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Petrified Buffalo Hearts, Indian Maiden Breasts, Stalagmites and 70 Million Year Old Worm Poop

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photo of Rosselia Worm

I recently attended the Lieutenant Governor of Alberta Distinguished Artist Awards in Maskwacis, Alberta. I was fortunate to meet Dr. Russ Schnell. He is the Deputy Director of the National Oceanic and Atmospheric Administration, Global Monitoring Division, in the United States. He grew up in the Battle River region and shared a fascinating story about discovering 70 million year old “Rosselia Worm Fossils” in 1958 in the bed of Castor Creek at the confluence of the Battle River.  

Dr. Schnell was kind enough to allow me to publish a story he had written some years ago.  I shot the video of Dr. Schnell as he was telling the story of how the fossils were formed.  

The following story is adapted from the book “Stories from Life: Beauty Everyday As It happens”, 2016, Jane Ross ed., ISBN:978-0-9695841-2-4, Friesens Books, Altona, Manitoba, 325 pages (for a copy contact: Jane Ross <[email protected]>).

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Petrified Buffalo Hearts, Indian Maiden Breasts, Stalagmites and 70 Million Year Old Worm Poop

By Dr. Russ Schnell,  B.Sc., Ph.D., Dr.Sci. (Hons).

It was a Saturday in August 1958.  The summer day was hot up on the open prairie in east-central Alberta. The air was much cooler in the narrow valley, especially in the shadows.  And most of the valley was in shadows from trees growing on the rims above the sandstone cliffs.

The rock was stored in my parent’s garage for 50 years until I brought it to Colorado, USA, where I now live.

About 1:00 PM, the noon wiener roast was over and we had waited the obligatory one hour after eating before going swimming.  Everyone knew that you would get cramps and drown otherwise!  No matter that the water was only 4 feet deep at the deepest, and then only behind the beaver dams.   And that the water was to cold to do much other than dip a few times, dog paddle for 10 feet, then shout out that it was “cold enough to freeze the balls off a brass monkey”1 and splash to shore and stand around a smoky campfire of poplar branches. It was too early in the day for mosquitoes, and even if they had been out, the eye-burning smoke would have kept them away from our tender, lily white bodies. Only our faces, necks and arms were tanned from spending every possible hour outside playing, hiking, swimming and riding bikes over the 20 square mile area of grasslands and creek valleys we considered our “territory”.

On this day, walking in the water bare footed on the bedrock, we would occasionally feel smooth, rounded, tapered stones under the water.   We recovered some of these “stones” which were very heavy for their size and that appeared to be composed of iron.  At least they looked the colour of rusted iron! 

No one seemed too concerned that the sparks from the fire could ignite the surrounding dry grass and possibly spread for miles.  Hey, we were six 9-12 years old boys, friends since toddlers, invincible, girls yet to be discovered, having another boy’s day out along the creek, 2 miles from Castor town.   We stood naked, dripping and shivering, occasionally stirring the fire back to life to keep warm while roasting (flaming) marshmallows on slender willow switches we had cut and peeled earlier on which to roast the wieners.

 1. “Cold enough to freeze the balls off a brass monkey” is possibly an old naval saying. A monkey was a brass plate with holes in which iron cannon balls were stacked. When it got very cold the brass would contract more than the iron cannon balls and therefore the balls would pop out and roll off the brass monkey!  Of course we did not know that then.  We had heard older boys make the “brass monkey” statement when they were around girls who would giggle, so we thought it was “big” to talk like that. 

 Before roasting the wieners, we had played “stretch”, a game where two boys stand facing each other then throw a hunting knife to stick no more than 2 inches to the side of an opponent’s bare foot.  If the knife stuck in the ground and was not more than the allowed 2 inches away, the recipient of the thrown knife moved his foot to touch the blade and then took a turn throwing his hunting knife to stick near the foot of the first thrower.  The game ended when one person’s legs could no longer stretch further apart, and that person was declared the loser.  There were always losers, never winners!    All boys carried hunting knives in hip scabbards that summer.  It was the thing to do.

A more imaginative member of the group said they felt like fossil Indian maiden breasts.

Now, to a pivotal juncture in this story.  One reason we played in this particular part of the valley was that the creek had cut through to bedrock making it easy to cross on a solid rock footing.  In most other stretches of the creek, the bottom was soft mud into which you would sink up to your knees or deeper.   On this day, walking in the water bare footed on the bedrock, we would occasionally feel smooth, rounded, tapered stones under the water.   We recovered some of these “stones” which were very heavy for their size and that appeared to be composed of iron.  At least they looked the colour of rusted iron!  They were conical in shape and every one had a well formed, round indentation on the apex. On the broad end there was generally (but not always) a finger size hole near the centre.  The stones varied in size from a large potato to a small watermelon.

Since we found the heart shaped rocks at the base of a cliff we “knew” was an Indian buffalo jump, some of us thought they were petrified buffalo hearts. Supporting this supposition was the fact that one of the group had found a black, perfectly shaped, sharp, fluted arrowhead near the creek on a sandy path worn by deer coming down the valley wall to cross the creek.  A more imaginative member of the group said they felt like fossil Indian maiden breasts, not that any of us could confirm how a maiden’s breast felt. One such “petrified buffalo heart”, presented upside down, is shown below.

This “petrified buffalo heart” is 8 inches tall and weighs 8 pounds.  It appears to be made of iron but is not magnetic. These fossils wash out of 70 million year old seashore sediments and settle onto bedrock in a small creek in east-central Alberta.  Photo by Ed Ries, Castor, Alberta, 2009.

I took one of the “buffalo hearts” home in my backpack wondering, occasionally, over the hour hike back to town, why I was carrying a rock that was so heavy.  The rock was stored in my parent’s garage for 50 years until I brought it to Colorado, USA, where I now live.

But, I digress from the timeline.  On the hike back to town our ragtag group diverted to look at the body of a dead cow lying in a pasture.  We had discovered it a few days earlier and were interested in looking at it again.  On the discovery visit, the cow must have been dead for only a few days.  It was bloated like an overextended balloon, there were flies buzzing around the mouth, eyes and anus, but otherwise the cow was as if sleeping on its side like a horse.  On this second visit, the carcass was less bloated, but to our great surprise had been completely hollowed out from the rear.

There were no intestines, no lungs, no heart, no stomach, no blood. The interior cavity was dry as dust, the hide was intact and the “roasts” were still on the thighs.  We surmised that coyotes had devoured the soft insides by chewing from the butt end into the body cavity.

Within a few minutes, he printed out a copy of a scientific paper on ancient marine worms that made burrows in the seafloor and left imprints of their existence. 

Before leaving the carcass we convinced, cajoled or otherwise enticed the youngest boy, who wanted to be part of the “big boys” group, to play “coyote” and crawl into the interior of the cow.  He did so to our great amusement as we beat on the hide covered ribs stretched taut like a large reddish drum.  When we returned to the carcass a week or so later, it was picked apart and remnants were being pecked at by magpies. What meat remained was a seething mass of white maggots.

Fast forward 50 years to 2008.  By this time I knew that the conical rock was not a petrified buffalo heart or a maiden’s breast. I was a slow learner!  I was now convinced though that the rock was a stalagmite formed by iron rich water that had dripped onto a cave floor over thousands of years.  I looked on the Internet for similar stalagmites, but did not find any.  Still, sure of my analysis, I wrote a letter to the director of the Royal Tyrrell Museum, Drumheller, Alberta enclosing photos, and described where these “stalagmites” were found and asking how old they were.   I wrote the letter on heavy, expensive looking stationary with an official U.S. government letterhead festooned with gold embossed logos, and signed with a number of titles.  I figured that might get his attention and a response.

A few weeks later I received an email thanking me for the letter and photos, and suggesting that the “stalagmite” was possibly a random iron accretion. Although not a paleontologist or geologist, I still believed that this rock was made by a deliberate, not random process.  After further correspondence, Dr. David Eberth, Senior Research Scientist, Royal Tyrrell Museum, agreed to meet in Castor, Alberta in late June, 2009, and to come to the valley to look at what I still believed were stalagmites.   I flew up from Colorado and David, myself, a sister and 5 friends from Castor proceeded out to the valley now owned by another friend from toddler days.  He took us to an area of the creek where there were many of the “stalagmites” and we each collected a few specimens.  David asked to see an exposed cliff so he could possibly find some of these iron rocks embedded in their natural habitat. Gary Dunkle, the land owner, duly took us to such an embankment and David found a few of the conical rocks imbedded in a loose, grey, alkaline soil in an exposed cliff face.

Then he told us that a world authority on such creatures was Professor Murray Gingras ’95 B.Sc., ’99 Ph.D., Department of Earth and Atmospheric Science, University of Alberta.

To my great surprise, the “stalagmites” were oriented conical point down in the cliff face.  This is not how stalagmites form!  David now lost some of his prior cool composure, as he convinced me that my earlier conjectures were incorrect, that we were looking at a 70 million year old seashore deposit, and these iron accretions had probably once been made by something related to the seashore.

In a humorous throwback to events 50 years earlier, one of the fossils that David had excavated became dislodged and rolled down the steep cliff splashing into the creek behind a beaver dam.  We convinced Eric Neilson ’88, B.Sc. Agriculture and ’09, B.Ed. and now a local school teacher, to wade into the water and retrieve the fossil.  The water was over four feet deep and Eric had to fully submerge to finally locate and recover the fossil that was embedded in silt.  There was no fire to get warm and dry beside this time!

We returned to the insurance and real-estate offices of Dale Emmett, one of the members on this current expedition, where David used a computer to begin looking up something called “Rosselia” on the Internet.  Within a few minutes, he printed out a copy of a scientific paper on ancient marine worms that made burrows in the seafloor and left imprints of their existence.  Then he told us that a world authority on such creatures was Professor Murray Gingras ’95 B.Sc., ’99 Ph.D., Department of Earth and Atmospheric Science, University of Alberta.  Small world!

We departed the office in triumph and sojourned to a nearby bar where Ed Ries, a local rancher and another member of the days’ expedition, bought us a round of beer to toast our success.  While at the bar, Brenda Scott ’73, B.Ed. (sister, also on the excursion) brought out some perfectly preserved fossil snails that she had collected the day prior in a nearby fossil bed. David was quite interested, as these were fresh water snails that rarely fossilize into such perfect iron accretions.  He wanted to know where they are found, but we declined to tell him as only a few members of our family know the location, and we do not want the location to be picked over.  Someday we might show him, but that will be another story.

So how did worms living in the sediment in a 70 million old marine seashore make 8 pound “petrified buffalo hearts?”  First, the worm is not like the garden variety earthworm one finds digging in Alberta garden soil. Instead it was thought be an elongated creature (let us say about one foot long) living vertically in seabed sediment with tentacles that could spread out over the seafloor to capture small organic particle or small creatures touching the tentacles.  A stylized depiction of the worm and its burrow is shown below.

Rosselia worms lived in a burrow at the bottom of ancient marine seashores and captured food with tentacles spread around the entrance to the hole.  They packed their poop into a bulbous structure within the hole.  Eventually the organic material in the poop was replaced with dissolved iron producing the conical imprint shown above.  (Drawing adapted from Masakazu Nara, Rosselia socialis: a dwelling structure of a probable terebellid polychaete,  Lethaia, vol. 28, pp.171-178, 1995.)

The fossilized worm burrow lay at the bottom of the ocean for eons becoming covered by many feet of sediment.

The worm would slide down into its burrow to digest its meals, to poop and to get away from predators.  To accommodate the poop, it would push out the sides of its vertical tube home which was probably easy to do as it was living is soft sediment.  Eventually the worm would die or move on to a new home leaving the organic evidence of its existence within its seabed home.

Now for the rare events that produced the “petrified buffalo hearts” and exposed them for observation today.  At some point 70 million years ago, the organic-rich waste in the worm hole was brought into sustained contact with a freshwater stream carrying dissolved iron compounds.  This iron slowly fossilized the poop and food detritus.  The fossilized worm burrow lay at the bottom of the ocean for eons becoming covered by many feet of sediment.

Eventually the land rose and the fossils were exposed by the Castor Creek that eroded through an uplifted area of the former beach.  Some of the exposed fossils settled on bedrock where they are found today.  Others are still slowly sinking in the muck at the bottom of the creek.

70 million year old fossilized poo from a Rosselia worm found in the Castor Creek near the confluence with the Battle River, September 18, 2019.

The Castor Rosselia fossils are rather rare in that they are well formed, well preserved iron accretions, and in the words of Dr. Gingras in an email to Dr. Eberth and copied to me, he states:  “Rosselia are normally much smaller than the cannon-balls you show”.

And so we come full circle in a small valley in East-Central Alberta; cannon-balls to cannon-balls.

Dr, Russ Schnell

Dr. Russ Schnell, Deputy Director, NOAA, Global Monitoring Division, Boulder, CO

Russ was born and raised in Alberta, Canada and educated at the Universities of Alberta; Newfoundland; Hawaii; Wales; Wyoming and Colorado. He holds degrees in Biology, Chemistry, Atmospheric Resources and Atmospheric Science.

Dr. Schnell discovered biological ice nuclei in 1970 now used in ski hill snowmaking worldwide, and by their removal on plants, prevention of frost damage to -3C. These nuclei are important in precipitation formation with papers from around the globe now being published on the topic.

His research, as Director of the Arctic Gas and Aerosol project in the 1980s, established that Arctic Haze was air pollution from Eastern Europe.  For 7 years he was director of the Mauna Loa Observatory, Hawaii, where the steady global increase in carbon dioxide that forms the backbone of the greenhouse gas atmospheric warming, was established.

He has conducted research on ozone destruction in the Arctic and Antarctic, ozone production from fossil fuel production and on the changing chemical composition of the atmosphere driving climate change.

He has published 125 scientific papers, nine of them in Nature, a premier scientific journal, and holds patents in plant science and biochemistry.

Russ has lived, traveled or worked in 92 countries, and on every continent including the North and South Poles.

In 2002, he received the NOAA Administrator’s Award for his work as director of the Mauna Loa Observatory.

In 2007, Dr. Schnell was recognized as one of the co-recipients of the Nobel Peace Prize as a member of the Intergovernmental Panel on Climate Change (IPCC).

In 2008, he was awarded the U.S. Department of Commerce Silver Medal the highest honorary recognition the Department bestows and in 2011 both the NOAA Distinguished Career and the NOAA OAR Outstanding Science Communicator Awards.

Dr. Schnell’s non-work interests include building wooden trains for children, “Little Free Libraries” for donation and real-estate investing.

He grew up near the Battle River in East Central Alberta. I met him while attending the Lieutenant Governor of Alberta Distinguished Artist Awards held in Maskwacis, AB on September 21, 2019.

President Todayville Inc., Honorary Colonel 41 Signal Regiment, Board Member Lieutenant Governor of Alberta Arts Award Foundation, Director Canadian Forces Liaison Council (Alberta) musician, photographer, former VP/GM CTV Edmonton.

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Alberta

ASIRT investigations concluded on fatal officer-involved shooting involving the RCMP.

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Incident investigation report from the Alberta Serious Incident Response Team (ASIRT)

Introduction

On December 22, 2022, the Alberta Serious Incident Response Team (ASIRT) was directed pursuant to s. 46.1 of the Police Act to investigate a then non-fatal Royal Canadian Mounted Police (RCMP) officer-involved shooting. The shooting of the affected person (AP) was reported to have happened during an interaction with him, as a result of him being a suspect in a complaint of a man with a gun.

While AP initially survived, he died of complications from the shooting the following day.

ASIRT’s Investigation

ASIRT’s investigation was comprehensive and thorough, conducted using current investigative protocols and principles relating to Major Case Management. Information from civilian witnesses, the subject and a witness officers, and importantly video recordings provided sufficient information to determine whether the force used by the subject officer during this incident was reasonable.

Circumstances Surrounding the Officer-Involved Shooting

On December 01, 2022, Maskwacis RCMP received a call reporting that a male [AP] had been drinking and left the caller’s house with a gun. AP was shooting the gun in the country (believed to be the area around the residence). Two RCMP officers responded.

Witness officer (WO) located AP walking on the road with a rifle. AP walked toward WO’s marked police vehicle with the rifle pointed at the vehicle/WO, while WO was seated in the driver’s seat. WO then exited his vehicle with his carbine rifle and moved to the rear of his vehicle while AP kept the rifle pointed at the police vehicle. The subject officer (SO) arrived on scene, but came from the opposite direction. AP turned around and walked toward SO with the barrel of the rifle pointed upwards. SO exited his police vehicle with his service pistol drawn and walked toward AP while he
repeatedly provided verbal direction to AP to drop the firearm. AP and SO were walking toward each other; at that time AP still had the barrel of the rifle pointed upward. As SO and AP got within approximately five meters of each other, AP lowered the barrel of the rifle and pointed it directly at SO. SO fired multiple rounds and struck AP with four rounds causing AP to stumble, drop the rifle and fall to the ground. AP initially survived the shooting and was transported to an Edmonton hospital, where he underwent emergency surgery. The following day, AP succumbed to his injuries.

Analysis

The subject officer was lawfully placed and acting in the execution of his duties in dealing with AP as a person who was the subject of a complaint about him being in possession of a firearm and shooting it off.

The Use of Force

Under s. 25 of the Criminal Code, police officers are permitted to use as much force as is necessary for the execution of their duties. Where this force is intended or is likely to cause death or grievous bodily harm, the officer must believe on reasonable grounds that the force is necessary for the self-preservation of the officer or preservation of anyone under that officer’s protection.

A police officer’s use of force is not to be assessed on a standard of perfection nor using the benefit of hindsight.

With the benefit of hindsight, time for detached reflection and knowledge of the ultimate outcome, it is easy to speculate about how things could have been done differently. That is not the standard, however, against which an officer’s conduct is measured. The question is, applying principles of proportionality, necessity, and reasonableness, whether the force used falls into a range of possible reasonable responses.

Proportionate Response

Proportionality requires balancing a use of force with the action to which it responds. Here, the subject officers were faced with an individual that was armed with a gun and pointing it in their direction. As such, the response by the subject officers in using their respective firearms to shoot AP was proportionate to the threat of death or grievous bodily harm that he reasonably posed to both of them.

Reasonably Necessary

As set out previously in this report, AP presented as a lethal threat to both SO and WO given his actions in pointing his rifle at them. While WO did not shoot during this incident that does not impact the analysis of SO’s actions. Under the circumstances as then faced by SO, no other use of force options were reasonably available for attempted use. The use by SO of his firearm to incapacitate this lethal threat was reasonably necessary. Given the above, the defence available to SO under s. 25 of the Criminal Code would apply.

Conclusion

Under s. 25 of the Criminal Code a police officer is justified in doing what he or she is authorized to do and to use as much force as is reasonably necessary where he or she has reasonable grounds to do so. Force intended to cause death or grievous bodily harm is justified if the officer believes, on reasonable grounds, that the force was necessary to prevent the death or grievous bodily harm of the officer and/or any other person. The analysis under s.34 of the Criminal Code leads to a similar finding that subject officer’s actions were lawfully permitted.

After a thorough, independent and objective investigation into the conduct of the subject officers, it is my opinion that they were lawfully placed and acting properly in the execution of their duties. There is no evidence to support any belief that any officer engaged in any unlawful or unreasonable conduct that would give rise to an offence. The force used was proportionate, necessary and reasonable in all the circumstances.

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Alberta requests more control over provincial immigration system

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Alberta is requesting more control over its provincial immigration to address its skilled workforce shortage, including increasing Ukrainian evacuee participation in the job market.

Premier Danielle Smith has written a letter to Prime Minister Justin Trudeau asking him to re-evaluate his government’s decision limiting the number of allocations for Alberta’s provincial nominee program in 2024. Last week, the federal government informed the province it would only receive 9,750 such allotments – which is the same number of allocations Alberta received in 2023 and is less than the 10,140 for 2024 the federal government had originally allocated.

As of February 2024, Alberta accounts for just under 12 per cent of Canada’s population, but it leads the nation in net employment growth, with 42.8 per cent of the country’s employment gains between January and February 2024. By not providing the requested increase to Alberta’s provincial nominee allocations, the federal government is restricting the province’s ability to keep up with its growing labour market demands, especially as it relates to integrating Ukrainian evacuees into Alberta’s job market.

“Alberta is growing and that is good news. Since January 2023, more than 100,000 new jobs have been created in our province and our employment rate has led the country even longer. At the same time, we continue to experience labour shortages that could be resolved by welcoming skilled workers from around the world, including evacuees from Ukraine, many of whom have the exact skills that our job market most needs. Alberta has long been the economic engine of Canada and we are once again requesting Ottawa respect section 95 of the Constitution and let us welcome the skilled individuals we need into our province on our terms.”

Danielle Smith, Premier

With Alberta’s population growth at levels not seen in four decades, Alberta’s Provincial Nominee Program is best placed to address the province’s unique immigration and economic goals.

Part of Alberta’s population growth has resulted from Russia’s invasion in Ukraine on February 24, 2022. Since that time, Alberta has welcomed a significant number of Ukrainian evacuees to the province. While it is anticipated that many will return to Ukraine following the war, Alberta is also expecting a number of families to apply for permanent residency via the Alberta Advantage Immigration Program. An increase in the number of allocations from the federal government would assist these new Albertans to fill positions in the province’s workforce.

“Immigration is key to Alberta’s ability to address labour shortages and to grow our economy. This limitation imposed by the federal government on our provincial nominee program will be a very difficult pill to swallow, not only for businesses that need this skilled labour but also to the many Ukrainian evacuees who have the skills we need and wish to stay permanently in Alberta.”

Muhammad Yaseen, Minister of Immigration and Multiculturalism

Quick facts

  • The federal government through Immigration, Refugees and Citizenship Canada sets provincial immigration nomination limits. It also approves all permanent resident applications.
  • Alberta maximized its 9,750 nomination allocations in 2023, with a total of 10,029 nominations issued within the federal government administrative buffer.

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