 84%
Ocean Acidification Effects and Responses
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