Limits to Diffusive O2 Transport: Flow, Form, and Function in Nudibranch Egg Masses from Temperate and Polar Regions

Background: Many aquatic animals enclose embryos in gelatinous masses, and these embryos rely on diffusion to supply oxygen. Mass structure plays an important role in limiting or facilitating O2 supply, but external factors such as temperature and photosynthesis can play important roles as well. Oth...

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Main Authors: Amy L Moran, H Arthur Woods
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Online Access:https://journals.plos.org/plosone/article?id=10.1371/journal.pone.0012113
https://journals.plos.org/plosone/article/file?id=10.1371/journal.pone.0012113&type=printable
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spelling ftrepec:oai:RePEc:plo:pone00:0012113 2024-04-14T08:03:47+00:00 Limits to Diffusive O2 Transport: Flow, Form, and Function in Nudibranch Egg Masses from Temperate and Polar Regions Amy L Moran H Arthur Woods https://journals.plos.org/plosone/article?id=10.1371/journal.pone.0012113 https://journals.plos.org/plosone/article/file?id=10.1371/journal.pone.0012113&type=printable unknown https://journals.plos.org/plosone/article?id=10.1371/journal.pone.0012113 https://journals.plos.org/plosone/article/file?id=10.1371/journal.pone.0012113&type=printable article ftrepec 2024-03-19T10:29:27Z Background: Many aquatic animals enclose embryos in gelatinous masses, and these embryos rely on diffusion to supply oxygen. Mass structure plays an important role in limiting or facilitating O2 supply, but external factors such as temperature and photosynthesis can play important roles as well. Other external factors are less well understood. Methodology/Principal Findings: We first explored the effects of water flow on O2 levels inside nudibranch embryo masses and compared the effects of flow on masses from temperate and polar regions. Water flow (still vs. vigorously bubbled) had a strong effect on central O2 levels in all masses; in still water, masses were considerably more hypoxic than in bubbled water. This effect was stronger in temperate than in polar masses, likely due to the increased metabolic demand and O2 consumption of temperate masses. Second, we made what are to our knowledge the first measurements of O2 in invertebrate masses in the field. Consistent with laboratory experiments, O2 in Antarctic masses was high in masses in situ, suggesting that boundary-layer effects do not substantially limit O2 supply to polar embryos in the field. Conclusions/Significance: All else being equal, boundary layers are more likely to depress O2 in masses in temperate or tropical regions; thus, selection on parents to choose high-flow sites for mass deposition is likely greater in warm water. Because of the large number of variables affecting diffusive O2 supply to embryos in their natural environment, field observations are necessary to test hypotheses generated from laboratory experiments and mathematical modeling. Article in Journal/Newspaper Antarc* Antarctic RePEc (Research Papers in Economics) Antarctic
institution Open Polar
collection RePEc (Research Papers in Economics)
op_collection_id ftrepec
language unknown
description Background: Many aquatic animals enclose embryos in gelatinous masses, and these embryos rely on diffusion to supply oxygen. Mass structure plays an important role in limiting or facilitating O2 supply, but external factors such as temperature and photosynthesis can play important roles as well. Other external factors are less well understood. Methodology/Principal Findings: We first explored the effects of water flow on O2 levels inside nudibranch embryo masses and compared the effects of flow on masses from temperate and polar regions. Water flow (still vs. vigorously bubbled) had a strong effect on central O2 levels in all masses; in still water, masses were considerably more hypoxic than in bubbled water. This effect was stronger in temperate than in polar masses, likely due to the increased metabolic demand and O2 consumption of temperate masses. Second, we made what are to our knowledge the first measurements of O2 in invertebrate masses in the field. Consistent with laboratory experiments, O2 in Antarctic masses was high in masses in situ, suggesting that boundary-layer effects do not substantially limit O2 supply to polar embryos in the field. Conclusions/Significance: All else being equal, boundary layers are more likely to depress O2 in masses in temperate or tropical regions; thus, selection on parents to choose high-flow sites for mass deposition is likely greater in warm water. Because of the large number of variables affecting diffusive O2 supply to embryos in their natural environment, field observations are necessary to test hypotheses generated from laboratory experiments and mathematical modeling.
format Article in Journal/Newspaper
author Amy L Moran
H Arthur Woods
spellingShingle Amy L Moran
H Arthur Woods
Limits to Diffusive O2 Transport: Flow, Form, and Function in Nudibranch Egg Masses from Temperate and Polar Regions
author_facet Amy L Moran
H Arthur Woods
author_sort Amy L Moran
title Limits to Diffusive O2 Transport: Flow, Form, and Function in Nudibranch Egg Masses from Temperate and Polar Regions
title_short Limits to Diffusive O2 Transport: Flow, Form, and Function in Nudibranch Egg Masses from Temperate and Polar Regions
title_full Limits to Diffusive O2 Transport: Flow, Form, and Function in Nudibranch Egg Masses from Temperate and Polar Regions
title_fullStr Limits to Diffusive O2 Transport: Flow, Form, and Function in Nudibranch Egg Masses from Temperate and Polar Regions
title_full_unstemmed Limits to Diffusive O2 Transport: Flow, Form, and Function in Nudibranch Egg Masses from Temperate and Polar Regions
title_sort limits to diffusive o2 transport: flow, form, and function in nudibranch egg masses from temperate and polar regions
url https://journals.plos.org/plosone/article?id=10.1371/journal.pone.0012113
https://journals.plos.org/plosone/article/file?id=10.1371/journal.pone.0012113&type=printable
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_relation https://journals.plos.org/plosone/article?id=10.1371/journal.pone.0012113
https://journals.plos.org/plosone/article/file?id=10.1371/journal.pone.0012113&type=printable
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