Introduction Directory UMM :Data Elmu:jurnal:S:Soil Biology And Chemistry:Vol32.Issue13.Nov2000:

Stimulation of peptidase activity in nutrient gradients in the Baltic Sea M. Nausch, G. Nausch Institut fu¨r Ostseeforschung, Seestrasse 15, D-18119 Rostock-Warnemu¨nde, Germany Accepted 3 May 2000 Abstract In the Baltic Sea, peptidase and alkaline phosphatase activities always show the same pattern in nutrient gradients: increasing enzyme activities with decreasing dissolved inorganic nitrogen DIN and phosphate. The field experiments reported here suggest that peptidase activity may be regulated by DIN in a manner similar to that of alkaline phosphatase by phosphate. In nutrient gradients established in mesocosms, peptidase activity increased 5- to 7-fold, whereas the alkaline phosphatase activity increased between 29- and 65-fold. Parallel to the enzyme activities, phytoplankton biomass measured as chlorophyll a, organic phosphorus and nitrogen increased, but the closest correlation was found between peptidase and alkaline phosphatase activity …r ˆ 0 : 90; n ˆ 18; p , 0 : 01† : The addition of nitrate, and nitrate plus phosphate, at the time where nutrients were depleted and both enzyme activities were high, did not result in a decrease of peptidase activity. Rather, the peptidase activity was highest after simultaneous treatment with phosphate and nitrate. The addition of 1 mg l 21 alkaline phosphatase caused a 6-fold increase of the peptidase activity after 96 h. Several mechanisms of the stimulation of peptidase activity by alkaline phosphatase are discussed. q 2000 Elsevier Science Ltd. All rights reserved. Keywords: Peptidase; Alkaline phosphatase; Phosphate; Inorganic nitrogen; Extracellular enzyme activities; Aquatic ecosystems

1. Introduction

Studies of extracellular enzyme activities are used to describe the degradation of organic matter in aquatic ecosystems Hollibaugh and Azam, 1983; Azam and Cho, 1987; Billen, 1991; Boetius and Lochte, 1994, 1996; Karner et al., 1995; Martinez et al., 1996 and terrestrial soils Asmar et al., 1994; Bishop et al., 1994; Falih and Wain- wright, 1996; Chander et al., 1997. They are determined by the addition of artificial substrates Darrah and Harris 1986; Chro´st, 1991; Hoppe, 1993; Shand and Smith 1997. The maximum rate of hydrolysis V max of artificial substrates is used to characterise these enzyme activities, and is an indir- ect measure of the quantity of enzymes in the environment. Due to differences in their regulation, in aquatic environ- ments some extracellular enzyme activities e.g. alkaline phosphatase are highest during the intensive phase of phytoplankton growth, whereas others reach highest values during phytoplankton breakdown or at the end of the growth season Chro´st, 1991; Mu¨nster, 1991; Nausch et al., 1998. Different abiotic and biotic factors may influence the synthesis and activity of extracellular enzymes, including temperature, pH Chro´st, 1990; Christian and Karl, 1995, the presence of humic substances Stewart and Wetzel, 1982; Carlsson and Graneli, 1993; Boavida and Wetzel, 1998, oxygen conditions Newman and Reddy, 1993, hydrogen sulphide Hoppe et al., 1990, or UV-B radiation Garde and Gustavson, 1999. In addition, heavy metals Yamada et al., 1983; Kandeler et al., 1996 and herbicides Simon and Bergerova, 1984 can influence enzyme activ- ities in soils. Enzyme stimulation and repression by substrates and end-products are assumed to be the main regulators Chro´st, 1990. However, the interaction of enzymes with their substrates is more complex. For exam- ple, the degradation of proteins by peptidases is not only necessary for the supply of nitrogen, but also to provide carbon. This is how glucose is thought to inhibit peptidase activity Chro´st, 1991; Boetius and Lochte, 1996. Hoppe and Ullrich 1999 proposed similar mechanisms for the regulation of phosphatase activity in the deep sea, where phosphate is available and hydrolysis of organic phosphorus compounds is used to meet the carbon demand of bacteria. In the Baltic Sea, inorganic nutrients are depleted below their detection limits PO 4 , 0.02 mM, NO 2 13 , 0.05 mM during the growth season Nehring et al., 1995. In the central part of the Baltic Sea, where the input from land sources can be neglected, regeneration from organic matter is the main source apart from nitrogen fixation of nutrients Soil Biology Biochemistry 32 2000 1973–1983 0038-071700 - see front matter q 2000 Elsevier Science Ltd. All rights reserved. PII: S 0 0 3 8 - 0 7 1 7 0 0 0 0 1 7 3 - 5 www.elsevier.comlocatesoilbio Corresponding author. Tel.: 149-381-5197-227; fax: 149-381-5197- 440. E-mail address: monika.nauschio-warnemuende.de M. Nausch. to maintain primary production Wasmund et al., 2000. We investigated both peptidase and alkaline phosphatase activ- ity in nutrient gradients in the Baltic Sea, and addressed the question of regulatory factors. It is assumed that peptidases are regulated by the availability of polymeric nitrogen substrates, such as proteins and large polypeptides, and provide low molecular weight compounds for rapid assim- ilation by bacteria Hollibaugh and Azam, 1983; Billen, 1991; Chro´st 1991. However, the influence of inorganic nitrogen on the peptidase activity of pure bacterial cultures is shown by Priest 1984 and was shown in the environment only by Chro´st 1991 in lakes. In contrast, the regulation of alkaline phosphatase in aquatic environments by phosphate availability has been described extensively e.g. Halemejko and Chro´st, 1984; Gage and Gorham, 1985; Paasche and Erga, 1988; Hernandez et al., 1993. We investigated the influence of nitrate, phosphate and alkaline phosphatase on peptidase activity in an attempt to explain the observed behaviour of peptidases in nutrient gradients in marine environments.

2. Material and methods