Effects of Field Simulated Marine Heatwaves on Sedimentary Organic Matter Quantity, Biochemical Composition, and Degradation Rates

Since rising temperature (T) will enhance biochemical reactions and coastal marine sediments are hotspots of carbon cycling, marine heatwaves’ (MHWs’) intensification caused by climate change will affect coastal biogeochemistry. We investigated the effects of MHWs on sediment organic matter (OM) in...

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Main Authors: Santina Soru, Patrizia Stipcich, Giulia Ceccherelli, Claudia Ennas, Davide Moccia, Antonio Pusceddu
Format: Article
Language:English
Published: MDPI AG 2022-05-01
Series:Biology
Subjects:
Online Access:https://www.mdpi.com/2079-7737/11/6/841
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author Santina Soru
Patrizia Stipcich
Giulia Ceccherelli
Claudia Ennas
Davide Moccia
Antonio Pusceddu
author_facet Santina Soru
Patrizia Stipcich
Giulia Ceccherelli
Claudia Ennas
Davide Moccia
Antonio Pusceddu
author_sort Santina Soru
collection DOAJ
description Since rising temperature (T) will enhance biochemical reactions and coastal marine sediments are hotspots of carbon cycling, marine heatwaves’ (MHWs’) intensification caused by climate change will affect coastal biogeochemistry. We investigated the effects of MHWs on sediment organic matter (OM) in a nearshore locality (NW Sardinia, Mediterranean Sea) receiving an artificial warm water plume generating T anomalies of 1.5–5.0 °C. Sediments were collected before and after 3 and 11 weeks from the initial plume release. Both MHWs influenced sedimentary OM quantity, composition, and degradation rates, with major effects associated with the highest T anomaly after 3 weeks. Both MHWs enhanced sedimentary OM contents, with larger effects associated with the highest T anomaly. Phytopigment contents increased in the short term but dropped to initial levels after 11 weeks, suggesting the occurrence of thermal adaptation or stress of microphytobenthos. In the longer term we observed a decrease in the nutritional quality of OM and a slowdown of its turnover mediated by extracellular enzymes, suggestive of a decreased ecosystem functioning. We anticipate that intensification of MHWs will affect benthic communities not only through direct effects on species tolerance but also by altering benthic biogeochemistry and the efficiency of energy transfer towards higher trophic levels.
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spelling doaj.art-6b2a8221f40c4980a2602644eff5a2242023-11-23T15:39:10ZengMDPI AGBiology2079-77372022-05-0111684110.3390/biology11060841Effects of Field Simulated Marine Heatwaves on Sedimentary Organic Matter Quantity, Biochemical Composition, and Degradation RatesSantina Soru0Patrizia Stipcich1Giulia Ceccherelli2Claudia Ennas3Davide Moccia4Antonio Pusceddu5Dipartimento di Scienze della Vita e dell’Ambiente, Università degli Studi di Cagliari, Via T. Fiorelli, 1, 09126 Cagliari, ItalyDipartimento di Architettura, Design e Urbanistica, Università degli Studi di Sassari, Via Piandanna 4, 07100 Sassari, ItalyDipartimento di Scienze Chimiche, Fisiche, Matematiche e Naturali, Università degli Studi di Sassari, Via Piandanna 4, 07100 Sassari, ItalyDipartimento di Scienze della Vita e dell’Ambiente, Università degli Studi di Cagliari, Via T. Fiorelli, 1, 09126 Cagliari, ItalyDipartimento di Scienze della Vita e dell’Ambiente, Università degli Studi di Cagliari, Via T. Fiorelli, 1, 09126 Cagliari, ItalyDipartimento di Scienze della Vita e dell’Ambiente, Università degli Studi di Cagliari, Via T. Fiorelli, 1, 09126 Cagliari, ItalySince rising temperature (T) will enhance biochemical reactions and coastal marine sediments are hotspots of carbon cycling, marine heatwaves’ (MHWs’) intensification caused by climate change will affect coastal biogeochemistry. We investigated the effects of MHWs on sediment organic matter (OM) in a nearshore locality (NW Sardinia, Mediterranean Sea) receiving an artificial warm water plume generating T anomalies of 1.5–5.0 °C. Sediments were collected before and after 3 and 11 weeks from the initial plume release. Both MHWs influenced sedimentary OM quantity, composition, and degradation rates, with major effects associated with the highest T anomaly after 3 weeks. Both MHWs enhanced sedimentary OM contents, with larger effects associated with the highest T anomaly. Phytopigment contents increased in the short term but dropped to initial levels after 11 weeks, suggesting the occurrence of thermal adaptation or stress of microphytobenthos. In the longer term we observed a decrease in the nutritional quality of OM and a slowdown of its turnover mediated by extracellular enzymes, suggestive of a decreased ecosystem functioning. We anticipate that intensification of MHWs will affect benthic communities not only through direct effects on species tolerance but also by altering benthic biogeochemistry and the efficiency of energy transfer towards higher trophic levels.https://www.mdpi.com/2079-7737/11/6/841marine heat wavessedimentary organic matterbiopolymeric CC degradationecosystem functioning
spellingShingle Santina Soru
Patrizia Stipcich
Giulia Ceccherelli
Claudia Ennas
Davide Moccia
Antonio Pusceddu
Effects of Field Simulated Marine Heatwaves on Sedimentary Organic Matter Quantity, Biochemical Composition, and Degradation Rates
Biology
marine heat waves
sedimentary organic matter
biopolymeric C
C degradation
ecosystem functioning
title Effects of Field Simulated Marine Heatwaves on Sedimentary Organic Matter Quantity, Biochemical Composition, and Degradation Rates
title_full Effects of Field Simulated Marine Heatwaves on Sedimentary Organic Matter Quantity, Biochemical Composition, and Degradation Rates
title_fullStr Effects of Field Simulated Marine Heatwaves on Sedimentary Organic Matter Quantity, Biochemical Composition, and Degradation Rates
title_full_unstemmed Effects of Field Simulated Marine Heatwaves on Sedimentary Organic Matter Quantity, Biochemical Composition, and Degradation Rates
title_short Effects of Field Simulated Marine Heatwaves on Sedimentary Organic Matter Quantity, Biochemical Composition, and Degradation Rates
title_sort effects of field simulated marine heatwaves on sedimentary organic matter quantity biochemical composition and degradation rates
topic marine heat waves
sedimentary organic matter
biopolymeric C
C degradation
ecosystem functioning
url https://www.mdpi.com/2079-7737/11/6/841
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