Thursday 29 August 2019

Some August updates and oddments

I have added some photos and comments to the Swans and Eel Grass post.

There is a heavy crop of Caladenia catenata along Karbeethong Rd near Genoa Rd.  This close up of the labellum of one of them is nice.
Going back on the 29th I got some decent photos of a double flowered C. catenata (I noticed about 4 such specimens out of at least 200 plants) ....
 ... and finally a good shot of a very pink specimen (still with a yellow tip to the labellum).
On the heathland walk we saw our first Stackhousia monogyna on 28 August.

 Also an open Hakea decurrens 'nut'.
On 30 August we went to Gipsy Point to see if we could find a walk there.  In fact there was quite a nice walk from the boat ramp by the lodge along a Peninsula.
The only real photo op was this Yellow-tailed Black-Cockatoo  peering round a tree!
Much of the vegetation seemed to be introduced stuff that had escaped from gardens!  We went back to the cemetery to see if there were any orchids visible (expecting it to be too early.  So it was: 1  Caladenia catenata was the total!

It seemed very dry but we did see quite a few Drosera

Wednesday 28 August 2019

Pebbly Beach

A member of the Mallacoota Weather and Wildlife Facebook group posted about the great crop of Caladenia catenata on the track to Pebbly Beach.  So we took ourselves off there and found it to be really good.  Here are some photos.

Hardenbergia violacea
An example of Caladenia catenata.  The biggest group was at least 40 plants and my guess would be over 100 scattered through the bush.
Acacia longifolia is colouring the entire bush.
Acacia verticillata
On getting to the beach we were greeted by a single Hooded Plover
I peered closely at these Cormorants, but could only get 2 Great and 2 Little Pied.  Not all shags on rocks are lonely!
Leucopogon parviflorus
Monotoca elliptica 
Alyxia buxifolia
Leptospermum continentale
Some guys from the Shire were out fixing up wind damage.  They are doing a fine job, but didn't get over the bridge to deal with this one!
Between the bridge and the fallen tree were a good crop of Pterostylis nutans (some were in fact under the fallen tree)...
,,, and a specimen of P. melagramma (there were more of these in the bush near the Caladenias).
I think there were also some P. pedunculata there but the mosquitos drove me off before taking the photo.  (An alternative is that they were in the bush at the top where another couple we met had photographed them.)

Monday 26 August 2019

Swans and Eel grass


In recent discussion of the numbers of Black Swans
... seen on the Mallacoota Inlet it was suggested that one factor leading to reduced numbers of Swans, compared to the very large flocks seen in the past, was the loss of eel grass for them to feed on.   This seemed like an interesting suggestion so I have researched the topic using the resources I have available.

Cutting to the chase, the answer is that it is a possibility, but the consequent question is what caused the eel grass to go away?  I have included some results from overseas articles about Brent Geese, which also feed on eel grass in the Northern Hemisphere.

What is eel grass?

According to Wikipedia it is either Zostera muelleri (salt water) or Vallisneria sp (a mainly tropical, fresh water genus).   I think the latter is disqualified as we aren’t in the tropics and the Inlet isn’t fresh water!

Looking at the Atlas of Living Australia (ALA) there are records for Zostera muelleri in the Inlet, but not enough records to make any statements about change in abundance.

I think this is Eel grass:
That collection was on the edge of the Betka River, where Swans were grazing.  I assume these blades were bits that the swans dropped.

What do Black Swans eat?

The short answer is vegetation.  Commentary in the Handbook of Australian, New Zealand and Antarctic Birds (HANZAB) suggest that while invertebrates are found in the gut contents of Black Swans this is most likely by-catch rather than targeted feeding.

The details given in HANZAB are from examination of contents the oesophagus or gizzards of birds from fresh water sites.  It seems that a fair proportion of the food is pondweed (Potamegeton sp. or Azolla sp.) which is not found in the Inlet.  The Cyperaceae (reeds) are also important.

Possibly more relevant is research in New Zealand[1] and Western Australia[2].  Both of these refer to the Black Swans feeding on Zostera. 

The focus of the NZ work is on whether the grazing by Swans is responsible for declines in Zostera abundance – the answer seems to be probably not, at least not on its own.

The WA work also includes 2 other sea grass species Ruppia meagcarpa and Halophila ovalis  The former seems to have also been recorded in the Inlet (and the Betka River where a flock of Swans have been resident for some time).  It appears that in WA, other things being equal, the Swans and the sea grasses keep a balance between grazing pressure and survival of the sea grass.  It is noted that the presence of algal blooms may upset this balance so that the grass cannot recover from the grazing.  I’m not aware of any algal blooms affecting the eel grass in the Inlet.

Unlike some species of ducks Swans do not dive, but feed by upending
This means that they can only feed where the water is shallow enough for them to reach the food resource. This limits them to sites where the water depth is 1m (+ the height of the food).  That being the case it is interesting how far out in Bottom Lake is that shallow.
The red circles are feeding Swans.  My guess is at least 200m off shore.

Comments from other species

The mention of Eel grass jogged my memory back some 60 years when concerns were expressed that warm water from a proposed nuclear power plant may adversely impact the eel grass at Bradwell in the UK, where it was an important Winter food source for an endangered subspecies of Brent Goose.  Reading two articles about Brents suggests some additional reasons for the decline of  eel grass. 

An article from the WWT[3] (Peter Scott’s organisation) from 1969 discusses this in detail.  Interestingly they comment:
 “The latter [Zostera sp.] was the preferred plant when, in the 1930s, it was attacked by a mysterious disease associated with, if not caused by, the mycetazoan Labyrinthula. Over the whole of its Atlantic and Pacific range the beds of Zostera were wiped out. “ 
They go on to describe how the plant has slowly and (to 1969 at least) incompletely recover. Reference is also made to the control of hunting as a factor in survival of the subspecies of Brent Goose that overwinters in Essex, especially in its Arctic breeding grounds.

Another article[4] discusses a world wide view of the relationship between Brents and eel grass.  As well as the fungal infection mentioned above, increased turbidity or eutrophication are suggested as reasons for reduced Zostera meadows.  Since the area around the Inlet is National Park these reasons seem unlikely to apply here.

What has happened to the Swans and Sea Grass in the Inlet?

Following publication of my article in the Mallacoota Mouth summarising this post I have been contacted by a long term resident of the area who can remember - more than 10 years ago - seeing the Goodwin Sands black with Swans, and large flocks flying overhead.  He considered the estimates of 3500 and 4000 quite believable.

In my informant's opinion they used to feed on sea grass which was abundant in the Inlet,  However when the Inlet was artificially opened the position of the outlet was such that it allowed the sand, which naturally washes up the beach to flood into the Inlet and cover the sea grass, killing it.  In his opinion the number of Swans has not recovered form this event.




[1] Dos Santos, V. (2011). Impact of black swan grazing and anthropogenic contaminants on New Zealand seagrass meadows (Thesis, Doctor of Philosophy (PhD)). University of Waikato, Hamilton,
[3] Brent Geese, mudflats and Man M. A. OGILVIE and G.V.T MATTHEWS (1969)
[4] Barbara Ganter; Seagrass (Zostera spp.) as food for brent geese (Branta bernicla): an overview

Saturday 24 August 2019

Summer comes to Bastion ...

... the day after a Winter storm!  I am judging it is Summer as we felt warm in the afternoon, and a Curlew Sandpiper was on the sand.  {I have put this image first so that it appears up front in any Facebook links.)
The sea wasn't quite as rough as it appeared, from Facebook posts, to have been yesterday, but there were good swells running and lots of white water.  It was running well up the beach.
And breaking attractively over the breakwater.
We had gone to the beach in the expectation that there would be interesting marine 'stuff' washed up.  However it seemed that either it had been flung far up the beach or sand had been washed in too, to cover it.  This coloured jellyfish (or part thereof) was an exception.
A less well lit view of the Curlew Sandpuper.
After strolling around it had a rest with some Red-capped Plovers.
Going round the mouth and on to the flats a large area of shells was visible.  I suspect this was due to scouring by the high water on the previous day.
Compared to recent days the water was covering a wide area on this visit.  (I had checked the gauge in the morning and it was about 0.3m , compared to a lowest reading of -0.15m a few weeks back.)  One outcome of this was the loafing terns were much closer.   I estimated 160 Crested Terns and 49 Australian Pied Oystercatchers.
A lone Caspian Tern was also present.
A splinter group of Pied Oystercatchers.
A lone Sooty Oystercatcher about to give some beak to a washed up limp of cunjevoi.
Two of the 5 Bar-tailed Godwits.
The Curlew Sandpiper again, this time including a Double-banded Plover in its companions.
We decided to return along Develings Inlet to minimise the risk of tromping on a Plovers nest but found the ground to be a bit soggy.  Presumably this was due to the high water the previous day.  As we headed back towards the beach we had a good view of a female White-fronted Chat ...
.. and a less good view of a male.
This next image is included to show the damp sand indicating where the waves broke over during the storm.  I'm not sure it does that very well!
A whelk - or at least gastropod - egg mass,
We went to the breakwater hoping to get some spectacular images of waves breaking but the big sets seemed to have gone elsewhere.  Also, Frances noted that they seemed to coming from two directions so not landing with full force.

Friday 23 August 2019

Draftiness and its aftermath

Wednesday 21 August and Thursday 22 August were a bit windy.  My weather station (in a relatively sheltered position) recorded a total wind run of 273 km  on Wednesday and 278 km on Thursday.  To put them in context they are the 6 th and 5 th longest runs I have recorded since firing up the station in February this year.  The longest run I have recorded was on 2nd March.

It has been suggested that some explanation of the meaning of wind run would be good.  It doesn't get a mention in the BoM Glossary but other sites have the following suggestions, which between them get the idea across:

  • It is a measure of the amount of wind in a period;
  • It is the average wind speed per recording period multiplied by the number of recording periods; 
  • It is a bit like the trip meter in a car, which measures the number of times the wheels go round and multiplies it by the circumference of the wheel telling you the distance you have traveled. For wind run is is the number of revolutions of the measuring device x the circumference of the device.

This graph compares the wind runs on the three dates.
Another way of assessing the windiness is to look at the maximum gust recorded.  This next chart shows the maximum gust x hour for the three days discussed above.
So which day was the windier?  
  • Looking at the wind run chart, it is clear that 2 March wins.  This is backed up by ranking each hourly reading (1 = biggest value) with 2 March clearly having the highest average rank (1.04) and the 2  days in August being similar at 2.42 and 2.33.  
  • For maximum gust the pattern is confused in the chart and only partially clarified by looking at the ranks.  2 March and 21 August are close with average ranks of 2.04 and 2.00 while 22 August is somewhat better with an average of 1.79.
An advantage of the maximum gust is that one can look at BoM data for that, while they don't show current data for runs in their free material.  Here are some numbers for the three dates (NB: as Blogger doesn't make nice with tables, this is an image so the data can't be copied as such).
In case  you wonder where Hogan Island is, wonder no more.
I scrolled West from Hogan Island, and the next non-trivial amount of land is s few km South of Buenos Aires - so the roaring 40s are a little North of their range.

This windiness leads to an amount of damage to trees etc so it was good to see a team of arborists out tidying things up this morning.  (They had been out and about yesterday as well.)


Well done that team!  Not everyone was feeling that energetic!