Skip to main content Accessibility help
×
Hostname: page-component-848d4c4894-75dct Total loading time: 0 Render date: 2024-05-01T13:24:28.789Z Has data issue: false hasContentIssue false

7 - ION AND WATER BALANCE

Published online by Cambridge University Press:  04 August 2010

Get access

Summary

Introduction

Species of aquatic crabs live in waters ranging in concentration from freshwater (0–15 mOsm.kg-1 H2O) to hypersaline media (>l, 000 mOsm-kg-1 H2O). These waters may be of relatively constant composition (offshore seawater and large lakes) or of fluctuating composition due to tidal or climatic factors. Crabs (and other aquatic organisms) have developed mechanisms to maintain the preferred concentrations of their tissue fluids in the particular medium in which they live. Several distinct patterns of osmotic and ionic regulation are evident (see reviews by Greenaway, 1979; Mantel and Farmer, 1983) and will be briefly summarized.

Species characteristic of sublittoral marine habitats have body fluids similar in concentration and composition to seawater. They are relatively permeable to water and ions and produce urine that is isosmotic with the hemolymph. Limited regulation of the ionic composition of the hemolymph is generally evident with magnesium and sulfate concentrations kept lower than in seawater by preferential elimination in the urine. Concentrations of the other major ions are often slightly higher in the hemolymph than in seawater. The animals may withstand limited dilution of their medium but show no ability to regulate the concentration of their extracellular fluids, which remain isosmotic with the medium. Crabs showing this pattern of osmoregulation are referred to as osmoconformers.

Many euryhaline crabs regulate the concentration of their hemolymph in dilute media. In seawater and concentrations higher than seawater, their extracellular fluids are isosmotic with the medium, but in media of lower concentration they attempt to maintain the osmolality of the hemolymph above that of the medium. This results both in loss of ions across the body surface down electrochemical gradients and in osmotic influx of water.

Type
Chapter
Information
Publisher: Cambridge University Press
Print publication year: 1988

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Save book to Kindle

To save this book to your Kindle, first ensure coreplatform@cambridge.org is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

Available formats
×