9
Phytochemistry,Vo l. 20, No . 4, pp . 659 -666 , 1981. 0031-9422/81/040659--08 $02.00/0 Printed in Great Britain. © 1981 Pergamon Press Ltd. A COMPARISON OF LIPID COMPONENTS OF THE FRESH LEAVES AND PNEUMATOPHORES OF THE MANGROVE AVICENNIA MAR INA AND DEAD G. P. WANNIGAMA,* J. K. VOLKMAN,~ F. T. GILLAN, P. D. NICHOLS and R. B. JOHNS~ Department of Organic Chemistry, University of Melbourne, Parkville, Victoria, 3052, Australia (Revised received 18 August 1980) Key Word Iudex--Avicennia marina; Avicenniaceae; mangrove; hydrocarbons; alcohols; sterols; triterpene alcohols; monobasic adds; ~t¢o-di basic cids; ¢o-hydroxy acids. A b s t r a c t - - T h e comp onent hydrocarbo ns, s t er o l s, a l c o h o ls , m o n o b a s i c , ~,c~-dibasic and co-h ydroxy a c i d s o f t h e f r e sh and decayed leaves and the pneumatopho res of the mangrove Avicennia marina are reported in detai l. Fro m the quantitative comparisons which can be drawn, relative changes in the lipid classes occurring during leaf decay can be highlighted. These base-line data are importan t to our understanding of inputs to m arine intertidal sedi ments. During leaf decay the o n l y significan t c h a n g e s w e r e a reduction i n the total a b s o l u t e c o n c e n t r a t i o ns ofmonob a s i c a c i d s due largely to adecrease in concentration of the C18 polyunsaturated fatty acids, and an enhancement of the concentrations of the long-chain monob asic acids, co-hydroxy acids and ~,co-dibasi c acids. This resistance to degrad ation shown by the cutin derived acids (or,co-dibasic, co-hydroxy and long-ch ain m ono basic acids) relative t o the cellular and wax derived lipids may allow these cutin components to be used as quantitative markers of A. marina in mangrove associated sediments. INTRODUCTION In the course of the studies of lipid input and diagenesis in mangrove associated sediments we have previously reported an analysis of the diacids of the mangrove Avicennia marina [1] and proposed direct input of the diacids to the sediments. A study by Sassen on mangrove peats [2,3 ], involving analysis of monobasic acids only, suggested a majo r input of man grove lipids to a sediment, and presented evidence (leaf litter analysis) of selective degradation of short-chain fatty adds. The mangroves Rhizophora mangle, Laguncularia racemosa, Avicennia germinans a n d A. nitida were analysed. Similar degradative studies have been reported on the sea grass Spartina alterniflora [4], and on leaves in fresh water streams [5,6]. In this paper a more detailed lipid analysis of the living and dead leaves and the pneumatopbores of Avicennia marina collecte d from Port Franklin, Victoria is reported. Lipid classes analysed include hydrocarbo ns, sterols, fatty alcohols, monobasic adds, ~¢o-dibasic acids and ~o- hydroxy adds. The fatty acids and alcohols were further subdivided into bou nd and solvent-extractabl e fractions, as prior work [7] has suggested the interpretative usefulness of this procedure. The monobasic acid data reported includes the molecular structures of the component fatty adds, since such data are essential for both biochemical and geochemical interpretation of the components present and of the changes observed during * On leave from the Department of Chemistry, University of Peradeniya, Peradeniya, Sri Lanka. t Present address: Organic Geochemistry Unit, School of Chemistry, Bristol University, BS8 ITS, U.K. To whom reprint requests should be addressed. mangrove biodegradation and early diagenesis in recent marine sediments [7]. Such knowledge is pertinent to models of lignite coal deposition. RESULTS AND DISCUSSION The component hydrocarbons of the fresh and dead leaves and the pneumatophores of Avicennia marina a r e presented in Table 1. The hydrocarbon distributions in the leaf wax and in the leaves after wax removal are also presented. The n-alkane distribution of the fresh leaves is similar to those reported for the waxes of most higher plants [8-10]. Features such as the abundance o f branched alkanes and the presence of long-chain alkenes do however make the hydrocarbon profile of A. marina distinctive. The paucity of previous alkane reports which incl ude data on these components m ay be the result of the insufficient resolution of the packed GC columns previously employed for such analyses. However, one example is the noting of branched alkanes in the epicuticular wax of Andropogon haUii [11]. The hydrocarbon distribution in the dead leaves is similar to that found in the fresh leaves even to the presence of branched alkanes and traces of long-chain length alkenes. The leaf wax contrasts with the who le leaf analysis only in the absence of squalene. The component hydrocarbons in the pneumatophores are characterized by a predominance of shorter chain n- alkanes. Long-chain n-alkanes, n-alkenes and branched alkanes were not detected in contrast to the leaves. Squalene was present, but at a reduced relative level compared to the leaf samples. These differences can be rationalized in terms of the different structure and function of these two plant organs. The sterol composition of the fresh and dead leaves of A. marina (Table 2) are extremely similar. Sitosterol (the 65 9

A Comparison of Lipid Components of the Fresh and Dead Leaves and Pneumatophores of the Mangrove Avicennia Marina

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Phytochemistry,Vo l. 20, No . 4, pp . 659 -666 , 1981. 0031-9422/81/040659--08 $02.00/0Printed in Grea t Britain. © 1981 Pergamon Press Ltd.

A C O M P A R I S O N O F L I P I D C O M P O N E N T S O F T H E F R E SH

L E A V E S A N D P N E U M A T O P H O R E S O F TH E

M A N G R O V E A V I C E N N I A M A R I N A

A N D D E A D

G . P . WANNIGAMA,* J . K. VOLKM AN,~ F . T . GILLAN, P . D . NICHOLS an d R. B . JOHNS~

De partm ent o f Organic C hemistry, University of Melbourne, Parkville, Victoria, 3052, Au stralia

(Revised received 18 August 1980)

Key Word Iudex--Avicennia marina; Avicenniaceae; mangrove; hydrocarbons; alcohols; sterols; tr i terpenealcoho ls; monobasic ad ds ; ~t¢o-dibasic cids; ¢o-hydroxy acids.

A b s t r a c t - - T h e c o m p o n e n t h y d r o c a r b o n s , s t er o l s, a l c o h o ls , m o n o b a s i c , ~ , c~ -d ib a si c a n d c o - hy d r o x y a c i d s o f t h e f r e sh a n d

d e c a y e d le a v es a n d t h e p n e u m a t o p h o r e s o f t h e m a n g r o v e Av ic e nn ia mar ina a r e r e p o r t e d i n d e t a il . F r o m t h e q u a n t i t a t i v ec o m p a r i s o n s w h i c h c a n b e d r a w n , r e l a t iv e c h a n g e s i n t h e l i p i d c l a s se s o c c u r r i n g d u r i n g l e a f d e c a y c a n b e h i g h l i g h t e d .T h e s e b a s e - l in e d a t a a r e i m p o r t a n t t o o u r u n d e r s t a n d i n g o f i n p u t s t o m a r i n e i n t e r ti d a l s e d im e n t s . D u r i n g l e a f d e c a y t h eo n l y s i g n i fi c a nt c h a n g e s w e r e a r e d u c t i o n i n t h e t o t a l a b s o l u t e c o n c e n t r a t i o n s o f m o n o b a s i c a c i d s d u e l a r g e l y t o a d e c r e a s ei n c o n c e n t r a t i o n o f t h e C 1 8 p o l y u n s a t u r a t e d f a t ty a c i ds , a n d a n e n h a n c e m e n t o f t h e c o n c e n t r a t i o n s o f t h e l o n g - c h a i nm o n o b a s i c a c i d s , c o - h y d r o x y a c i d s a n d ~ , co - d ib a s ic a c id s . T h i s r e s i s ta n c e t o d e g r a d a t i o n s h o w n b y t h e c u t i n d e r i v e d a c i d s( or,c o-d ib as ic , c o - h y d r o x y a n d l o n g - c h a i n m o n o b a s i c a c i d s ) r e la t i v e to t h e c e l l u l a r a n d w a x d e r i v e d l i p i d s m a y a l l o w t h e s ec u t i n c o m p o n e n t s t o b e u s e d a s q u a n t i t a ti v e m a r k e r s o f A. marina i n m a n g r o v e a s s o c i a te d s e d i m e n t s.

INTRODUCTION

I n t h e c o u r s e o f t h e s t u d i e s o f l i p i d i n p u t a n d d i a g e n e s i s i n

m a n g r o v e a s s o c i a t e d s e d i m e n t s w e h a v e p r e v i o u s l yr e p o r t e d a n a n a l y s i s o f t h e d i a c i d s o f t h e m a n g r o v eAv ic e nn ia mar ina [ 1 ] a n d p r o p o s e d d i r e c t in p u t o f th e

d i a c i d s t o t h e s e d i m e n t s . A s t u d y b y S a s s e n o n m a n g r o v ep e a t s [2 ,3 ] , i n v o l v i n g a n a l y s i s o f m o n o b a s i c a c i d s o n l y ,s u g g e s te d a m a j o r i n p u t o f m a n g r o v e l i p i d s t o a s e d i m e n t,a n d p r e s e n t e d e v i d e n c e ( l e af l i t t e r a n a l y s i s ) o f s e le c t iv ed e g r a d a t i o n o f s h o r t- c h a i n f at t y a d d s . T h e m a n g r o v e sRhizophora mang le , L agunc u lar ia rac e mosa , Av ic e nn ia

ge rminans a n d A. n i t i da w e r e a n a l y s e d . S i m i l a rd e g r a d a t i v e s tu d i e s h a v e b e e n r e p o r t e d o n t h e s e a g r as sSpar t ina a l t e rn i f l o ra [ 4 ] , a n d o n l e a v e s i n f r e sh w a t e rs t r e a m s [ 5 , 6 ] .

I n t h i s p a p e r a m o r e d e t a i l e d l i p i d a n a l y s i s o f t h e l i v i n ga n d d e a d l e a v e s a n d t h e p n e u m a t o p b o r e s o f Av ic e nn ia

mar ina c o l le c t ed f r o m P o r t F r a n k l i n , V i c t o r i a i s r e p o r t e d .L i p i d c l a s s e s a n a l y s e d i n c l u d e h y d r o c a r b o n s , s t e r o l s , f a t t ya l c o h o l s , m o n o b a s i c a d d s , ~ ¢ o - d i b a s i c a c i d s a n d ~ o-h y d r o x y a d d s . T h e f a t t y a c id s a n d a l c o h o l s w e re f u r th e rs u b d i v i d e d i n t o b o u n d a n d s o l v e n t - e x tr a c t a b le f r ac t io n s ,a s p r i o r w o r k [ 7 ] h a s s u g g e s t e d t h e i n t e r p r e t a t i v eu s e fu l n es s o f t h is p r o c e d u r e . T h e m o n o b a s i c a c i d d a t ar e p o r t e d i n c l u d e s t h e m o l e c u l a r s t r u c t u r e s o f t h ec o m p o n e n t f a tt y a d d s , s i n ce s u c h d a t a a r e e s s en t i al fo rb o t h b i o c h e m i c a l a n d g e o c h e m i c a l i n t e r p r e t a t i o n o f t h ec o m p o n e n t s p r e s e n t a n d o f t h e c h a n g e s o b s e rv e d d u r i n g

* On leave from the D epartm ent of Chemistry, University ofPeradeniya, Peradeniya, Sri Lanka.

t Present address: Org anic Geochemistry Un it , School ofChemistry, Bristol University, BS8 ITS, U.K.

To w hom reprint requests should be addressed.

m a n g r o v e b i o d e g r a d a t i o n a n d e a r l y d ia g e n e s is in r e c e n tm a r i n e s e d i m e n t s [ 7 ] . S u c h k n o w l e d g e i s p e r t i n e n t t om o d e l s o f l i g n i t e c o a l d e p o s i t i o n .

RESULTS AND DISCUSSION

T h e c o m p o n e n t h y d r o c a r b o n s o f t h e fr e sh a n d d ead

l e av e s a n d t h e p n e u m a t o p h o r e s o f Av ic e nn ia mar ina are

p r e s e n t e d in T a b l e 1. T h e h y d r o c a r b o n d i s t r i b u t i o n s i nt h e l e a f w a x a n d i n t h e l e a v e s af t e r w a x r e m o v a l a r e a l s op r e s e n t e d . T h e n - a l k a n e d i s t r i b u t i o n o f t h e f r es h l ea v e s iss i m i l a r t o t h o s e r e p o r t e d f o r t h e w a x e s o f m o s t h i g h e rp l a n t s [ 8 - 1 0 ] . F e a t u r e s s u c h a s th e a b u n d a n c e o f

b r a n c h e d a l k a n e s a n d t h e p r e s e n ce o f lo n g - c h a i n a l k e n e sd o h o w e v e r m a k e t h e h y d r o c a r b o n p r o f il e o f A . m a r i n ad i s t in c t i v e . T h e p a u c i t y o f p r e v i o u s a l k a n e r e p o r t s w h i c h

i n c lu d e d a t a o n t h e s e c o m p o n e n t s m a y b e t h e r e s u l t o f t h ei n su f fi ci e nt r e so l u t i o n o f t h e p a c k e d G C c o l u m n sp r e v i o u s l y e m p l o y e d f o r s u c h a n a l y s e s . H o w e v e r , o n ee x a m p l e i s t h e n o t i n g o f b r a n c h e d a l k a n e s i n t h ee p i c u t i c u l a r w a x o f Andropogon haUi i [ 1 1 ] . T h eh y d r o c a r b o n d i s t r i b u t i o n i n t h e d e a d l e av e s i s s i m i l a r t ot h a t f o u n d i n t h e f r es h l e a v es e v e n t o t h e p r e s e n c e o fb r a n c h e d a l k a n e s a n d t r a ce s o f l o n g - c h a in l e n g t h a l k en e s .T h e l e a f w a x c o n t r a s t s w i t h t h e w h o l e l e a f a n a l y s i s o n l y i nt h e a b s e n c e o f s q u a l e n e .

T h e c o m p o n e n t h y d r o c a r b o n s i n th e p n e u m a t o p h o r e sa r e c h a r ac t e r i z ed b y a p r e d o m i n a n c e o f s h o r t e r c h a i n n -a l k a n es . L o n g - c h a i n n - a lk a n e s , n -a l k e ne s a n d b r a n c h e da l k a n e s w e r e n o t d e t e c t e d i n c o n t r a s t t o t h e l e a v e s .S q u a l e n e w a s p r e s e n t , b u t a t a r e d u c e d r e l a t i v e l e v elc o m p a r e d t o t h e l e a f s a m p l e s . T h e s e d i f f er e n ce s c a n b er a t i o n a l i z e d i n t e r m s o f t h e d i f f e r e n t s t r u c t u r e a n df u n c t i o n o f t h e s e t w o p l a n t o r g a n s .

T h e s t e ro l c o m p o s i t i o n o f t h e f re s h a n d d e a d l e a ve s o fA. mar ina ( T a b l e 2 ) a r e e x t r e m e l y s i m i l a r . S i t o s t e r o l ( t h e

659

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Lipids of mangrove leaves 661

Table 3. Fatty alcohol composition of Anicennia marina

Percentage composition of total alcohols

Fresh leaves Dead leaves

Homologue TSE

12:o 0.25

14:o -

15:o 0.17

16:0 0.13

18:0 1.88

18:l -

20:o 0.88

21:o tr

22:o 0.84

23:0 0.45

24:0 4.45

25:0 0.33

26:0 7.06

27~0 1.84

28:0 8.50

29:0 0.31

30:o 5.08

Phytol 55.84

Others 8.90

Wax

0.66

tr

2.0

tr

18.7

2.4

37.6

1.7

21.2

1.3

14.4

(TSE - wax)

0.7

tr

1.3

tr

1.1

1.4

17.5

0.71

49.5

0.51

20.9

nad

tr

Bound

0.25

tr

tr

0.13

0.67

tr

3.41

0.42

5.45

0.70

11.81

1.61

11.11

1.52

25.14

0.10

20.96

12.97

3.76

TSE

0.32

0.60

tr

0.27

0.40

1.80

tr

1.77

0.16

6.28

0.99

9.10

0.75

12.75

0.20

3.00

33.76

27.67

Bound

tr

0.30

0.58

0.13

3.96

1.40

4.66

1.25

8.89

0.69

6.53

1.21

9.53

tr

2.93

33.46

24.29

Pneumatophores

7.9

7.3

12.7

17.3

30.8

5.9

9.2

2.6

6.3

-

tr

Total absolute

concn (kg/g

dry wt.) 2270 150 1500 100

tr = Trace, ~0.1%.nad = Not accurately determined.

TSE = Total solvent extractables.

differs from the leaves where the ratio of sitosterol to

stigmasterol is 3 to 1.

The distribution of alcohols in the leaves of A. marina

(Table 3) is typical of most higher plants [8], ranging

from 18 :0 to 30:0 and maximiz ing a t 28:0 . Phyto l was

detected in significant quantity in both the fresh and dead

leaf samples, but was not detected in the wax fraction of

the fresh leaves. The alcohol fraction of the solvent extract

of the fresh leaves contained a significantly higher relative

and absolute amou nt of phytol than was found in the deadleaves indicating that rapid degradation of the phytol and

the chlorin pigment occurs du ring leaf decay (equivalent

chlorophyll-a ratio of fresh leaves/dead leaves is 35). The

concentration of bound alcohols in the fresh leaves was

appreciably lower than the level of solvent extractable

alcohols (Table 4 ), and was not observed to increase on

leaf decay. The distribution of alcohols within the

pneum atophore sample was unusu al, with li tt le even over

odd predominance occurring. Phytol w as a minor

com ponent only of this fraction after sapon ification

reflecting the low concen tration of chlorop hyll in the

pneumatophores.

Six compou nds identified by characteristic massspectral fragmentation patterns and GC retention data as

triterpene alcohols were found in both the fresh and dead

* Double bond positions (w) are numbered from the methyl

end of the fatty acid, all subsequent double bonds are methylene

interrupted.

leaves (Table 5) and in the pneumatopho res of A. marina

(these compoun ds were major components in the wax

fraction of the leaves). The triterpene alcohols identified

were: urs-12-ene-38-01, olean-12-ene-3p-01, lup-

20(29)ene-3 /3-ol and friedoolean-38-01. The major

component (RR, 1.168 ) has not yet been fully identified.

The absolute amou nts of this class of compou nd in both

the fresh and dead leaf samples were similar, apart from a

large decrease in the concentration of friedoolean-3B-01.

This constancy in absolute amou nts of the triterpenealcohols between the two samples was also observed for

the hydrocarbons, sterols and fatty alcohols indicating

that these classes of compoun ds are not degraded rapidly

during leaf decay. T his may reflect their l imited value as

microbial nutrients.

The monobasic acid composition of the fresh leaves of

A . marina (Table 6) ranges from C,, to C,, with 16:0 ,

1 8 : lw9*, 18 :2 ~6 a n d 1 8 :3~3 present as the predominant

acids. These data are similar to those reported previously

fo r A . nitada an d A. germinans [2,3] but include the

molecular structures of the component mono carboxylic

acids unlike the previous work. The significance of

knowing the isomer positions in the monoenoic acids hasbeen documented previously [14,15 ], and the monoenoic

acids detected in the fresh leaves were: 1.5:1, 16:lw7 ,

1 6 : 1 ~9 , tram 16: 1~13, 17:108, 18: lw7, 18:109, 19: l

and 20: 1~9.

The bound monob asic acids (released after saponi-

fication of the solvent extracted leaf residue) of the fresh

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66 2 G. P. WANNIGAMA et trl.

Table 4. Absolute amounts of lipid classes of Aricennia mu r in u

Concentration klg/g (dry wt.)

Lipid class Fresh leaves Dead leaves Ratio dead,‘fresh

Hydrocarbons 3070 3200 1.04

Sterols 1900 1640 0.86

Alcohols TSE 2270 1500 0.66

TSE less phytol 1000 990 0.99

Phytol 1270 510 0.40

Bound alcohols 150 100 0.06

Triterpene alcohols 1090 1130 1.04

Monobasic acids TSE 18420 7730 0.42

Saturated short-chain 5190 4040 0.78

Unsaturated 12660 3370 0.27

Long-chain 570 320 0.56

Bound 930 2520 2.71

Saturated short-chain 330 1140 3.45

Unsaturated 440 770 1.75

Long-chain I60 610 3.81

Total 19350 10250 0.53

Saturated short-chain 5520 5180 0.94

Unsaturated 13100 4140 0.32

Long-chain 730 930 1.27

r,cu-Dibasic acids 1600 2870 1.79

c+Hydroxy acids 1190 1550 1.30

TSE = total solvent extractable.

leaves contained lower relative am ounts of 18 :2 ~6 a n d

18:3w 3. This decrease is largely compensated for by a

corresponding increase in the relative am ount of high

M W mon obasic acids (22:0 to 30:O ). The ratios ofsolvent

extractable and bound long chain acids in dead to fresh

leaves (Table 4) suggest some interconversion from solvent

extractable to bound is occurring for this l ipid class. A

similar change is observed for the short chain (C < 22)

fatty acids. T he absence of long-chain acids in the solvent

extracted fraction of the fresh leaves after the wax has been

removed demonstrates their non-involvement in the

membrane lipids.

The major difference between the monob asic acid

composition of the fresh and dead leaves is the marked

decrease in the relative and absolute amo unt of 18:2w 6

and 18:3w 3. The rela tive abundance of 14:O and 16:0

increased dramatically. During leaf decay under oxic

conditions all unsaturated acids present would be

expected to be degrad ed after cellular lysis: the rate being

dependent on the degree of unsaturation.

The presence of a numb er of iso and ant&so branched

acids, 17:lwlO and ~6, cyclopropyl 19:0 along with

higher relative amou nts of 14:0, 16 :0, and 18: lo>7 in the

dead leaves sam ple is indicative of a significant

contribution to the component fatty acids by sedimentary

microorganisms involved in leaf degradation. The

bacterial origin of these acids has been reportedpreviously [ 15 1, which suggests that significant bacterial

colonization of the dead A. mu r i ru z leaves has occurred.

The longer chain monoenoic acids 22: 1 and 24: 1 not

found in the fresh leaf sample and believed to be mainly

the w9-isomers were detected in the dead leaves of A.

ma r in a . The occurrence of these acids in sediments

(thought to be of yeast origin) and M ~~rohn ctrri~~ has been

reported previously [ 16,1 71 indicating that an exogenous

origin for these acids in the dead leaves of A. rn a r in u is

probable.

The absolute amou nts of the long-chain saturated fatty

acids in the dead leaves is increased when com pared with

the fresh leaves (T able 4 ). These acids are probably less

viable microbiological substrates than the short chain

saturated and unsaturated fatty acids as noted previously

[2,3]. The presence of a num ber of C,, and Cl2

polyunsaturated fatty acids not detected in the fresh

leaves, but present in the dead leaves sample indicates that

an alternative source for these acids is l ikely. Marine

dia toms a re r ich in 20:4~16 and 20:5w 3 [18] , however ,

colonization by other microscopic algae e.g., certain

Chrysoph yta [19] could also account for these acids. The

fatty acid distribution of the pneumatopho res is similar to

the fresh mangrove leaves although the relative

concentration of 18:30.1 3 n particular is reduced. Sm all

quantities of 22: 1 and 24: 1 were also detected.

The r,w-dibasic acid composition of A. nzariru isolatedby sapon ification of the leaf residues after solvent

extraction (Table 7) shows di 16:0, di 18:0 and di 18: 1 as

the major components with di 18:2 present at a lower

relative level. The absolute amo unt of the r,w-dibasic

acids in the fresh leaves is 8”, of that of the monobasic

fatty acids. The dead leaves sample showed a similar

diacid distribution to that of the fresh leaves of A. rrrcviuuwith some changes in the minor co nstituents observed.

The relative amo unt of di IX::! was diminished and the

higher M W components increased. Th e absolute am ounts

of the diacids in the dead leaves were 1.8 times that

observed in the fresh leaves and 28 I’ ,>of that of the

monob asic acids in the dead leaves. It was also noted that

the absolute amo unt of long-chain monoacids in the dead

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Lipids of mangrove leaves

Table 5 . Triterpene alcohol concentration of the fresh and dead leaves of Auicennia marina

6 6 3

Co mp o u n d

Percentage composition MS fragmentation m/e (rel. int.)RR,* Fresh leaves Dead leaves M ’ (of TMSi ether)

Unidentified A

Lup-20(29)ene-

38-01 (lupeol)

Olean-12-en-3P-

01 (/I-amyrin)

Urs-12-en-3B-01

(a-amyrin)

Unidentified B

Friedoolean-

3/?-01 friede-

linol)

0 .9 0 4

0 .9 3 7

1 .0 0 0

1 .1 1 0

1 .1 6 8

1 .3 9 1

1.6 2 .7

3 .6 4 .9

11.9 12 .1 498(1 .3) 218(100) , 203(35) , 190(19) , 189(17) ,

204(12) , 109 (7) , 121(7) , 135(7) , 147(7) ,175(7) , 161(4) , 257(3) , 279 (3) , 483(l ) .

17 .6 20 .5 4 9 8 (3 )

57.6 57 .1 4 9 8 (1 9 )

218(100) , 18 9(22) , 190(16) , 203(16) ,

220(16) , 135 (12) , 121(10) , lC9(8) ,

147(7) , 161(6) , 175 (5) , 279(5) , 257(l ) ,

408(l ) .

189(100) , 109(73) , 190(64) , 135(58) ,203(51) , 121 (50) , 218(32) , 147(29) ,

175(28) , 156(27) , 369(21) , 231(16) ,

279(15) , 393(10) , 257(9) , 407(8) ,

299(7) , 483(6) , 245(5) , 325(4) .

N o m a s s spectral data.

498(17) 189(100) , 205(90) , 190(86) , 218(80) ,203(75) , 109(74 ) , 147(26) , 119(22) ,

161(20) , 174(20) , 279(20) , 229(18) ,

293(8) , 257(6) .

7 .7 2 .7 SO O (2 .5 )69(100) , 109 (70) , 123(68) , 125(62) ,

205(42) , 273(37) , 163(33) , 137(32) ,

159(30) , 190(26) , 179(25) , 149(23) ,

246(21) , 231(18) , 302(16) , 217(15) ,

426(15) , 341(11) , 287(6) , 259(5) ,

41 l (5) .

Total absoluteconcn (fig/gdry wt.) 1 0 9 0

* RR, on SE 30, p-Amyrin = 1 .0 .

1 1 3 0

l e aves was increased by a factor of 1.3 compared with the

fresh leaves (T able 4), this factor being the same as that

observed for the total o-hydroxy acids. The high absolute

concentrations of a,w-dibasic acids in A. marina is unusu alsince these acids are generally considered to be mino r

constituents of leaf cutin [20]. The pneumatophores

contained the same diacid components as the A. marina

leaves although di 18: 2 was not detected. The dibasic acid

concentration in the pneumatophores was calculated,

however, to be 1.7 times the monobasic acid

concen tration, significantly different from that found in

the leaves.

The w-hydroxy acid profile of the fresh and dead leaves

of A. marina (Table 8) shows both identical chain-length

distribution and similar relative concen trations of

individual components when compared with the a,w-di-

basic fatty acids of A. marina (Table 7) . These data suggestthe direc t biosynthesis of the a ,w-dibasic ac ids from the o-hydroxy acids in the mang rove A. marina. This hypothesis

has been repor ted previously [21] , as has the oxidativeconversion of monobasic ac ids to o-hydroxy acids [22] .

The tota l absolute amounts of monob asic ac ids in thedead leaves o f A . marina are 53 % of the absolute amounts

found in the f resh leaves, wh ereas the absolute amounts ofboth the so-dibasic and w-hydroxy acids have increased(Table 4) . This observed increase in the absolute level of

diac ids in the dead leaves indicates preferentia ldegradation of the ce llular contents and resultant

enrichm ent of the cutin (obtained by saponification of theleaf residues a f ter solvent extrac tion) and w ax der ivedcomponents .

The chain length distr ibution of the a ,o-dibasic ac idsand w-hydroxy acids in the pneum atophores of A. marina

(Tables 7 and 8) are very similar , as expected. The

presence of o-hydroxy 12:0 and 14:0 in the

pneum atophores but not in the leaf suggests somedifferences in the chain- length specif ic i t ies of the enzymesinvolved. These shor ter chain-length o-hydroxy acids arenot fur ther oxidized to cc ,w-dibasic ac ids. We suggest tha t

the o-hydroxy acid dehydroge nase is specif ic for the C,,and C, , chain lengths in the pneum atophores of A.

marina.

The data p resente d on the lipid distribution in thedecayed leaves re la t ive to the f resh leaves of A. marina

(Table 4 ) show the only signif icant changes to be areduction in the tota l amount of monoba sic ac ids present

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666 G . P. W A N N I G A M A t u l .

SIL 47C NP (47 “/ ‘, cyanopropyl silicone) 43m x 0.2mm i.d.

column [25]. He was used as carrier gas (linear flow: 20cm/sec).

The SE30 column was programmed from 160” to 280” at 2.5” per

mm and the SIL47CNP column from loo” to 240” at 3” per min.

FID detectors were used with injector and manifold temperatures

at 280” and 300” respectively. Monobasic Me esters were

tentatively identified by co-chromatography with authentic

standards and by RR, [26,27] and ECL measurements [28,29].

All lipid components were quantitated by calibrated GC response

and are subject to errors of + 10 T0

Sterol identifications were based on RR, co-injection with

authentic standards and 0~0, oxidation [2.5]. The latter

technique allowed differentiation of the degree of unsaturation of

individual sterols. This is especially important in the separation

of 28isofucosterol and Sa-stigmastanol which had the same R,

on the GC columns employed. The major sterols were confirmed

by GCMS.

Acknowl&ements-The authors thank the ARGC for financial

support. J.K.V. and F.T.G. acknowledge C.P.G. Awards andP.D.N. a University of Melbourne Postgraduate Award.

Professor G. Eglinton FRS, is thanked for access to the NERC

financed C-GC-MS (GR3/2951 and GR3/3419).

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