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      Size Is the Major Determinant of Pumping Rates in Marine Sponges

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          Abstract

          Sponges play an important ecological function in many benthic habitats. They filter large volumes of water, retain suspended particles with high efficiency, and process dissolved compounds. Nevertheless, the factors that regulate sponge pumping rate and its relation to environmental factors have been rarely studied. We examined, in situ, the variation of pumping rates for five Mediterranean sponge species and its relationship to temperature, particulate food abundance and sponge size over two annual cycles. Surprisingly, temperature and food concentration had only a small effect on pumping rates, and the seasonal variation of pumping rates was small (1.9–2.5 folds). Sponge size was the main determinant of the specific pumping rate (pumping normalized to sponge volume or mass). Within the natural size distribution of each species, the volume-specific pumping rate [PR V , ml min −1 (cm sponge) −3] decreased (up to 33 folds) with the increase in sponge volume ( V, cm 3), conforming to an allometric power function (PR V = aV b ) with negative exponents. The strong dependence of the size-specific pumping rate on the sponge size suggests that the simplistic use of this value to categorize sponge species and predict their activity may be misleading. For example, for small specimens, size-specific pumping rates of the two low-microbial-abundance (LMA) species (allometric exponent b of −0.2 and −0.3) were similar to those of two of the high-microbial-abundance (HMA) species ( b of −0.5 and −0.7). However, for larger specimens, size-specific pumping rates were markedly different. Our results suggest that the pumping rate of the sponges we studied can be approximated using the measured allometric constants alone in conjunction with surveys of sponge abundance and size distribution. This information is essential for the quantification of in situ feeding and respiration rates and for estimates of the magnitude of sponge-mediated energy and nutrient fluxes at the community level. Further work is required to establish if and to what extent the low seasonal effect and the strong size dependency of pumping rate can be generalized to other sponges and habitats.

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          Surviving in a marine desert: the sponge loop retains resources within coral reefs.

          Ever since Darwin's early descriptions of coral reefs, scientists have debated how one of the world's most productive and diverse ecosystems can thrive in the marine equivalent of a desert. It is an enigma how the flux of dissolved organic matter (DOM), the largest resource produced on reefs, is transferred to higher trophic levels. Here we show that sponges make DOM available to fauna by rapidly expelling filter cells as detritus that is subsequently consumed by reef fauna. This "sponge loop" was confirmed in aquarium and in situ food web experiments, using (13)C- and (15)N-enriched DOM. The DOM-sponge-fauna pathway explains why biological hot spots such as coral reefs persist in oligotrophic seas--the reef's paradox--and has implications for reef ecosystem functioning and conservation strategies.
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            Scaling metabolism from organisms to ecosystems.

            Understanding energy and material fluxes through ecosystems is central to many questions in global change biology and ecology. Ecosystem respiration is a critical component of the carbon cycle and might be important in regulating biosphere response to global climate change. Here we derive a general model of ecosystem respiration based on the kinetics of metabolic reactions and the scaling of resource use by individual organisms. The model predicts that fluxes of CO2 and energy are invariant of ecosystem biomass, but are strongly influenced by temperature, variation in cellular metabolism and rates of supply of limiting resources (water and/or nutrients). Variation in ecosystem respiration within sites, as calculated from a network of CO2 flux towers, provides robust support for the model's predictions. However, data indicate that variation in annual flux between sites is not strongly dependent on average site temperature or latitude. This presents an interesting paradox with regard to the expected temperature dependence. Nevertheless, our model provides a basis for quantitatively understanding energy and material flux between the atmosphere and biosphere.
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              Global warming-enhanced stratification and mass mortality events in the Mediterranean.

              Summer conditions in the Mediterranean Sea are characterized by high temperatures and low food availability. This leads to "summer dormancy" in many benthic suspension feeders due to energetic constraints. Analysis of the most recent 33-year temperature time series demonstrated enhanced stratification due to global warming, which produced a approximately 40% lengthening of summer conditions. Many biological processes are expected to be affected by this trend, culminating in such events as mass mortality of invertebrates. Climatic anomalies concomitant with the occurrence of these events represent prolonged exposure to warmer summer conditions coupled with reduced food resources. Simulation of the effects of these conditions on a model organism demonstrated a biomass loss of >35%. Losses of this magnitude result in mortality similar to that noted in field observations during mass mortality events. These results indicate that temperature anomalies are the underlying cause of the events, with energetic constraints serving as the main triggering mechanism.
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                Author and article information

                Contributors
                Journal
                Front Physiol
                Front Physiol
                Front. Physiol.
                Frontiers in Physiology
                Frontiers Media S.A.
                1664-042X
                11 December 2019
                2019
                : 10
                : 1474
                Affiliations
                [1] 1Max Planck Institute for Marine Microbiology, HGF MPG Joint Research Group for Deep-Sea Ecology and Technology , Bremen, Germany
                [2] 2Department of Marine Biology and Oceanography, Institut de Ciències del Mar (ICM-CSIC) , Barcelona, Spain
                [3] 3The Faculty of Marine Science, Ruppin Academic Center , Michmoret, Israel
                [4] 4Department of Marine Ecology, Centre d’Estudis Avançats de Blanes (CEAB-CSIC) , Girona, Spain
                Author notes

                Edited by: Silvia Franzellitti, University of Bologna, Italy

                Reviewed by: Lorenzo Gallus, University of Genoa, Italy; Simon Morley, British Antarctic Survey (BAS), United Kingdom

                *Correspondence: Teresa Maria Morganti, tmorgant@ 123456mpi-bremen.de

                This article was submitted to Aquatic Physiology, a section of the journal Frontiers in Physiology

                Article
                10.3389/fphys.2019.01474
                6917621
                31920688
                d5a91688-619a-476b-a0be-ae3cc32b0ae2
                Copyright © 2019 Morganti, Ribes, Yahel and Coma.

                This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

                History
                : 09 August 2019
                : 14 November 2019
                Page count
                Figures: 5, Tables: 6, Equations: 2, References: 120, Pages: 18, Words: 14326
                Funding
                Funded by: Spanish Government
                Award ID: RTI2018 – 094187-B-100
                Funded by: EU Project AMARE
                Funded by: Ministerio de Educación, Cultura y Deporte (MECD) 10.13039/501100003176
                Funded by: Max Planck Society 10.13039/501100004189
                Funded by: Marine Biogeochemistry
                Funded by: Generalitat de Catalunya 10.13039/501100002809
                Award ID: 2017SGR1011
                Funded by: ISF
                Award ID: 1280/13
                Funded by: BSF
                Award ID: 2012089
                Categories
                Physiology
                Original Research

                Anatomy & Physiology
                porifera,pumping rate,environmental factors,size,seasonality,allometric scaling,high-low microbial-abundance sponges

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