Sunday, October 1, 2023

ATH 2023 Erindale Park

 This year the hike was abbreviated to an out and return loop from Erindale park to Riverwood and back, a total distance of around 7.5km increasing the approximate length of time of an average stride to about 120 thousand years.  The planned major common ancestor stops which we had plotted on the original hike were replotted by Jerry onto the new map and were remarkably well distanced on the hike.  It gave us time to enjoy the scenic route as well take in all the other activities on the trail and in the river.  The salmon migration had started so the Credit river fishermen were taking advantage of the great weather and the narrow window of opportunity for displaying their catch and release techniques.

This year's theme was 'CARBON - Why should we care about it?'

All life on earth is based on this fourth most abundant element in the universe after Hydrogen, Helium and Oxygen.  It was created in the furnaces of early stars and seeded into the universe by their dying explosions.  Its unique properties lend well to polymer building but also to unique combinations with other elements most importantly for building life studied by the field of Organic Chemistry.  But this property of harnessing the energy of the sun to nourish carbon based life by photosynthesis created a large deposit of energy when ancient trees died and were buried underground for hundreds of millions of years.  Those stores are now being exploited as fossil fuels and the resulting release of stored carbon in the form of carbon dioxide is changing the climate more rapidly than ever before.  The history we will be hiking through is only the most recent connection with this wonderful story of life on earth.  No life, as we know it, would be possible without carbon but that element is now taking a beating in the popular press.

We are still in the process of collating our album of pictures but you can access whatever has been uploaded so far at https://photos.app.goo.gl/1tQ719xLkzLiW1Kf9

Why Is Life On Earth Carbon-Based?

The main reason that life on Earth is carbon-based is because of the unique properties of the carbon atom. Carbon atoms can form strong bonds with other atoms, including other carbon atoms, which allows for the formation of complex molecules like DNA and proteins. Additionally, carbon atoms are relatively small, which makes them ideal for forming the millions of intricate chemical bonds and reactions that are necessary for sustaining life. Finally, carbon is abundant on Earth, making it the perfect element for building life from scratch. Speculation about the existence of extraterrestrial life has been a perennial occupant of humanity’s endless capacity for wonder. To see if there is anyone out there, we sent both Voyagers, not to study a particular star, but to leave our shores and explore other islands in the vast oceans of outer space. Astrophysicists have also wondered (if we do discover one) about the nature of such an alien civilization. If we were to infer the biochemistry of any life form from what we have already encountered, which is well, us, we’d conclude that it would be based on carbon. Carbon, or as science fiction regularly depicts, carbon’s closest cousin, silicon. However, Carl Sagan called this parochial view Carbon chauvinism. He believed that we shouldn’t limit our imagination and ridiculed the assumption that alien life would resemble life on Earth. Still, due to its sheer dominance on Earth, carbon remains our best guess. Given that, what makes carbon so special?

Life Is Complex

Every life form, whether plant or animal, is the embodiment of complexity. The first self-replicating organism evolved more and more complex biological functions by incorporating more and more molecular complexity. Here, complexity refers to fostering millions of intricate chemical bonds and reactions that are imperative to sustain higher forms of life. A primitive life form, such as an amoeba, fosters far lesser molecular complexity than a higher mammal, such as a dog. Molecular complexity enabled the synthesis of functions, such as breathing, excretion, digestion and most importantly, reproduction. None of this would have been possible without carbon. Without carbon, there would have been no DNA, proteins, lipids, sugar, fat, muscle tissue or anything else that makes up the stuff of life. Considering the 118 elements known to man, it’s strange why only 5-6 of them are used to construct organic life. The most common of them is, of course, carbon, dedicated to whose antics is an entire branch of chemistry. It is carbon’s extraordinary thermodynamic and chemical properties that render it so superior to other elements.

Carbon Amiability

A carbon atom has four valence electrons, allowing it to form four single bonds (methane), two double bonds (carbon dioxide) and a triple bond (acetylene, a welding fuel and a raw material for synthesizing plastic). The dominance of carbon, however, isn’t a result of its ability to form these complex bonds, but rather the ease and pliancy with which it forms them. In fact, all the elements residing in the column that carbon occupies in the periodic table possess four valence electrons, but the stability of the bonds they form is incomparable to carbon. Even silicon, the element that resides right below carbon, forms countless molecules, but a double-bonded silicon molecule, unlike double-bonded carbon, is transient – its instability eventually forces it to part into single-bonded silicon atoms. Carbon molecules, such as hydrocarbons, one of the most crucial species of molecules to sustain life, are neither too frail to easily break down, nor too rigid to deter plasticity and adaptability. This allows enzymes to easily manipulate carbon molecules. Furthermore, reactions with silicon aren’t all that efficient; silicon dioxide is a huge molecule (sand), as compared to carbon dioxide, which comfortably exists as a gas. Silicon-based life can’t survive on Earth anyway. Silicon is more reactive than carbon and can form long ‘chains’ of molecules, reminiscent of hydrocarbons, but it will also react violently with oxygen at relatively low temperatures. This means that silicon chains or ‘silanes’ couldn’t have survived within our atmosphere. Carbon-based life also wouldn’t have survived if organisms stored energy directly as hydrocarbons — alkanes are quite flammable themselves (petrol and kerosene), but carbon-based organisms store energy as sugars, lipids, alcohols and other hydrocarbons that exhibit very different chemical properties. All of these properties can be explained by a single statement: carbon is the smallest atom that possesses four valence electrons. Its size renders it the ideal friend to make. Bonds on one branch are unaffected by bonds on other branches. However, life would have been impossible to manufacture if nature lacked the raw materials itself. Carbon is abundant on Earth, so nature couldn’t have missed the opportunity. It leveraged its properties to build life right from scratch!

Thank you to all who attended the hike and to Lynda who made sure our reserved shelter was not usurped by other users of this popular park in Mississauga.

Wednesday, June 14, 2023

Route Overview



 Please see Google Map for actual rendezvous points

Erindale Park - START - 8:00AM - One bya (billion years ago)

Multicellular progenitors of all animal life consisted of Mesomycetozoea:

DRIPs ( Dermocystidium, Rosette agent, Icthophonus & Psorospermium - all protozoan parasites of fish )

Fungi

Amebozoans 


Credit Heights - 8:30am - 900mya - Choanoflagellates

  The Choanoflagellate's Tale is about the evolution of multicellularity. Choanoflagellates are the closest living relatives of the multicellular animals, and can form temporary colonies from a free-living unicellular stage. Sponges have choanocytes, cells that resemble single-celled choanoflagellates, providing an indication about how multicellularity may have evolved.


Burnhamthorpe Bridge - 9:00am - 780mya - Placozoans

The Placozoa are a basal form of invertebrate. They are the simplest in structure of all non-parasitic multicellular animals (Metazoa). They are generally classified as a single species, Trichoplax adhaerens, although there is enough genetic diversity that it is likely that there are multiple, morphologically similar species. Although they were first discovered in 1883, a common name does not yet exist for the taxon; the scientific name literally means "flat animals".


Wellesborough Circle - 9:30am - 630mya - Acoelomorphs

The Acoelomorpha are a disputed phylum of animals with planula-like features that were considered to belong to the phylumPlatyhelminthes. In 2004 molecular studies demonstrated that they are a separate phylum,[1] although their position in the tree of life is contentious; most researchers believe them to be basal among the Bilateria, slightly more derived than the cnidaria. Recent (2011) results suggest that they (along with Xenoturbella) may lie near the base of the deuterostomes.[2][3]

Earlier (2007) work dismissed the phylum as paraphyletic, with Acoela and Nemertodermatida as separate clades.[4]

An ongoing (Feb. 2011) collaborative research project has "the researchers ... confident that they can reach an agreement about where acoels fit in evolutionary history.[2]

Acoels are almost entirely marine, living between grains of sediment, swimming as plankton, or crawling on algae. Acoels have a statocyst, which presumably helps them orient to gravity. Their soft bodies make them difficult to classify.[5]


Creditpointe Dr. - 9:45am - Protostomia - 590mya

Worms, insects (arthropods), crustaceans, barnacles & octopus (molluscs)

 

Protostomia (from Greek meaning "mouth first") are a clade of animals. Together with the deuterostomes and a few smaller phyla, they make up the Bilateria, mostly comprising animals with bilateral symmetry and three germ layers. The major distinctions between deuterostomes and protostomes are found in embryonic development.

Protovsdeuterostomes.svg

In animals at least as complex as earthworms, the embryo forms a dent on one side, the blastopore, which deepens to become the archenteron, the first phase in the growth of the gut. In deuterostomes, the original dent becomes the anus while the gut eventually tunnels through to make another opening, which forms the mouth. The protostomes were so named because it used to be thought that in their embryos the dent formed the mouth while the anus was formed later, at the opening made by the other end of the gut. More recent research, however, shows that in protostomes the edges of the dent close up in the middle, leaving openings at the ends which become the mouth and anus.[1][clarification needed] However, this idea has been challenged, because the Acoelomorpha, a group which forms a sister group to the rest of the bilaterian animals, have a single mouth which leads into a blind gut (with no anus). The genes employed in the embryonic construction of this mouth are the same as those expressed around the protostome mouth, [2]

 

Eglinton Ave.- 10:00am - Jawless hagfish and lamprey - 530mya

Lampreys (sometimes also called lamprey eels) are a family of jawless fish, whose adults are characterized by a toothed, funnel-like sucking mouth. Translated from a mixture of Latin and Greek, lamprey means stone lickers (lambere: to lick, and petra: stone). While lampreys are well known for those species which bore into the flesh of other fish to suck their blood, most species of lamprey are not parasitic and never feed on other fish.[2] In zoology, lampreys are sometimes not considered to be true fish because of their distinctive morphology and physiology. The lampreys are the basal group of Vertebrata (hagfishes are actually not vertebrates, but craniates).


ADMills - 10:15am - Sharks & Rayfish - 460mya

Sharks are a group of fishes characterized by a cartilaginous skeleton, five to seven gill slits on the sides of the head, and pectoral fins that are not fused to the head. Modern sharks are classified within the clade Selachimorpha(or Selachii), and are the sister group to the rays. However, the term "shark" has also been used for extinctmembers of the suborder Elasmobranchii outside the Selachimorpha, such as Cladoselache and Xenacanthus. Under this broader definition, the earliest known sharks date from more than 420 million years ago.[1]

Since that time, sharks have diversified into over 400 species. They range in size from the small dwarf lanternshark(Etmopterus perryi), a deep sea species of only 17 centimetres (6.7 in) in length, to the whale shark (Rhincodon typus), the largest fish in the world, which reaches approximately 12 metres (39 ft). Despite its size, the whale shark feeds only on planktonsquid, and small fish by filter feeding. Sharks are found in all seas and are common down to depths of 2,000 metres (6,600 ft). They generally do not live in freshwater although there are a few known exceptions, such as the bull shark and the river shark that can survive in both seawater and freshwater.[2] They breathe through five to seven gill slits. Sharks have a covering of dermal denticles that protects their skin from damage and parasites in addition to improving their fluid dynamics. They also have several sets of replaceable teeth.[3]

Well-known species such as the great white sharktiger sharkblue sharkmako shark, and the hammerhead sharkare apex predators—organisms at the top of their underwater food chain. Their predatory skill fascinates and frightens humans, even though their survival is threatened by human-related activities.


BarberHouse - 10:30am - Ray finned fish - 440mya

The ray-finned fishes are so called because they possess lepidotrichia or "fin rays", their fins being webs of skin supported by bony or horny spines ("rays"), as opposed to the fleshy, lobed fins that characterize the class Sarcopterygii which also, however, possess lepidotrichia. These actinopterygian fin rays attach directly to the proximal or basal skeletal elements, the radials, which represent the link or connection between these fins and the internal skeleton (e.g., pelvic and pectoral girdles).

In terms of numbers, actinopterygians are the dominant class of vertebrates, comprising nearly 96% of the 25,000 species of fish (Davis, Brian 2010). They are ubiquitous throughout fresh water and marine environments from the deep sea to the highest mountain streams. Extant species can range in size from Paedocypris, at 8 millimetres (0.31 in), to the massiveOcean Sunfish, at 2,300 kilograms (5,100 lb), and the long-bodied Oarfish, to at least 11 metres (36 ft).


Reid Dr. - 10:45am - Lungfish & Coelocanths - 420mya

Coelacanths belong to the subclass Actinistia, a group of lobed-finned fish that are related to lungfish and certain extinct Devonian fish such as osteolepiformsporolepiformsrhizodonts, and Panderichthys.[1] Coelacanths were thought to have gone extinct in the Late Cretaceous, but were rediscovered in 1938 off the coast of South Africa.[2]Latimeria chalumnae and the Latimeria menadoensis are the only two living coelacanth species, which are found along the coastlines of the Indian Ocean and Indonesia.[3][4] The coelacanth has been nicknamed a “living fossil”, because it originally was known only through fossils, long before the first discovery of a live specimen.[1] The coelacanth is thought to have evolved into roughly its current form approximately 400 million years ago.[5]

 Lungfish (also known as salamanderfish[1]) are freshwater fish belonging to the subclass Dipnoi. Lungfish are best known for retaining characteristics primitive within the Osteichthyes, including the ability to breathe air, and structures primitive within Sarcopterygii, including the presence of lobed fins with a well-developed internal skeleton.

Today, lungfish live only in AfricaSouth America and Australia. While vicariance would suggest this represents an ancient distribution limited to the Mesozoic supercontinent Gondwana, the fossil record suggests advanced lungfish had a widespread freshwater distribution and the current distribution of modern lungfish species reflects extinction of many lineages following the breakup of PangaeaGondwana and Laurasia.


Vic Johnsons - 11:00am - Amphibians - 340mya

Amphibians, members of the class Amphibia, whose living forms include frogstoadssalamandersnewtsand caecilians, are ectothermic tetrapod vertebrates whose non-amniote eggs are not surrounded by membranes. Most amphibians lay their eggs in water, with their larvae underging metamorphosis from a juvenile form with gills to an adult air-breathing form with lungs. Some, however, like the Common Coquí frog develop directly into the adult form, while others like Mudpuppies and olms are paedomorphs that retain the juvenile gilled water-breathing form throughout life. Adult amphibians also use their skin for respiration, with some small terrestrial salamanders even lacking lungs.

The earliest amphibians evolved in the Devonian Period from sarcopterygian fish with lungs and bony-limbed fins,[1] features that were helpful in adapting to dry land. They diversified and became dominant during theCarboniferous and Permian periods,[2] but were later displaced by reptiles and other vertebrates. Over time, amphibians shrank in size and decreased in diversity, leaving only the modern subclass Lissamphibia.

The three modern orders of amphibians are the Anura (frogs and toads), Caudata (salamanders and newts) and Gymnophiona (caecilians, limbless amphibians that resemble large earthworms with jaws). The total number of known amphibian species is approximately 7,000.[3] They are superficially similar to reptiles, but reptiles, along with mammals and birds, are amniotes, having impervious membranes that surround the egg. With their often complex reproductive needs and permeable skins, amphibians are often ecological indicators,[4] and in recent decades there has been a dramatic decline in amphibian populations of many species around the globe. The smallest vertebrate in the world is the New Guinea frog, Paedophryne amauensis.[5] The largest amphibian is the Chinese Giant Salamander, Andrias davidianus.[6] The study of amphibians is called batrachology while the study of both reptiles and amphibians is called herpetology.


Streetsville Cemetery - 11:00am - Sauropsids

The concestor of all reptiles (including turtles, lizards, snakes and dinosaurs) and the precursor of birds evolve.

 Sauropsida ("lizard faces") is a group of amniotes that includes all existing reptiles and birds and their fossil ancestors, including the dinosaurs, the immediate ancestors of birds. Sauropsida is distinguished from Synapsida, which includesmammals and their fossil ancestors.

 The cladogram presented here illustrates the "family tree" of sauropsids, and follows a simplified version of the relationships found by Laurin and Gauthier (1996), presented as part of the Tree of Life Web Project.[10]

Sauropsida
unnamed
Anapsida
 

Mesosauridae Mesosaurus BW.jpg

 
unnamed
 

Millerettidae Milleretta BW.jpg

 
unnamed
 

Lanthanosuchidae

 
unnamed
 

Nyctiphruretia

 
unnamed
 

Pareiasauria Scutosaurus BW.jpg

 
 

Procolophonoidea Hypsognathus BW.jpg

 
 
 

?Testudines (turtlestortoises, and terrapinsFlorida Box Turtle Digon3 re-edited.jpg

 
 
 
 
 
Romeriida
 

Captorhinidae Captorhinus BW.jpg

 
unnamed
 

Protorothyrididae* Hylonomus BW.jpg

 
Diapsida
 

Araeoscelidia Petrolacosaurus BW.jpg

 
unnamed
 

Younginiformes Hovasaurus BW.jpg

 
Sauria
 

?Ichthyosauria Mixosaurus BW.jpg

 
 

?Sauropterygia Thalassiodracon BW.jpg

 
 

Lepidosauromorpha (lizardssnakestuatara, and their extinct relatives) Plumed.basilisk.750pix.jpg Coast Garter Snake.jpg Sphenodon punctatus in Waikanae, New Zealand.jpg

 
 



Archosauromorpha (crocodilesbirds, and their extinct relatives) Chinese alligator and rhea.jpgHatzegopteryx BW.jpgStegosaurus BW.jpg


Rivergrove Community Center: 11:45am - 4th extinction 205mya

The Jurassic-Triassic extinction allowed the dinosaurs to flourish and become the dominant species occupying almost every ecological niche on earth.

Triassic–Jurassic extinction event (End Triassic): 205 Ma at the Triassic-Jurassic transition. About 23% of all families and 48% of all genera (20% of marine families and 55% of marine genera) went extinct.[6] Most non-dinosaurian archosaurs, most therapsids, and most of the large amphibians were eliminated, leaving dinosaurs with little terrestrial competition. Non-dinosaurian archosaurs continued to dominate aquatic environments, while non-archosaurian diapsidscontinued to dominate marine environments. The Temnospondyl lineage of large amphibians also survived until the Cretaceous in Australia (e.g., Koolasuchus).


Rivergrove Community Centre 11:45am Monotremes join - 180mya

 This rest stop is the last opportunity to use the washrooms. 

Monotremes (from the Greek μονός monos "single" + τρῆμα trema "hole", referring to the cloaca) are mammals that lay eggs (Prototheria) instead of giving birth to live young like marsupials (Metatheria) and placental mammals (Eutheria). The only surviving examples of monotremes are all indigenous to Australia and New Guinea, although there is evidence that they were once more widespread. Among living mammals they include the platypus and four species of echidnas (or spiny anteaters); there is debate regarding monotreme taxonomy (see below).

 4th Major Extinction - Jurassic/Triassiac - 205mya

Triassic–Jurassic extinction event (End Triassic): 205 Ma at the Triassic-Jurassic transition. About 23% of all families and 48% of all genera (20% of marine families and 55% of marine genera) went extinct.[6] Most non-dinosaurian archosaurs, most therapsids, and most of the large amphibians were eliminated, leaving dinosaurs with little terrestrial competition. Non-dinosaurian archosaurs continued to dominate aquatic environments, while non-archosaurian diapsidscontinued to dominate marine environments. The Temnospondyl lineage of large amphibians also survived until the Cretaceous in Australia (e.g., Koolasuchus).

 

Britannia Rd. 12:00n Marsupials join 140mya

Marsupials are an infraclass of mammals living primarily in the Southern Hemisphere; a distinctive characteristic, common to most species, is that the young are carried in a pouch. Well-known marsupials include kangarooskoalas,possumsopossumswombats and the Tasmanian devil. Marsupials represent the clade originating with the last common ancestor of extant metatherians. Like other mammals in the Metatheria, they are characterized by giving birth to relatively undeveloped young, often residing in a pouch with the parent for a certain time after birth. Close to 70% of the 334 extantspecies occur in AustraliaNew Guinea, and nearby islands, with the remaining 100 found in the Americas, primarily inSouth America, but with thirteen in Central America, and one in North America, north of Mexico.


RiverRun Park 12:15p Laurasiatheres join 85mya

Laurasiatheria is a large group of placental mammals believed to have originated on the northern supercontinent ofLaurasia. It includes shrewshedgehogspangolinsbatswhales, most hoofed mammals, and carnivorans, among others.