Gross primary production, respiration, and net calcification in coral reef sediments of Heron Island Lagoon, Australia, determined by in situ benthic chamber incubations

Fuente: PANGAEA
Enregistré dans:
Détails bibliographiques
Auteurs principaux: Lantz, Coulson A, Schulz, Kai Georg, Stoltenberg, Laura, Eyre, Bradley D
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 2017
Sujets:
Accès en ligne:
Tags: Ajouter un tag
Pas de tags, Soyez le premier à ajouter un tag!
_version_ 1867170079505907712
author Lantz, Coulson A
Schulz, Kai Georg
Stoltenberg, Laura
Eyre, Bradley D
author_facet Lantz, Coulson A
Schulz, Kai Georg
Stoltenberg, Laura
Eyre, Bradley D
collection Datos científicos de ciencias marinas y ambientales
contents Rates of gross primary production (GPP), respiration (R), and net calcification (Gnet) in coral reef sediments are expected to change in response to global warming (and the consequent increase in sea surface temperature) and coastal eutrophication (and the subsequent increase in the concentration of organic matter (OM) being filtered by permeable coral reef carbonate sediments). To date, no studies have examined the combined effect of seawater warming and OM enrichment on coral reef carbonate sediment metabolism and dissolution. This study used 22-hour in situ benthic chamber incubations to examine the combined effect of temperature (T) and OM, in the form of coral mucus and phytodetritus, on GPP, R, and Gnet in the permeable coral reef carbonate sediments of Heron Island lagoon, Australia. Compared to control incubations, both warming (+2.4 ºC) and OM increased R and GPP. Under warmed conditions, R was enhanced to a greater extent than GPP, resulting in a shift to net heterotrophy and net dissolution. Under both phytodetritus and coral mucus treatments, GPP was enhanced to a greater extent than R, resulting in a net increase in GPP/R and Gnet. The combined effect of warming and OM enhanced R and GPP, but the net effect on GPP/R and Gnet was not significantly different from control incubations. These findings show that a shift to net heterotrophy and dissolution due to short-term increases in seawater warming may be countered by a net increase GPP/R and Gnet due to short-term increases in nutrient release from OM.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_883559
institution PANGAEA
language en
publishDate 2017
publisher PANGAEA
record_format pangaea
spellingShingle Gross primary production, respiration, and net calcification in coral reef sediments of Heron Island Lagoon, Australia, determined by in situ benthic chamber incubations
Lantz, Coulson A
Schulz, Kai Georg
Stoltenberg, Laura
Eyre, Bradley D
Alkalinity, total; Aragonite saturation state; Australia; Calcification rate of calcium carbonate; Carbon, inorganic, dissolved; DATE/TIME; Gross primary production/Respiration rate ratio; Gross primary production of oxygen; Heron_Island_lagoon; Incubation duration; Net calcification rate of calcium carbonate; Net primary production of oxygen; Oxygen; pH, total scale; Respiration rate, oxygen; Time in hours; Treatment
Rates of gross primary production (GPP), respiration (R), and net calcification (Gnet) in coral reef sediments are expected to change in response to global warming (and the consequent increase in sea surface temperature) and coastal eutrophication (and the subsequent increase in the concentration of organic matter (OM) being filtered by permeable coral reef carbonate sediments). To date, no studies have examined the combined effect of seawater warming and OM enrichment on coral reef carbonate sediment metabolism and dissolution. This study used 22-hour in situ benthic chamber incubations to examine the combined effect of temperature (T) and OM, in the form of coral mucus and phytodetritus, on GPP, R, and Gnet in the permeable coral reef carbonate sediments of Heron Island lagoon, Australia. Compared to control incubations, both warming (+2.4 ºC) and OM increased R and GPP. Under warmed conditions, R was enhanced to a greater extent than GPP, resulting in a shift to net heterotrophy and net dissolution. Under both phytodetritus and coral mucus treatments, GPP was enhanced to a greater extent than R, resulting in a net increase in GPP/R and Gnet. The combined effect of warming and OM enhanced R and GPP, but the net effect on GPP/R and Gnet was not significantly different from control incubations. These findings show that a shift to net heterotrophy and dissolution due to short-term increases in seawater warming may be countered by a net increase GPP/R and Gnet due to short-term increases in nutrient release from OM.
title Gross primary production, respiration, and net calcification in coral reef sediments of Heron Island Lagoon, Australia, determined by in situ benthic chamber incubations
topic Alkalinity, total; Aragonite saturation state; Australia; Calcification rate of calcium carbonate; Carbon, inorganic, dissolved; DATE/TIME; Gross primary production/Respiration rate ratio; Gross primary production of oxygen; Heron_Island_lagoon; Incubation duration; Net calcification rate of calcium carbonate; Net primary production of oxygen; Oxygen; pH, total scale; Respiration rate, oxygen; Time in hours; Treatment
url https://doi.org/10.1594/PANGAEA.883559