• Keine Ergebnisse gefunden

maenas to Ocean Acidification

N/A
N/A
Protected

Academic year: 2022

Aktie "maenas to Ocean Acidification "

Copied!
1
0
0

Wird geladen.... (Jetzt Volltext ansehen)

Volltext

(1)

0 100 200 300 400 500 600

control OA low TA OA + low TA

haemolymph ion concentration (mM)

Cl- Na+

K+

Mg2+

Ca2+

20 40

While treatments caused elevated haemolymph levels of cations, [Cl-] were depressed under

normocapnic low TA. The increase in [cations] at mostly constant [anions] reflects a higher strong ion difference under acidified water conditions.

ab a

b a

c d cd d

e

f f f

g h gh h

Bastian Maus, Christian Bock, Hans-O. Pörtner

References

1) Pörtner, H.-O., Langenbuch, M., Reipschläger, A. (2004): Biological Impact of Elevated Ocean CO2 Concentrations: Lessons from Animal Physiology and Earth History. Journal of Oceanography. 60: 705-718.

2) Whiteley, N. M. (2011): Physiological and ecological responses of crustaceans to ocean acidification. Mar Ecol Prog Ser. 430: 257-271.

3) Steffensen, J. F. (1989): Some errors in respirometry of aquatic breathers: how to avoid and correct for them. Fish Physiology and Biochemistry. 6: 49-59.

4)  Gillies, R. J., Liu, Z., Bhujwalla, Z. (1994): 31P-MRS measurements of extracellular pH of tumors using 3-aminopropylphosphonate.

American Journal of Physiology. 267: C195-C203.

5)  Steward, P. (1978): Independent and dependent variables of acid-base control. Respiration Physiology. 33: 9-26.

Contact Bastian Maus

Am Handelshafen 12 27570 Bremerhaven

Telefon +49 471 4831-2198 bastian.maus@awi.de

SEB Annual Meeting Gothenburg 2017

A5.39

Seawater alkalinity modulates the response of Carcinus

maenas to Ocean Acidification

Methods

Shore crabs C. maenas were exposed for four weeks to: 1. control; 2. ocean acidification (1800 µatm); 3. low total alkalinity (TA = 1.1 mM); 4: OA + low TA. Metabolic rates were determined using intermittent flow

respirometers3. Haemolymph CO2 and ion

concentrations were measured through gas-, and ion- chromatography, respectively. In vivo MRI determined heart rate and blood flow, while 31P-NMR spectroscopy was used to measure pHe and pHi from the chemical shift of 3-aminopropylphosphonate (3-APP) and Pi

signals, relative to PLA as an internal standard (below)4.

Anatomical MRI overview slice, including the heart of C. maenas (dorsal view). In the centre of the heart, the entrance to the arteria sternalis is visible. Single gill

filaments are visible, lateral of the heart.

anterior

posterior

systole diastole

A B

C D

Self-gated, flow-weighed MR images of systole (A, B) and diastole (C, D) of

arteria sternalis and heart of C. maenas.

Bruker IntraGate© software detects heart rate non-invasively.

0 1 2 3 4

30 50 70 90

control OA low TA OA + low TA

flow rate (cm s-1 )

heart rate (bpm)

FR HR

ab a

b b

Heart rates were unaffected by changes in

water chemistry, while blood flow in the arteria sternalis under OA was significantly depressed at low TA.

0 20 40 60

control OA low TA OA + low TA

oxygen consumption (nmol min-1 g-1 )

spMR

a SMR

a

ab

b

cd c

d d

Standard metabolic rates and oxygen

consumption rates during spontaneous activity were both significantly depressed under OA, when TA was reduced.

0.27 0.40 0.53 0.80

1.07

0.13

2 6 10 14 18

7.6 7.7 7.8 7.9 8.0

[HCO 3- ] (mM)

pHe

control OA low TA OA + low TA

P(CO2)e (kPa)

C. maenas was able to maintain pHe during

exposure to different acidified water conditions, through actively elevating haemolymph

bicarbonate concentrations.

Results Background

Conclusions

Hypercapnia led to elevated haemolymph

PCO2, but changes in intra- and extracellular pH were compensated for through increased

bicarbonate levels, irrespective of ambient

alkalinity. pH regulation caused an increasing strong ion difference5, possibly elicited by Na+/ H+ exchange or related to NH4+ excretion as acid-base regulatory mechanisms.

Total alkalinity simultaneously affects the

response of cardiovascular activity and whole- animal energy demand under OA. High oxygen consumption rates and blood flow under OA

were significantly depressed under hypercapnic low TA.

The seawater carbonate system does not affect pH regulation, but

hypercapnic low alkalinity depresses cardiac- and whole-animal activity

Decapod crustaceans are thought to compensate for an

hypercapnic acidosis through net uptake of bicarbonate from sea water. Failing to maintain pHe would induce metabolic

depression1;2. We studied the capacity for acid-base regulation in

Carcinus maenas under various conditions of water

physicochemistry and responses of internal acid-base parameters and ion concentration, relating to potential feedbacks on

metabolic rate and cardiovascular activity.

0 -10 -20 -30

10 20

30

chemical shift (ppm)

PLA

AEP Pi γ α β

3-APP ATP

δ (Pi) δ (3-APP)

In vivo 31P-NMR spectrum of C. maenas. Intra- and extracellular pH were calculated from chemical shifts of Pi and 3-APP signals, relative to PLA.

Phase contrasted MRI (dorsal view), depicting haemolymph velocity in C.

maenas. Brightness indicates flow direction and -intensity. The red

arrow highlights the arteria sternalis.

anterior

posterior

Referenzen

ÄHNLICHE DOKUMENTE

A stronger gradient in chloride concentrations between haemolymph and seawater, as it was seen in groups 3 (tab. The maintenance of a high-.. However, activity measurements of

Increasing atmospheric concentrations of CO 2 result in an increased flux of CO 2 into a mildly alkaline ocean, resulting in a reduction in pH, carbonate ion concentration, and

Anthropogenic CO 2 • Seawater acidity • Saturation state • Climate change • Physical carbon pump • Global warming • Biological carbon pumps • Phyto- plankton •

The effect of elevated CO 2 concentrations on the inor- ganic to organic carbon ratio of three coccolithophore species: Emil- iania huxleyi, Coccolithus braarudii and

Downwelling ocean currents carry carbon into the deep ocean (the solubility pump), and play a role in controlling the level of atmospheric carbon. The formation of North Atlantic

For instance, the Symposia on the Ocean in a High-CO 2 World (ioc3.unesco.org/oanet/HighCO2World.html), the Impacts of Increasing Atmospheric CO 2 on Coral Reefs and Other Marine

To help ensure that the ACdi s values were determined on waters moving into the main Indian Ocean basin, mean AC* t values were only estimated from samples north of 35øS

In only a few species has this approach been combined with an analysis of CO 2 effects on metabolism, not only when hypoxia and anaerobic metabolism occur (Reipschläger et al.,