Temperature‐Oxygen Interactions and the Evolution of Giant Antarctic Sea Spiders

For more than a hundred years, scientists have known that many marine invertebrate taxa grow to unusually large size in polar waters. This biogeographic pattern has become known as polar gigantism, and it occurs in taxa as diverse as glass sponges, ctenophores, foraminiferans, polychaete annelids, i...

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Published in:The FASEB Journal
Main Authors: Woods, H. Arthur, Moran, Amy L., Tobalske, Bret W, Lane, Steven J, Shishido, Caitlin L.
Other Authors: National Science Foundation
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2016
Subjects:
Online Access:http://dx.doi.org/10.1096/fasebj.30.1_supplement.1230.1
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spelling crwiley:10.1096/fasebj.30.1_supplement.1230.1 2024-06-02T07:58:39+00:00 Temperature‐Oxygen Interactions and the Evolution of Giant Antarctic Sea Spiders Woods, H. Arthur Moran, Amy L. Tobalske, Bret W Lane, Steven J Shishido, Caitlin L. National Science Foundation 2016 http://dx.doi.org/10.1096/fasebj.30.1_supplement.1230.1 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#am http://onlinelibrary.wiley.com/termsAndConditions#vor The FASEB Journal volume 30, issue S1 ISSN 0892-6638 1530-6860 journal-article 2016 crwiley https://doi.org/10.1096/fasebj.30.1_supplement.1230.1 2024-05-03T11:19:32Z For more than a hundred years, scientists have known that many marine invertebrate taxa grow to unusually large size in polar waters. This biogeographic pattern has become known as polar gigantism, and it occurs in taxa as diverse as glass sponges, ctenophores, foraminiferans, polychaete annelids, isopod crustaceans, copepods, amphipod crustaceans, and pycnogonids. Despite being common, polar gigantism remains a physiological and evolutionary mystery; how and why do polar taxa grow to such large sizes? Using Antarctic sea spiders (pycnogonids), we tested one of the leading physiological hypotheses about polar gigantism—the oxygen hypothesis, proposed by Chapelle and Peck, which states that polar giants are permitted in very cold water by high levels of oxygen supply coupled to low metabolic demand for that oxygen. We measured whole‐body metabolic rates spanning three orders of magnitude in body size. Metabolic rate scaled to body mass with an exponent of 0.9, indicating that giant sea spiders do not require unusually low metabolic rates. Using oxygen electrodes and dye‐tracer experiments, we examined the details of oxygen transport across the cuticle and of oxygen levels and transport in the hemocoel. Oxygen is taken up across the cuticle (there is no distinct respiratory organ), and the cuticle is a much greater barrier to oxygen movement than is the mix of fluids and tissues inside the legs and trunk. Oxygen levels in the hemocoel were high everywhere in the body, but were consistently highest in distal parts of the legs and lowest in the trunk. In addition, larger sea spiders had lower central levels of oxygen. Our dye tracer experiments suggested that contractions of the heart and muscles in the legs drive relatively rapid blood circulation, especially between the trunk and proximal parts of the legs. This indicates that sea spiders use their proximal leg segments as respiratory surfaces. Building on these physiological details, we constructed a mathematical model of oxygen transport and consumption, which ... Article in Journal/Newspaper Antarc* Antarctic Copepods Glass sponges Wiley Online Library Antarctic The FASEB Journal 30 S1
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description For more than a hundred years, scientists have known that many marine invertebrate taxa grow to unusually large size in polar waters. This biogeographic pattern has become known as polar gigantism, and it occurs in taxa as diverse as glass sponges, ctenophores, foraminiferans, polychaete annelids, isopod crustaceans, copepods, amphipod crustaceans, and pycnogonids. Despite being common, polar gigantism remains a physiological and evolutionary mystery; how and why do polar taxa grow to such large sizes? Using Antarctic sea spiders (pycnogonids), we tested one of the leading physiological hypotheses about polar gigantism—the oxygen hypothesis, proposed by Chapelle and Peck, which states that polar giants are permitted in very cold water by high levels of oxygen supply coupled to low metabolic demand for that oxygen. We measured whole‐body metabolic rates spanning three orders of magnitude in body size. Metabolic rate scaled to body mass with an exponent of 0.9, indicating that giant sea spiders do not require unusually low metabolic rates. Using oxygen electrodes and dye‐tracer experiments, we examined the details of oxygen transport across the cuticle and of oxygen levels and transport in the hemocoel. Oxygen is taken up across the cuticle (there is no distinct respiratory organ), and the cuticle is a much greater barrier to oxygen movement than is the mix of fluids and tissues inside the legs and trunk. Oxygen levels in the hemocoel were high everywhere in the body, but were consistently highest in distal parts of the legs and lowest in the trunk. In addition, larger sea spiders had lower central levels of oxygen. Our dye tracer experiments suggested that contractions of the heart and muscles in the legs drive relatively rapid blood circulation, especially between the trunk and proximal parts of the legs. This indicates that sea spiders use their proximal leg segments as respiratory surfaces. Building on these physiological details, we constructed a mathematical model of oxygen transport and consumption, which ...
author2 National Science Foundation
format Article in Journal/Newspaper
author Woods, H. Arthur
Moran, Amy L.
Tobalske, Bret W
Lane, Steven J
Shishido, Caitlin L.
spellingShingle Woods, H. Arthur
Moran, Amy L.
Tobalske, Bret W
Lane, Steven J
Shishido, Caitlin L.
Temperature‐Oxygen Interactions and the Evolution of Giant Antarctic Sea Spiders
author_facet Woods, H. Arthur
Moran, Amy L.
Tobalske, Bret W
Lane, Steven J
Shishido, Caitlin L.
author_sort Woods, H. Arthur
title Temperature‐Oxygen Interactions and the Evolution of Giant Antarctic Sea Spiders
title_short Temperature‐Oxygen Interactions and the Evolution of Giant Antarctic Sea Spiders
title_full Temperature‐Oxygen Interactions and the Evolution of Giant Antarctic Sea Spiders
title_fullStr Temperature‐Oxygen Interactions and the Evolution of Giant Antarctic Sea Spiders
title_full_unstemmed Temperature‐Oxygen Interactions and the Evolution of Giant Antarctic Sea Spiders
title_sort temperature‐oxygen interactions and the evolution of giant antarctic sea spiders
publisher Wiley
publishDate 2016
url http://dx.doi.org/10.1096/fasebj.30.1_supplement.1230.1
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
Copepods
Glass sponges
genre_facet Antarc*
Antarctic
Copepods
Glass sponges
op_source The FASEB Journal
volume 30, issue S1
ISSN 0892-6638 1530-6860
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