|The Dark Decay Assay was not discovered through one moment of inspiration but through stepwise exploration of an idea that had a good chance of succeeding. This chapter shows how. Once a workable method transpired, it was used to explore the environment, leading to more discoveries but also to paradoxes that simply meant that there was still more to discover and to understand.|
|Simplification of the plankton ecosystem. A pH meter leads the way but initial measurements are disappointing. How the DDA was discovered. Hydrogen ions escape. Minimising hydrogen ion losses. Natural pH of the sea.|
|A standardised method could be achieved only by stabilising temperature. By elevating the temperature somewhat, experiments could be shortened considerably, saving both time and effort while also increasing accuracy.|
|A failed linearity experiment showed that completely decomposed samples decomposed further when a small amount of energy food was added. This reminded us of the laws of thermodynamics that complete decomposition is not possible without addition of a high quality fuel.|
|Vial size and type are important as the bacterial activity is easily disrupted.|
|In any test which is intended to povide quantitative data, it is important to know the relationship between the measured and the actual quantity. Ideally such a relationship is linear, meaning that there exists a one-to-one correspondence between the two. We encountered interesting difficulties.|
|For those who visit the sea under water, visibility is an important indicator of water quality because the environment becomes poorer when visibility decreases. Visibility may enable us to estimate the biomass of the producers.|
|The DDA measures decomposer activity, of which the first three days are the most decisive. The rate of attack (RoA) is one of the most important outcomes, correlating well with degradation but results show inexplicable variability.|
|What is the quality of the water around Northland? Do the measurements make sense? Do we need more measurements?|
|Because freshwater lakes are not intensively interconnected like the seas, their DDA curves are quite variable and indeed specific to each lake. Results show that acidic lakes can accommodate higher densities of plankton.|
|If samples can be kept in storage without loss of information, it would be beneficial to the accuracy of the method and it would also be easier to obtain samples from people who do not do the actual measurements.|
|Inside aquariums of no more than one litre, one can grow a plankton ecosystem until long-lived algae begin to grow on their walls, but even then the biomass inside remains what matters.|
|Plankton in eutrophied environments is often growing at maximum densities, leaving excess nutrients unused. These can be measured by diluting the sample and growing plankton or other plant matter. But there are problems.|
The Dark Decay Assay was not discovered by accident. It followed on from observations of decay underwater and the subsequent discovery of the missing ecofactor, the planktonic decomposers. There had to be a way to measure these and the only instrument capable of measuring such low concentrations had to be an accurate pH meter.
|It is common knowledge that scientific research on plankton has been rather disappointing, hampered by an ever changing mix of thousands of species and millions of individuals, ranging from viral particles less than 0.2µm to just visible zooplankton of 2mm, a range of over 4 orders of magnitude. The only real progress could be expected from far-reaching simplification of the whole, as shown in this diagram. The three arrows represent the three main groups of life. The producers (green) make long biomolecules with hydrogen bonds, thus scavenging hydrogen ions from the surrounding water: the pH goes up. The food chain (orange) burns these biomolecules with oxygen while also storing for growth: the pH changes little. The planktonic decomposers (brown) break down wastes and dead bodies by breaking the biomolecules and their many hydrogen bonds: the pH goes down. Although this is very much an oversimplification of all the processes taking place, it sums up its essence.|
|The simple idea is to measure the pH of the sea and if the pH is high, the producers rule, which is good. If the pH is low, the decomposers rule, which is bad. When measuring the actual pH in the sea around the North Shore peninsula of Auckland, New Zealand, a range is found from 7.62 in a brackish upper-estuary creek to 8.13 at the East Coast beaches. It corresponds roughly with what we would call the quality of the water, from bad to good. Thus by going further out to sea, much higher pH values should be found but they seem to level off at 8.20. Yet there exists an enormous difference between the fauna found at remote islands, compared to that found here at the East Coast beaches.|
|It comes to mind that the differences in salinity may have caused the observed differences in pH, and when these are plotted, a clear relationship emerges. So what are we measuring? What is THE pH of the sea anyway?|
|Surprisingly, a clear relationship is found between turbidity and initial pH. Turbidity or poor visibility has always been a good indicator of water quality, and finding this relationship is encouraging but unfortunately not very useful.|
When measuring three points in the Manukau Harbour where Auckland's sewage is discharged after treatment, it was clear that initial pH could not be used as a measure of water quality. At French Bay inside the harbour we measured 8.06 while we could see and smell that the water there was very polluted, to the extent that oysters, eelgrass and sea lettuce could no longer live there. At Cornwallis, halfway to the entrance, the water was of much better quality and the shores showing more life as well at a pH of 8.16. But at the entrance the pH slumped back to 8.07 with visibly much better water, allowing even mussels (Perna canaliculus) and stalked kelp (Ecklonia radiata) to grow. In a high tide rock pool we measured a pH of 8.74. It became clear that the pH meter was able to 'see' things we could not see but that it was rather useless to measure water quality with.
On the way home, while making a stop for an icecream, the DDA idea was born. It was obvious that in the sea the producers were able to push the pH up while at the same time the decomposers were pulling it down, resulting in all kinds of possibilities. It occurred to me that we should exclude the producers so that the decomposers could be measured. This could easily be done by placing vials in the dark so that the phytoplankton would immediately cease activity and eventually die, but the vials had to be sealed in order to keep all chemicals inside. The resulting effect was large and meaningful as the graph shows. At French Bay the decomposition rate is indeed highest, followed by Cornwallis Beach and then the entrance at Whatipu. The pH of the rock pool also dips to meet the final pH of the inner harbour. The water at the entrance does not decay as much as that of the inner harbour and final pH could well be a proxy for the total biodensity in the water.
|To test whether decomposition had completed, we exposed the vials to light again with varying results. After a small immediate recovery, pH remained either constant or decomposition set in again. So what were we really measuring?|
|To prove that the effect was caused by life, a slight quantity of formalin (formol, a 35-40% solution of formaldehyde CH3.COH) was added. Even one drop (~0.07ml) of formaldehyde (40%) was sufficient to halt decomposition. Sample A was taken from a reasonably healthy harbour, whereas sample B originated from the backwaters where salinity was also much lower. The formol curves slowly creep towards pH=8.1, the natural pH of seawater, as bacterial activity has been halted.|
From two decades of careful observation, we knew that the area around Cape Brett had the clearest coastal water found around Northland, New Zealand. Samples taken here showed a great deal of variation with varying rates of decomposition. While travelling over patch R, we noticed that the smell of the seawater had changed, and stopped to take a sample. It turned out to be rather unusual but more in line with what we had expected of all previous samples. First the living plankton must die before rapid decomposition can take place. However, in all previous (and future) samples we found high chronic decay right from the first measurement.
We named this plankton assemblage powerplankton because of its
ability to transfer the solar energy straight into the food chain without
measurable losses: there is no measurable chronic decomposition (no left-overs
for the bacteria). We now posit (propose, assume) that the powerplankton
was once abundantly available, powering the once bountiful coastal fisheries.
Its loss has led to weak fish stocks that are easily overfished. But the
discovery may go one step further, explaining why fisheries worldwide have
entered a critical phase, even where managed extensively. Fishermen report
that fish are dying from starvation in seas green with chlorophyll. It
is a paradox that may now have been solved. Of course further confirmation
loss of hydrogen ions
In order to study the rate of loss of hydrogen ions, vials from two batches were opened. Within hours their pH jumped up, equal to a rapid loss of hydrogen ions, most likely caused by escaping decomposition gases like carbondioxide CO2, hydrogen sulphide H2S, dimethyl sulphide (DMS), methane CH4 and others. In the end, all samples converged on the same pH, which we named natural pH or the intrinsic pH of the sea. Such rapid loss of hydrogen ions was a little unexpected and made us aware that the DDA method needed to be improved in order to minimise losses caused by opening the vials for measuring.
pH and salinity
In the beginning we observed how initial pH and salinity were somehow related, and we wondered how much this was supported by measuring the natural pH of the sea by first decomposing a sample fully and the ventilating it to equilibrate with the air. It is an experiment taking two weeks for full decomposition, followed by a full week of ventilation. In the meantime some water has evaporated, which needs to be replenished with distilled water, which in turn upsets pH somewhat. Two experiments were done showing very little difference from pH=8.1 over a range of realistic salinities. Note that natural fresh water has a large range of natural salinities, depending on the geology of their catchment areas and volcanic vents. For more accuracy a larger number of experiments is needed.
|site||pH, day 0||pH, day 13||natural pH, day 20||final salinity ppt|
|Lucas Creek High||7.73||6.99||8.11||31.9|
|Lucas Creek Low||7.67||7.14||8.12||20.5|
|Minimising hydrogen ion losses
A number of experiments were done to investigate the best ways to minimise hydrogen ion losses. The size of the gas bubble above the sample proved to be of critical importance. During the experiment, but particularly towards the end, gases equilibrate into the bubble such that their partial pressures are equal to those in the liquid. At the moment the sample is opened, these gases escape and upon completion of the measurement, the new air bubble is slowly charged again with escaping gases.
Because the DDA tests depend entirely on microbial activity, it is also very sensitive to temperature and fluctuations thereof. An affordable portable incubator which could be powered from both 12 Volt DC and AC mains power was not available, so we decided to construct our own by modifying a commercially available Peltier-effect car fridge.
Our modifications entailed a mechanical thermostat whose bulb connects to the inside of the box. Also a small rechargeable emergency battery was mounted to protect against power breaks, and whenever the unit is disconnected from a power source. This has proved very helpful inside cars that switch their cigarette-lighter power off when parked. The modifications have proved effective and enabled us to standardise the procedure such that measurements done in one time and place can now be compared with those done elsewhere. But it also gave scope to elevate the temperature for the following reasons:
|This graph shows two temperature experiments conducted simultaneously at constant temperatures of 21ºC and 27ºC. The six degree difference suggests that one should find the cold sample lagging behind by about a factor of two. In reality the outcome depends also on what is in the sample and it also shows that accuracy deteriorates when the duration of the experiment is extended. Note also that alcohol enhancement after day 5 delivers inconsistent results.|
A failed linearity test with agar added to expired water gave the paradoxical results shown in this diagram. The quantities of the test solution, a diluted agar, were chosen such that in a log-log graph a straight line should result (1,2,4,..,256 drops). But what we really measured was a renewed decomposition initiated by agar as energy food. Although the highest concentrations of agar gave fastest response, even a single droplet was sufficient to achieve the same a few days later. What was going on here?
The problem with diluted fuels like agar and sugar is that they eventually
rot or ferment inside the bottle. They are also difficult to calibrate
and administer. We therefore resorted to ethyl alcohol, the most basic
of all fuels. A poison to higher organisms, it can effectively be converted
by bacteria and its effect is direct and drastic. From a 90% pure solution
a 20% solution was made by adding 3.5 parts of double-distilled water.
|The first laws of thermodynamics
1. Energy can neither be created nor destroyed. Thus all forms of energy ultimately convert to heat.
2. All physical processes lead to a decrease in the availability of the energy involved. This defines that all energy conversions such as photosynthesis and decay are accompanied by intrinsic losses. Some of these losses are due to the energy being used by organisms for the sake of living. Other losses occur from the thermodynamic conversions of one energy (a hydrogen bond, e.g.) to another.
The ecological consequences of this discovery are rather fundamental and important and require further study. In our thinking about closed nutrient loops within ecosystems, we must now also account for the energy deficit in the decomposition paths. Somehow from somewhere an additional energy must be provided at a stage that it is needed and not just consumed.
With these thoughts in mind, we decided to add alcohol in an advanced
state of decomposition but long before exhaustion was reached, on day 5
of the experiment. Several experiments were conducted to compare the old
method with the new.
the profound effect of alcohol enhancement was discovered, we asked ourselves
whether old experiments could be corrected to fall in line with the new
ones. Was the energy deficit threshold a fixed percentage and was it consistent?
In the scatter diagram a number of typical types of water were plotted,
but not all because many were almost duplicates. It turned out that the
West Coast water (90-100%) did not need much alcohol enhancement, whereas
east coast water does (20-40%), particularly that associated with clear
water (10-25%). The Seafriends aquariums showed erratic results because
its water quality was changing (prograding) rapidly (See aquarium
Paradoxically, the East Coast water shows much larger biodensities than the West Coast water, which can not yet be explained.
|Discussion - the slush
From the freshwater lakes we discovered that a large proportion of biomass is occupied by decomposers when lakes are eutrophied. Because these lakes are also more acidic, making hydrogen ions easier to scavenge, their phytoplankton productivity is correspondingly higher. But the sea with its high and rather constant natural pH of 8.10 paints a different picture.
From the day/night rhythm produced by freshwater lakes, we see that a pH of 8.1 is a rather limiting ceiling. From this we suggest that in the sea the scarcity of hydrogen ions forms a serious limiting factor.
The above scatter diagram shows that the clear water of the outer shelf leaves up to 90% of its biomatter undecomposed. In these areas the pH is also higher. So there is a large amount of undecomposed biomatter complete with unavailable nutrients, for which we coined the new word slush (as in half molten snow). So the sea does not only have phytoplankton (the old way of thinking) but also a great deal of decomposers (the new way of thinking) and now also slush. Decomposers cannot decompose this slush because an additional fuel is not available.
The slush hypothesis suggests that this is nature's way of preserving nutrients (they may float up due to long fatty molecules) but plants able to provide a high energy fuel can reach these nutrients with the help of (friendly) decomposers in their surface slime. As the slush is decomposed, the plant gets primarily hydrogen ions it craves for, and as a bonus nutrients as well. Thus this mechanism enables marine plants to grow much faster within a hydrogen ion starved environment. And as the pH increases in the clearer waters, so does the amount of slush!
It is remarkable that the West Coast water near Auckland behaves quite different, suggesting that it incorporates little slush as it decomposes nearly fully and rather quickly as well. This can not yet be explained.
Reader, please note that the slush hypothesis is very speculative but if one does not think outside the square, one misses the most important things to be discovered.
|Vial size and type
We may have been lucky in our choice of vial because other types do not respond as well to dark decay. The graph shows two separate experiments, done ten days apart with water from the same origin (solid lines vs dotted lines). Our Fuji film container is about 30ml, made from high density poly ethylene (HDPE). One would say that a larger vial would yield more accurate results as it averages over a larger quantity and one could make it such that a very small air bubble remains. However, vial size should have no influence on how the ecosystem inside develops, although the relative amount of wall surface may have an effect. Two different sizes of transparent PVC of 200ml (dark blue curve) and 400ml (light blue curve) did not respond to dark decay, with no difference accounting for vial size. It appears as if volatile substances in the PVC halt decomposition. However when after day five some alcohol was added (1 drop per 10ml), the decomposition proceeded to the same point as reached by the 30ml HDPE vial. Ironically, the largest vial did not reach the proper ending pH, perhaps through hydrogen ion losses or needing more alcohol
A glass vial of 220ml was part of the test (grey), and it too gave poor results. Why the larger PVC and glass vials were unsatisfactory, cannot be explained. Fortunately the much smaller vial works and this saves space in incubators.
We also tested the amount of alcohol required by two separate experiments (thin green curves and green dotted curves) for 1, 2, 4 and 8 drops per 30ml vial. The amount of alcohol had no significant influence over the results even though the sea water used had a biodensity of over 500 hion because of local sewage spills.
In any test which is intended to povide quantitative data, it is important to know the relationship between the measured and the actual quantity. Ideally such a relationship should be linear, meaning that there exists a one-to-one correspondence between measured and actual quantity. Our preliminary explorations of freshwater lakes gave good evidence of stunning precision and linearity over four orders of magnitude, but a clean experiment would settle any doubt. The test is really very simple: just add known quantities to pure solutions and measure the results. However, a plethora of difficulties has to be overcome.
How does one obtain pure sea water without organic matter (virgin natural water)? All sea samples and all sea salts are contaminated with organic matter. We even had difficulties obtaining pure fresh water. Even a biomedical supply company sold us purified water as distilled water, even though this purified water had very high concentrations of minerals and organic matter! It wasn't even suitable for topping up batteries! Eventually we purchased our own distiller and produced our own double-distilled water but this introduced other problems.
For salt water we resorted to expired water of which all organic matter has been decomposed, but this had its own problems and led to the discovery of alcohol enhancement as explained above.
We obtained pure sea water from the island state of Niue where we measured the underwater visibility at 60m, but surprisingly, even this clear water contained high biodensity.
|Biomass and visibility
Divers know that the visibility of water is strongly correlated with water quality, as the environment becomes poorer (degrades) when visibility decreases, even when sediment deposition by mud does not play a role. This is really a contradiction because increased densities of phytoplankton should be beneficial for the food chain, resulting in better opportunities for life. The Plankton Balance hypothesis and the Dark Decay Assay now provide the answer to this paradox.
|Degradation of the underwater environment is mainly caused by the presence of decomposers which increase their numbers suddenly as plankton becomes denser. To get a grip on these issues, we measured visibility whenever possible and plotted it against biomass in a log-log scale. The conceptual diagram shown here gives an idea what is to be expected. Plankton responds to two main environmental factors: availability of nutrients and availability of light. Where nutrients are in short supply, the water clears and plankton biomass follows an inverse relationship: double the biomass and visibility will halve. Towards very murky waters, soiled by mud, plankton biomass follows a light-limited relationship: halve the visibility and half the biomass can be maintained by sunlight. The data points should thus fall inside the green boomerang which has a maximum somewhere in the middle. Where the two lines cross cannot theoretically be predicted and must be established from many sets of actual data.|
diagram (which may need another one since alcohol enhancement) shows how
the theoretical expectations are by-and-large met by the actual data. The
idea is that the biodensity of phytoplankton lies on the green lines. What
is found to the left of it represents light obstruction without biomass
and what is below it, the biodensity other than that from producers. If
this is true, the decomposers can increase suddenly at about 9m viz, but
this does not happen predictably.
The grey cloud we named the graveyard, as it is associated with (non-living) biomass accumulating at the surface without being visible. The graveyard was found only in areas with relatively deep clear water, in late autumn. The dots' colours correspond to the areas shown on the map, which allows one to see how they are grouped.
Note how the biodensity, calculated from initial and ending pH, is plotted upside-down on a logarithmic scale which is very similar to the pH scale. A new unit is proposed, the hion which is the biodensity corresponding to the number of hydrogen ions in a pH of 9.00. One day the hion will be accurately linked to biodensity in micrograms per litre of dry organic matter or carbon. However, when using the DDA it is not important to know this.
biodensity = ALOG( - final pH ) - ALOG( - initial pH) in ppb as hionsWork is continuing on this interesting aspect of the DDA, particularly now that complete decomposition can be achieved by alcohol enhancement. Please note that meaningful values for visibility can be obtained only rarely, during prolonged calm dry weather, low wave energy and neap tides, while taken from a boat, at least several hundred metres from the shore. Meaningful visibility in estuaries can be measured only after prolonged dry weather during neap tides.
|Rate of Attack
Due to temperature stabilisation, decomposition curves can be compared. To our surprise, hardly any showed the shoulder typical of powerplankton, as all suffered from ever-present chronic decay. The rate at which initial decomposition happens can be measured as the Rate of Attack (RoA). It has been standardised at 48 hours for the following reasons:
|As we knew how important water visibility is to the quality of the environment, we were interested whether this also showed in the measured rates of attack. This graph plots both in a log-log relationship, visibility horizontally and RoA in hion vertically. For comparison the linear relationship is drawn as the green dash-dotted line. The colours correspond to the areas shown on the map. Note how the various plankton assemblages neatly group together although with large differences between them. One can say that the rate of attack increases as visibility decreases and that this is much less so in clear water where the curves flatten out. Also a sudden increase is seen between 5 and 10m viz. Note that these measurements were done before alcohol enhancement but that this should not affect these results. We found a very similar relationship for freshwater lakes.|
expected the rate of attack to be related to decomposer biomass and thus
to total biodensity. The idea is simple: the more bacteria, the steeper
their attack. The graph shows horizontally the relative rate of attack
as a percentage of biodensity and vertically log biodensity. The colours
correspond to the assemblages in the previous graph. The only certainty
obtained from this relationship is that low relative RoA is rare
and high relative RoA happens at the West Coast and that most relative
RoA is between 10% and 20% of biodensity. With some imagination one
can even say that relative RoA declines as biodensity increases.
Note that these results may ned to be reinterpreted with the introduction of alcohol enhancement because that affects total biodensity and this scatter diagram will be upgraded in due time.
By mapping the results, we could obtain an overview of what the DDA says about water quality in an area we know well from frequent diving. The map shows the results of measurements done mainly between March and May, late summer to autumn when water quality is at its best. But remember that it is but a snapshot in time and does not reflect average conditions. Much more sampling needs to be done throughout the seasons. Even so, results look promising as they also correlate to degradation observed under water. For a complete report visit map01.htm.
showing both RoA (in red) and biodensity (in green), one can get an idea
of the situation. None of the sites shows powerplankton. Healthy
plankton has RoA= 5 to 10 over biodensities of 30-60. Sick plankton
has RoA between 10 and 30 and killer plankton RoA over 30. (see
above) Maximum biomass is less than 100 hion and where it exceeds this,
raw sewage must be suspected. Using these criteria, one can see that the
seas around Northland are rather sick, sufficiently degraded to affect
The West Coast suffers from the runoff from a large area to the south of this map, which flows through the Waikato River into the sea where 100/238 is marked. Also the (treated) sewage from one million inhabitants flows into the sea from the Manukau Harbour where 69/160 and 54/154 have been marked. These are extremely high RoAs and biodensities that make life impossible for a vast range of species. In the Far North also very high biodensities are found, which cannot be explained from local runoff and we suspect that West Coast water flows northward, around North Cape and then back southward along the east coast. This also needs further investigation.
Please note that the biodensities shown here may need to be reinterpreted because of the improved technique of alcohol enhancement. However, the charted rates of attack (red) remain valid.
Further mapping is needed and also further out to sea and all around
Because freshwater lakes are not intimately interconnected like seas, their DDA curves show high variability, and are indeed specific to each lake. The minerals and acids of a lake depend largely on the geology and land use of its surrounding catchment area and also on the presence of volcanic vents. Freshwater lacks the salt of the sea that makes sea water much less solvent. As a consequence, fresh water can store higher concentrations of nutrients and minerals and produce much higher plankton biodensity than seawater. All this shows clearly in DDA tests.
this single graph 24 New Zealand lakes have been brought together. It shows
that the DDA has a proven range from pH= 5.5 to 9.5, over four orders of
magnitude, which is quite outstanding for a measuring device. The curves
can be compared with one another because all have been incubated at a constant
elevated temperature of 27ºC but alcohol enhancement had not been
invented yet. At the conclusion of each curve, the vials were opened (while
still in darkness) to ventilate in order to establish the natural pH
of each lake. For some curves this has been drawn as the upward segment
ending in a large dot. The DDA curves are full of surprises and paradoxes,
some of which touched upon here.
Most lakes show very high rates of attack and high biodensities. Only in Lake Tarawera and Taharoa (a dune lake in the north) is the powerplankton found. Fishermen say that the trout there are fat and healthy, unlike those in the other lakes. Lakes Rotorua and Rotoehu show a rise in pH before decomposition sets in, perhaps because they are so shallow that the bottom (benthic) decomposers dominate.
For completeness we also measured the crystal-clear spring water of Hamurana Springs, that flows out into Lake Rotorua. It had a very slight hint of peat (we tasted it) and measured a biodensity of 93 hion of what is almost certainly non-living organic matter. We cultivated this water to estimate its mineral/nutrient content and the DDA curve of this aquarium is shown in Ea, measuring 405 hion. Thus even very clear streams can contribute large to the nutrient budget of a lake. Lake Rotorua had biodensities of 578 (north) and 1030 (city)! The Blue Lake due to its volcanic vents is rather acidic and supports nearly 2000 hion biodensity! All very surprising results, opening a world of interest. For the table of results see fresh01.htm
the rate of attack (over 48 hours, green) is plotted versus biodensity,
an almost straight line results (green), implying that bacterial attack
rate in 48 hours is a constant part (27% at 27ºC) of the measured
biodensity but much less for low biodensities. (Note that the black dash-dot
line gives precise linearity) This is the relationship we expected to find
for saltwater, but it has eluded us so far because marine plankton ecosystems
are more complex.
The straight-line relationship suggests a kind of normality for lakes, that bacterial activity (and thus their biomass) is a fixed part of biodensity. Some lakes deviate from the 'rule'. Pupuke, Rotoma (roadside) and Quarry have lower than expected bacterial activity, whereas the rather clear dune lake Taharoa has a higher one.
of the amazing results of the lakes expedition is the discovery that the
maximum biodensity a lake can carry when it is fully eutrophied, is a function
of its natural pH. The lower this pH (the more acidic the lake),
the higher biodensity the lake can carry. It appears that the availability
of hydrogen ions is what matters to the maximum density of life in water.
In the graph we have named the lakes that deviate from the eutrophication
line as these are perhaps not fully eutrophied. The crystal clear water
of Hamurana Springs (30m viz) is of course exemplary but its cultured aquarium
falls inside the line. All named lakes are known to be of high quality
and even Rotoiti on both sides falls just left of the line. Note that lakes
Tarawera and Pupuke who stand out by their low rates of attack, are still
in a precarious state on the eutrophication line.
Note also that the sea (East Coast natural pH=8.12; Westcoast = 8.03) falls neatly in place on this graph with Murrays Bay dipping far below the line because of a massive ingress of raw sewage. The ultra-clear water of Niue plots very high above the line.
What the graph suggests is that a water body's maximum biodensity is limited by the value of its natural pH. The question remains whether this natural pH is determined by nutrient concentrations from nitrates and phosphates. In other words, is the eutrophication state of a lake given by its natural pH? For the moment, the maximum biodensity follows this equation:
maximum biodensity = ALOG( 1.55 - natural pH ) hion, where the factor 1.55 needs further confirmation.The idea behind this graph is that lakes cannot overstep their maximum biodensity as given by the eutrophication line and the above formula. Any nutrients in excess cannot be used (but we have not measured these). It is worrisome that even our clearest lakes are close to being fully eutrophied and the situation in the sea is worse still in many places.
|By plotting biodensity versus visibility, it was hoped to find a relationship. One would think that in still lakes the amount of phytoplankton can be derived from measured visibility, and that the data points would be located along two conceptual lines (reciprocal relationships like y=x and y=1/x), one for nutrient-limitation and the other for light limitation. That Waahi, Waikato and Waikare lie most left of the centre is caused by the amount of sediment in these waters. Because the data is coherent in other aspects, one cannot escape the conclusion that most of the biomass in the eutrophied lakes is made up of decomposers. The thin V-curves indicate decomposer levels of 2, 5 and 10 times that of the producers. In order to sustain such high decomposer levels, the producers must be correspondingly more productive. This seeming paradox needs further investigation.|
placing the one litre 'aquariums' in light by day and darkness by night
at room temperature, we observed spectacular growth and decay in a single
day and night, after which the day-night rhythm disappeared. When plotted
against natural pH (on right), it reveals that phytoplankton growth indeed
follows the relationship discovered before for biodensity. Thus slightly
acidic lakes indeed maintain large biodensities of decomposers through
their sheer productivity by day. But this situation is not without risk
as the experiment shows. In the end the decomposers won and the lake in
the 'aquarium' died. It shows that lakes maintaining high levels of decomposers
can suddenly die by a combination of external factors such as a run of
dark days or a sudden warming.
Remarkably, three lakes scavenged hydrogen ions up to the magical ceiling of pH=8.1 which may well be an overall limit. Ironically, the natural pH of the sea is also 8.1 and most samples taken during a day are not far from that level. It suggests that a pH above 8.0 is limiting plant growth.
Freshwater planktonic ecosystems are perhaps easier to study because they are rather similar with low numbers of species. Because of this the relationships between biodensity and RoA and the natural pH of freshwater bodies became evident whereas in the sea it eluded us. Even so, the relationship between the clarity of the water and biodensity seems a paradox.
Our conclusion would be that in the nutrient-limited part of the graph (right-hand side), the difference between the red datapoints and the green dash-dot line represents decomposer biomass and perhaps a little of unknown dissolved organic material. The observation that bacterial activity (RoA) is proportional to total biodensity, except for those lakes with low biodensity, supports this. Is bacterial behaviour inside our vials different from that in situ? They are obviously more aggressive due to the higher temperature, but would their numbers have increased too? This is unlikely as their food source has not changed, except for the phytoplankton dying after 24-36 hours. From the graph one can see that the biodensity of phytoplankton is a small part of the total as most lakes have 2 to 10 times more decomposer biodensity than producer biodensity. Would it mean that Taharoa, Blue Lake and Rotoma have higher productivity to match this, even though they have very different acidities? When the initial pH is related to the natural pH, expressed in hions (see table in fresh01.htm), one can see that in most lakes the producers can keep up with the decomposers. But lakes Rotorua (-212 to -676) and Rotoehu (-225) cannot. Surprisingly, clear dune lake Taharoa (-305) also fails in this respect. The crystal clear Hamurana Springs water (-320) also fails because it has not seen the sunlight for years.
The day/night rhythm experiment reported above indeed indicates that phytoplankton productivity depends on the availability of hydrogen ions and that it can achieve amazing rates of growth during the few hours of daylight to match the decomposers' rates of attack which continues unabated day and night.
In order to find answers to these puzzling paradoxes, the freshwater lakes series is continued by resampling for every season. Results are reported in freshwater studies (1) (fresh01.htm)
|Keeping in storage
If samples could be kept for a while without losing their information, it would be easier to obtain them from helpers. One could go out in a boat for one or more days, take samples here and there and these could be measured later. Using this technique, one could place the samples in the incubator all at the same time which would make the calculation of RoA easier too. It would also be beneficial in case a previous experiment had not quite finalised.
graph shown here gives the general idea. Samples were taken from a one
litre aquarium on days 0, 1 and 6, but these measurements date from a time
before temperature stabilisation and other improvements. The main question
is: can a plankton ecosystem be kept, and if so, for how long? What one
often forgets is that one of the most important environmental factors affecting
plankton is that it knows of no walls. Plankton organisms live all their
lives without ever encountering a wall. It means that macro algae and thread
algae cannot survive, because they need something to attach to. Once attached,
these longer-lived algae take over, changing their environment, like raising
the pH as they successfully scavenge hydrogen ions in competition with
the short-lived phytoplankton.
The graph follows an aquarium for over two weeks, and after one week the pH rises. It can rise to 9.5, we noticed, as the plankton ecosystem gradually changes, behaving more like a rock pool.
order to test how well samples keep in a one litre jar, a sample of eutrophied
seawater was taken and over a period of three days two vials were taken
from it each day and subjected to the DDA. In the graph these have been
lined up on day one, and in order to synchronise at 'day 13', all samples
were treated to two drops alcohol on days 11, 12, 13, shown here as a single
The curves show that initial pH first goes down, then up again, but this depends on the amount of sunlight experienced through the window the jar was placed before, at ambient temperature. The results have been summarised in the table below. It suggests that samples can be kept for a few days without seriously affecting the outcomes. So it is possible to have assistants collect water samples during one day, to be tested that same evening or the next day. It is necessary, however, to store the samples in a light, cool place.
Note that alcohol at day 12 is not a good strategy as it introduces uncertainty. It is better to administer the alcohol between days 3 and 5.
It is hard to believe that a sample taken from a lake or sea, looking very much like a glass of clear drinking water, represents a fully operational ecosystem with thousands of species and millions of individuals. Most of these are sub-microscopic and their collective biomass rules when eutrophication (over-feeding) is neared.
One would think that plankton can be grown from a sample of sea water, but this is not entirely true as the composition of life inside a jar changes and short-lived planktonic organisms are replaced by longer-lived sessile ones. In a professional microbiology laboratory one can isolate a monoculture of phytoplankters and cultivate these in a suitable medium under sterile conditions such that decomposers and sessile algae are eliminated, but this does not resemble the plankton ecosystems of the sea.
The method of growing plankton and/or micro algae is very useful to
determine the potential biodensity from free nutrients. The clear water
is contaminated with a few drops of salt or fresh water to introduce species,
and left to incubate in daylight in an open container to let carbondioxide
in. Evaporated water is eventually replenished by distilled water. After
3-4 weeks all nutrients will have been converted to biomatter and this
can be measured using the DDA. In this manner one can measure nutrient
concentrations in units meaningful to life (hions).
As a matter of interest, we have been successfully growing an entire but simple ecosystem inside a one litre peanut butter jar. It consists of phytoplankton, sessile algae and bacteria. In it swim a dozen or so hardy brine shrimps and many eggs and babies. This ecosystem-in-a-bottle is hermetically sealed and its lid glued in place, such that it cannot be opened accidentally. It has been living in a cool place of the garden, in half sunlight since January 2003. Whenever we teach about ecosystems, the bottle is paraded on top of the overhead slide projector and children have to figure out how my pets live from sunlight and never need to be fed. Ideally, every classroom should have one.
Did you know the answer? In a true ecosystem everything is recycled. The brineshrimps need food and they eat the planktonic algae which you can see in the top as a green soup. The food provides them the building blocks for growth and the energy for swimming. But they need oxygen too, which is also provided for by the plants. But the plants need carbon dioxide, which is what the shrimps breathe out. And they need nutrients. These come from the shrimps' wastes which are converted by bacteria to nutrients and carbondioxide. So, all minerals and oxygen are recycled. The only thing needed from the outside is sunlight for the plants to grow. So, in effect, the shrimps live from sunlight (and so do the plants, and the bacteria).
|Diluting for nutrients
The DDA cannot measure free or unused nutrients in heavily eutrophied waters or where fresh water mixes with salt. But a sample can be diluted with virgin water and then left to grow until all nutrients have been used up. Once that has been achieved, the once free and excessive nutrients converted to biomatter, can be measured with the DDA.
We are looking at using salt water from a place where nutrients and
biomatter are indeed very scarce in order to continue these kinds of experiment.
It could also teach us more about how degraded fresh water mixes into clear