Respiratory and cutaneous water loss of temperate-zone passerine birds
Jennifer Ro ⁎, Joseph B. Williams
Department of Evolution, Ecology and Organismal Biology, 318 West 12th Avenue, Aronoff Laboratory, Ohio State University, Columbus, OH 43201, USA
abstract article info
Article history:
Received 2 December 2009
Received in revised form 10 February 2010
Accepted 10 February 2010
Available online 16 February 2010
Keywords:
Bird
Cutaneous water loss
Respiratory water loss
Lipid
Skin
Stratum corneum
Temperate birds
We measured respiratory water loss (RWL) and cutaneous water loss (CWL) of 12 species of passerine birds,
all from a temperate environment, and related their CWL to classes of lipids within the stratum corneum
(SC). We purposed to gain insight into the generality of patterns of CWL in birds that have been generated
mostly from studies on species from deserts, and we addressed the hypothesis that CWL is a passive diffusion
process. Despite taxonomic and ecological differences among 12 species of temperate birds, mass-specific
RWL and surface-specific CWL were statistically indistinguishable across species. When the birds were dead,
CWL was reduced by 16.3% suggesting that CWL is, in part, under physiological control. We found that
ceramides, cerebrosides, dioscylceramides, cholesterol, cholesterol sulfate, fatty acid methyl esters, free fatty
acid, sterol esters, and triacylglycerol constituted the intercellular lipids of the avian SC. CWL was positively
associated with amount of ceramide 3, but this lipid class represented less than 2% of the total SC lipids.
Combining direct measurements (n = 24) of RWL with indirect estimates (n = 25) yielded the equation log
RWL (g H
2
O/d) =-0.86 + 0.73 (log body mass, g).
© 2010 Elsevier Inc. All rights reserved.
1. Introduction
To maintain an aqueous internal milieu in the face of a desiccating
external environment, terrestrial animals have developed behavioral,
morphological, and physiological mechanisms, produced by natural
selection, to conserve body water (Bartholomew and Cade, 1963;
Addo-Bediako et al., 2001; Lillywhite, 2006). Among the morpholog-
ical and associated physiological mechanisms that terrestrial
endotherms possess to reduce evaporative water losses are structures
in the nares called nasal turbinates that are thought to recover water
from the exhaled air stream, thereby reducing respiratory water loss
(RWL), and a relatively impermeable integument with an attendant
lower cutaneous water loss (CWL) (Hillenius 1992; Gorden and Olson,
1995; Tieleman et al., 1999; Tieleman and Williams, 2002). In many
species of birds, evaporative water demand is relatively high because
they are diurnal, exposed to higher solar radiation loads, higher
ambient air temperatures (T
a
), and increased wind speeds (Maclean,
1996). In addition, birds have high mass-specific rates of metabolism
and as a result high oxygen demand, which influences RWL (Tieleman
et al., 1999).
The importance of understanding mechanisms of evaporative
water loss in small birds is underscored when one considers that total
evaporative water loss (TEWL), the sum of RWL and CWL, is their
major avenue of water loss, accounting for up to 83% of total water
loss at moderate temperatures (Willoughby, 1968; Bartholomew,
1972; Williams, 1996). At these same temperatures, CWL comprises
over 60% of TEWL emphasizing the importance of this variable in the
water economy of birds (Wolf and Walsberg, 1996; Tieleman and
Williams, 2002; McKechnie and Wolf, 2004; Muñoz-Garcia and
Williams, 2005b, 2007).
Most investigators have indirectly estimated RWL by measuring
the temperature of exhaled air and minute volume during respiration,
and then calculating RWL as a product of minute volume and the
saturated water vapor density at the temperature of exhaled air
(Withers and Williams, 1990; Tieleman and Williams, 1999; Geist,
2000). CWL has also been indirectly estimated by using whole body
plethsesmography (Withers and Williams, 1990), or by evaluating
resistance of sites on the skin and calculating whole organism CWL
from Fick's law of diffusion and estimates of skin surface area
(Michaeli and Pinshow, 2001; Marder et al., 2003; Larcombe et al.,
2003). Direct measurements of RWL and CWL of birds are few, mostly
from desert species; RWL and CWL has been measured in only four
non-desert species of birds (Tieleman and Williams, 2002; Muñoz-
Garcia and Williams, 2005b, 2007).
Whether water permeation through the skin is dictated entirely by
passive diffusion, or if it is under active physiological control
mechanism(s), remains a subject of debate (Chuong et al., 2002;
Muñoz-Garcia and Williams, 2005b; Falkenberg and Georgiadis,
2008). Some authors have suggested that CWL is a passive diffusion
process (Pinnagoda, 1994; Wilson and Maibach, 1994; Chuong et al.,
2002), whereas others have suggested that water transport across the
living epidermis can be physiologically altered by changing ion
gradients, a process involving active transport (Falkenberg and
Georgiadis, 2008), or by altering vascular blood supply to the dermis;
Comparative Biochemistry and Physiology, Part A 156 (2010) 237–246
⁎ Corresponding author. Tel.: + 1 614 292 3393; fax: +1 614 292 2030.
E-mail address: ro.25@buckeyemail.osu.edu (J. Ro).
1095-6433/$ – see front matter © 2010 Elsevier Inc. All rights reserved.
doi:10.1016/j.cbpa.2010.02.008
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