• Keine Ergebnisse gefunden

IFM-GEOMAR Re� 2002-2004

N/A
N/A
Protected

Academic year: 2022

Aktie "IFM-GEOMAR Re� 2002-2004"

Copied!
6
0
0

Wird geladen.... (Jetzt Volltext ansehen)

Volltext

(1)

IFM-GEOMAR

Leibniz-lnstitut fur Meereswisse st

'IN•

r

,. j.

a n d er U n iv er sit at Kie I Iv O

I

o -:::·

O

'

c

,,....

'1--· ::::

t::. /.�/ � I

IFM-GEOMAR Re�

2002-2004

From the Seafloor to the Atmosphere - Marine Sciences at IFM-GEOMAR Kiel -

lune 2005

(2)

Preface

F

or the first time, the Leibniz Institute of Marine Sciences (IFM-GEOMAR) presents a joint report of its research activities and de­

velopments in the years 2002-2004. In Janu­

ary 2004 the institute was founded through a merger of the former Institute for Marine Re­

search (IfM) and the GEOMAR Research Center for Marine Geosciences. This report addresses friends and partners in science, politics and private enterprises. It gives an insight into the scientific achievements of IFM-GEOMAR and its predecessor institutes during the last three years.

(3)

3.11 New Approaches to the Dynamics of Fishand Squid Populations

M

any exploited stocks of fish and squid un- dergo large fluctuations or extended trends in population size on different time scales, re- lated to environmental changes as weil as to fishing pressure. Therefore, one major aim of fishery biology is to understand the mecha- nisms regulating these stock fluctuations and to develop methods to predict the effects of fishery on exploited stocks and ecosystems in total as weil as the effects of natural environ- mental fluctuations and climate trends on the exploitable production. The complexity of the task is increased by the fact that natural and manmade effects are strongly interlinked and cannot be considered separately. One aspect of crucial importance is the reproductive strat- egy of exploited stocks which is in many spe- cies adapted to a highly variable environment, based on extremely high fecundities and diver- sities in stock structures, which includes the chances for population survival over periods of unfavourable conditions as weil as the devel- opment of large stock sizes under favourable conditions. The regional stock structure, the size and age structure of the spawning stocks, both influenced by fishery, the nutritional con- dition of adults and thus the quality of gametes and the survival of the early life stages related to stock structure, abiotic environment and presence of prey and predators are the key factors determining the reproductive success of a species. One focus of the Research Unit Fishery Biology is to improve the knowledge on the most relevant factors governing the re- cruitment processes in fish and squid stocks by the development of new methodical approach- es, which allow to elucidate the characteristics of survivors during early development and to address also behavioural patterns that provide best likelihood for survival. For this purpose the growthhistory and the chronology of im- portant events during the early development of individual fish have to be considered. This can be supported by analysing the optical and chemical microstructures of fish otoliths or sta- toliths in squids, combined with new methods in survey strategies, drift modelling, biochemi- cal identification of nutritional conditions, uti- lization of experimental results on physiology and behaviour for individual based modelling of survival success. Examples for correspond- ing activities are presented below.

Figure 1: Sprattus sprattus otolith. (a. embryonie phase, b. larval growth zone with daily increments)

Figure 1 depicts an otolith of a larval sprat (Sprattus sprattus). The inner part of the oto- lith refers to the embryonie life phase (a.), while the part marked with "b" corresponds to the larval phase. In this part several rings are easily detectable. Each increment repre- sents one day in a larva's life and consists of a "white" and a "dark" zone. The white zone is formed during phases of high metabolic rates and somatic growth, while the dark zone corre- sponds to resting periods or reduced metabolic activity. Thus, the alternation of both zones reflects typical daily activity patterns. The number of rings provide information on age, and the widths of daily as weil as annual rings reflect individual growth patterns, so that indi- vidual growth histories can be obtained from otolith analysis, which is of special interest for the early larval development. In addition, the trace element composition in otoliths can be utilized to provide information on the ambient environmental conditions like water tempera- ture and salinity, and high resolution analysis techniques allow to relate this information to age and growth based on the ring structure of the otoliths. Thus, otoliths/statoliths can be regarded as an archive recording the life his- tory. Reading this archive, provides important information to identify characteristics of sur- vivers and environmental conditions they were exposed to.

- - - IFM - GEOMAR Report 2002-2004

---~·

(4)

3. Scientific Highlights

10 12 14 16

Number or oncrements (age) 1,8

-&-StatJon 514 - -StatJon 515 1,6 -. . -StatJon 519 ....-. StatJon 521

..R

'E y ....

2: 1.4 I

I Q

" j I I I I

c

.,

E 1.2

/.

,.-

....

.../

4

I

&" 'o--

~ .0/

s 1,0 c

..

"'

:::<

0,8

0,6

6 10 12 14

lncrement number Mean ol lengthclass> 10mm 4.4

4.2 4.0 3.1

3.6

T

3.4

<3.2

T

iS 3.0

~ 2.8

T l

a:2.6

_l

2.4

j_

2.2

T

2.0

1.8

l_

1.6

1.4 Mean

514 515 51t 521 I Stdev.

Station

Figure 2: Comparison of size at age (apparent growth rate within the population, upper panel) and mean increment width (average and variation of in- dividual growth rates, middle panel) of sprat and sardine larvae sampled from a tidal mixing front in the German Bight. Stations 514, 515 represent the mixed water body, stations 519, 521 the stratified water body. The lower panel indicates the mean and standard deviation of the RNA/DNA ratios reflecting protein metabolism as a measure of feeding activ- ity determined from the same larvae caught at the different stations.

Larval Growth and Nutritional Condition in Relation to Environmental Conditions Otolith analysis have been applied to study variations in growth and nutritional condition of fish larvae and the impact of hydrographic features like frontal systems. As an example Figure 2 presents growth rates and a bio- chemical measure for nutritional condition in a mixed population of sprat (Sprattus sprattus) and sardine (Sardina pilchardus) larval sam- pled on 4 stations across a tidal mixing front in the German Bight.

By relating size of the larvae to number of increments (age), the average growth rates within the sampled populations have been de- termined and compared between the mixed and stratified area (Fig. 2, upper left panel) . Highest growth rates were found at the strati- fied water stations offshore. The results from this traditional approach may have been influ- enced by size selective mortality and, as it is based on a single survey and is not following the development of hateh-time cohorts, they also may have been effected by differences in the initial size of larvae. In this case some slight indication is given for a larger initial size in the mixed area.

Using increment width from otoliths provides a measure of actual daily growth rates for those individuals which have survived until the time of sampling (Fig. 2, upper right panel). These data confirm differences in growth among sta- tions with all larvae from one station and the later larval stages from both stations of the stratified water body showing larger increment widths compared to the mixed area. These growth differences were related to higher chlorophyll concentrations and indicate higher abundance of larval food.

The assumption about food availability and consumption as basis for the observed growth differences can be verified by comparison with a biochemical index of nutritional condi- tion measured from the same larvae. Fig. 2, lower panel presents average RNA/DNA ratios per station, reflecting protein metabolism as a measure of feeding activity. These ratios, which relate only to the conditions a short time prior to sampling, show the same ranking among stations as can be seen among the in- dividual growth rates of the later larval stages, confirming the differences in food availability at about the time of sampling.

(5)

the otolith increment width data are pre-

S.mplcd "" IR July Samplcd on 29 July

i •

sented in a standardized form, as devia-

!. 2 tions from the mean over time for each

j i'

1 daily age group. The results presented

~ !:: o ~~t-;:!;iil;~~lliiP.I~~jiif~!i=!j "-"'...,,...--~-'~~-~ in the fig u re in d icate an obvious s h ift in

"Bi

m

.!j !i ·I ~.-...~~'P-'4. the distribution of growth rates per age

l .

2 group towards higher values from one to

~ 3 ... ~ ... u. ... ~~ ... ~w the next survey and thus for the Ionger

S 10 IS ~0 2S 30 S 10 IS 20 2S 30 S 10 1s 20 2s 3o surviving part ofthe cohorts. It illustrates

Agc on 18 Jul)

Figure 3: Standardized otolith increment widths as relative measure of individual daily growth rates, obtained for a popu- lation of radiated shanny larvae sampled at three successive dates. The lines show the 1 ()lh, 5()lh, and 9()lh percentiles of the cumulative probability distribution. Shifts between survey dates in the growth rate distribution per age group indicate size selective mortalities.

that slower growing individuals were ex- posed to higher mortalities during this study, which was most pronounced for the oldest larvae in the period between the first and secend survey and for mid aged larvae from the secend to the third survey. lt could be judged from addi-

Size Selective Mortality

Differences in the average individual growth rates of larval cohorts surviving to a later stage of development may be influenced by mortal- ity again, which complicates the interpreta- tion of growth data, but also allows to identify size selective mortality effects, when the same population of larvae is sampled by repeated survey.

Figure 3 presents an example of results on individual growth from a comprehensive co- operative study on the development of larval radiated shanny (V/varia subbifurcata) in a large bay of Newfoundland. In order to allow a comparison of the variation and shift in daily growth rates for larval cohorts of different age,

Tamperature & ingested prey

1.7 "1.:.0~~---"----~

1.6 1.5 1.4 1.3 1.2 1.1 1.0 0.9 0.8 0.7

0.6

,...,".

0.5

14.500E 15.500E 16.500E 17.500E

lncrement width [J.Im)

tional information that predation was the most important factor, depending in its effect on the distribution of larvae and preda- tors combined with temperature related spatial differences in the growth characteristics.

Identification of Feeding Habitats

Simulations with a coupled biophysical model of the Baltic Sea have been performed in order to enable the reconstruction of the environmen- tal conditions (temperature, prey) sprat larvae had been exposed to du ring their development.

By comparing these environmental conditions with the growth histories of sprat larvae based on otolith increment width, it was possible to define areas where these larvae had encoun- tered suitable feeding conditions. Temperature and prey ingestion have been considered as

lngested prey :..o..;.;...__ _____ .,

14.500E 15.SOOE 16.500E 17.500E

Temp. Norm. lncr. width [J.ImJOC]

0.17 0.16 0.15 0.14 0.13 0.12 011 0.1 0.09 0.08 0.07 0.06 0.05

Figure 4: Horizontaldistribution of otolith increment widths of sprat larvae in the Bornholm Basin in May 2001 (left panel). By separating the temperature effect on otolith growth, highest Feeding success was observed es- pecially in the eastern part of the basin, whereas less optimal feeding conditions could be related to the centre and northern area of the basin (right panel).

- - - IFM - GEOMAR Report 2002-2004

---~·

(6)

3. Scientific Highlights

Sr/Ca

0,01 Atlantlc

0,008 " ' 0,006

•'!

Sr-distribution Eel

0,004 Freshwater

BaHic Sea

l'.,a,.,. ~

0,002

L

I ; -....~ut&

0

~~-

, ,

core <-measuring points -> rlm

Figure 5: Strontium/Calcium ratio of an otolith of the European eel (Anguilla anguilla), caught in Kiel Bight.

driving key factors influencing otolith growth.

As an example, Figure 4 displays the horizontal distribution of otolith increment widths based on the drift and growth history of sprat larvae in the Bornholm Basin in May 2001.

By separating the temperature effect on otolith growth, highest feeding success was identified for the eastern part of the basin and somewhat less for the western part, whereas less optimal feeding conditions could be related to the cen- tre and northern area of the basin.

Detection of Migration Routesand Pathways

The trace element composition of hard struc- tures, such as fish otoliths and Statoliths of cephalopods is influenced by, e.g., ambient water temperature and salinity. Trace element composition in combination with age readings provide a powerful tool to reconstruct life his- tory events and migration pathways of individ- ual specimen.

Presently two different methods to determine the trace element distribution are applied by the fishery biology group in cooperation with geologists: The Synchrotron X-ray Fluores- cence Analysis (SYXRF) and the use of an elec- tron microprobe. In the marine geochemistry group at IFM-GEOMAR, electron microprobe and X-ray Flurescense analyses have fre- quently been applied to investigate, e.g., plate tectonic processes. The excellent micro-scale resolution and the precise analysis of elements from Calcium (Ca) to Lead (Pb) makes SYXRF a very accurate tool to gather life history infor- mation of fish and cephalopods from their oto- liths and statoliths, respectively. Beam-based

eiemental assays can take advantage of the chronological growth sequence recorded in the otolith and are able to resolve different age or date ranges of the animal's individual history.

Both methods are extremely powerful in de- scribing fish migration routes and pathways or the identification of fish nursery areas. Taking advantage of the merger of the former IfM and the GEOMAR Institute, geologists and fishery biologists have now introduced both techniques to address questions related to fish behaviour.

As an example, in Figure 5 the strontium/cal- cium ratio and its spatial distribution from the inner part to the outer margins of an eel's oto- lith caught in the Kiel Bight are displayed. As clear Atlantic, freshwater and brackish signals were detected, this specific eel has crossed the Atlantic during its larval phase, entered fresh- water afterwards and moved further on into the brackish habitat of the Baltic.

IFM-GEOMAR Contributions

Baumann, H., Pepin, P., Davidson, F.J.M., Mowbray, F., Schnack, D., and Dower, J.F., 2003: Reconstruction of environmental histories to investigate pattern of larval radiatied shanny (V/varia subbifureata) growth and slective survival in a large bay of Newfoundland. !CES J. Mar. Set., 60, 243-258.

Hinrichsen, H.-H., Lehmann, A., Möllmann, C., and Schmidt, J.O., 2003: Dependency of larval fish survival on retention/dispersion in food limited environments: The Baltic Sea as a case study. Fish. Oeeanogr., 12, 425-433.

Huwer, B., 2004: Larval growth of Sardina pilchardus and Sprattus sprattus in relation to frontal systems in the German Bight.

Diplomarbeit, Universität Kiel, 107 pp.

Köster, F.-W., Hinrichsen, H.-H., Schnack, D., St. John, M.A., MacKenzie, B.R., Tomkie- wicz, J., Möllmann, C., Kraus, G., Plikshs, M., Makarchouk, A., and Aro, E., 2003:

Recruitment of Baltic cod and sprat stock: identification of critical life stages and incorporation of environmental variability into stock-recruitment relationships. Sei.

Mar., 67 (Suppl. 1), 129-154.

Schröder, J., 2004: Der Einfluss von Umwelt- faktoren auf die chemische Mikrostruktur von Fischotolithen. Diplomarbeit, Univer- sität Kiel, 114 pp.

Dietrich Schnack

Referenzen

ÄHNLICHE DOKUMENTE

As the two techniques are comple- mentary, we have followed both strategies, develop- ing a pool of ocean bottom Seismometers for detailed determination of seismic

The consequence is that sub-surface oxygen concentrations, and the overall partitioning of oxygen between atmosp here and ocean, are sensitive to the rate

We have ex plored the dynamics and predict- ability of the North Atlantic/ European climate variability on multi-decadal timescales initally using an extend ed-range

Second, they demonstrate that nitrogen fixation is co-limited by iron and P in a region where mineral dust deposition is high and iron should be in excess.

T he ocean plays a major role in shaping the Earth's climate, not only because it covers more than 70% of the surface of our planet, but also because of the

The rapid dis- solution rate of carbon-dioxide hydrate implies that in the case of the disposal of liquid C0 2 on the sea floor, the potential to form hydrate will not

est at high northern latitudes. In view of re- cent human-induced environmental changes it is important to assess the response of climates at mid latitudes where the

To further investigate the feedbacks between marine productivity and redox conditions, a new model for the particulate organic carbon (POC), oxygen, nitrogen, and