Showing posts with label Water Quality. Show all posts
Showing posts with label Water Quality. Show all posts

Tuesday, November 18, 2014

The Wonderful World of Diatoms

November 18, 2014 0


I admit that I ended that last post a bit unclear. But diatoms, it should be said, aren’t (or, rather, shouldn't be said since I shouldn't use double negatives. Ah, well.).


http://tmagazine.blogs.nytimes.com/2014/09/16/diatomist-film-matthew-killip-premiere/?_php=true&_type=blogs&smid=nytcore-ipad-share&smprod=nytcore-ipad&_r=0
Not physically, that is; you see, diatom cell walls are made of silica (glass), and that feature is actually incredibly important (not to mention gives rise to beautiful 'micromanipulations' like this one by Klaus Kemp - different colors in part because of different thicknesses of their glass). Diatoms arose between 180 and 225 million years ago – youngsters in the algal world (compare that to the geezer cyanobacteria of 3+ billion – way vintage) – and in so doing utilized an under-used, widely available resource that set them apart. The genealogy (or “systematics”) of diatoms has since expanded to include anywhere from 20,000 to over 1 million species that span almost every aquatic or semi-aquatic habitat imaginable – oceans, lakes, rivers, moss, soil. In those habitats they can be suspended in the water column, anchored onto plants or rocks, and moving through the soil. And the species diversity of diatoms is mirrored by their physical diversity: some are round (‘centric’ – shaped like a barrel), others needle-like (‘pennate’), others bent or otherwise contorted (‘yogis’ – don’t quote me on that, though! Those are really just rebellious pennates), all of them in a variety of shapes and sizes. They are unicellular (just like, say, a red blood cell. Only they can be just as small as a red blood cell [~7 micrometers] or over 20 times as large!). Their glass cell walls are adorned with tiny holes in very distinct patterns, glass thickness varies, spines might protrude, a slit used to move may vary in shape and placement. And what’s cool is that you can use all these miniscule features to differentiate species based on appearance alone – quickly and relatively inexpensively (with the right training and tools – mostly a good microscope and a literal library of reference material. I hope you know German, though [the language of some of the best reference texts]!). So the take-home is that diatoms can be identified based on species’ unique cell wall ornamentation (a Who’s Who Among Diatoms in American Rivers and Lakes, if you will. Now that's a taxonomy textbook title!), and that allows us to figure out who’s where and why.
Tom-ay-to, tom-ah-to.

And understanding who’s where lets us use diatoms as very dependable indicators for ecosystem changes. Diatoms are sensitive and like what they like (what's that on the Myers-Briggs Type Indicator? ISFP?). They often fill very specific roles in their communities, and if something happens to the environment – changing temperatures, physical disturbance, nutrient enrichment – then the diatoms, and other algae, are among the first to respond. So you can catch the effects of, say, agricultural runoff into a lake early on if you look at how the algae changes. And arguably the best algae for noting that change is the diatoms because of their diversity, ID-ability, and preservability. Because glass tends to linger in most conditions we can even take a soil core of that 'polluted' lake and examine the diatoms from years past to then model and understand what past conditions were like! Their cell wall ornamentation is preserved, allowing us to still identify their dead ‘shells’ (properly, “frustules”) – a natural preservation that we replicate in the lab by killing modern diatoms so we can look at just their glass frustules to make identification easier. Talk about bio-indicators (and cruelty to diatoms). And that diversity within and among habitats allows us to use diatoms to answer some very fundamental ecological questions involving metacommunity diversity and microbial dispersal and biogeography (I know, I know: those will be discussed in entirely separate posts to come).

And I’m just getting started (“Oh, no,” you’re thinking.). I’ll be quick. Going back to the uninformative reasons of why they’re awesome, some clarification. Diatoms alone produce around anywhere from 25 to 40% of Earth’s oxygen and are large carbon sinks (translation: they gobble up that pesky carbon dioxide and give us oxygen, free of charge. So generous!). They produce oil droplets that are delicacies for primary consumers (as well as nutritious – think Flintstones gummies good) – and they have potential to be used for biofuels (they’re trying to squeeze the oil out of them. Literally.). When they died off en masse thousands of years ago (diatom genocide! Where was the UN?!) their graveyards eventually became reserves of  


(or diatomaceous earth), which is great if you like clean teeth (as an abrasive) and beer (as filters) and don’t like ants in your house (natural pesticide). But even when they’re alive some species secrete vast amounts of 'mucus' around them that invite all sorts of other creatures (mainly bacteria, fungi, and/or other algae) to party and form a biofilm, which have even more ecosystem benefits (outside of making you fall on your face in a lake)! Imagine coating yourself in your own snot and letting stay anything that wants to use, eat, or add onto that snot (not quite a perfect example of the intricacies, but what a vivid picture for the general idea! That makes the "affectionate" term of "rock snot" for biofilms of the diatom Didymosphenia geminata even apter, eh?).

Didymosphenia geminata biofilm
I realize that all of this may be a little too general to be overly informative, but my hope is that it piques your interest in learning a bit more about diatoms – whether scientist or enthusiast. In the Everglades we’re using diatoms to look at ecosystem-scale effects of sea level rise on the Everglades. Diatom indicator species of nutrient enrichment are used in assessing the efficacy of Everglades restoration and conservation. We see poignant applications of diatom science right here in South Florida that are visible all the way up to reports to Congress! (Mastogloia smithii Goes To Washington, anyone? Though Sylvia Lee may have something to say about that nomenclature!)

But in all this excitement about diatoms it’s important to recognize algae as a whole. Cf. T. jeffersonii (invalid, illegitimate, and insane taxonomy?) doesn’t agree with discrimination, remember. So to rectify this miscarriage of algal civil rights, stay tuned for the next installment of the Wonderful World of Algae! (Will there be death? Will there be destruction [of tasteful writing, yes! Of algae…?]? Will there be adorable pictures of sea otters on an Everglades research page? Find out next week!)

This blog post was written by Nick Schulte, a Master's student in Evelyn Gaiser's lab at FIU.

Thursday, September 11, 2014

Okeechobee or Okoboji? An Everglades Student’s Corny Tale

September 11, 2014 0

This post was written by Nick Schulte, a Master's student in Evelyn Gaiser's lab at Florida International University. 

So where would you go to study how Everglades algae respond to increased nutrients from sea level rise? The Florida Everglades, right? That’s what I thought. But I went to Iowa.


Iowa Lakeside Laboratory, more specifically, on the shores of Lake Okoboji (yes, I still confuse it with that big lake in the northern ‘Glades). A bit clearer but still unhelpful? This summer I attended two courses at Lakeside: Ecology and Systematics of Diatoms and Ecology and Systematics of Freshwater Algae. In that order – specific to general, that’s how it’s normally done, right? Start looking at the fineries of a specific group of algae (“the algae that live in glass houses”, or diatoms) and then see how they fit into the bigger picture of general phycology (“phykos” for “seaweed”). It actually makes a lot sense, especially when my research pays particular attention to the changes among the diatoms within algae communities in the Everglades (now I’m finally getting to the point). And it just so happens that the place to learn about diatoms is 1,800 miles from South Florida (or a 26-hour car drive, but who counted?). So while many of my peers were up to their knees in peat or swarmed by mosquitoes in the mangroves of the Everglades this summer field season, I was swarmed by mosquitoes by the lake, up to my knees in what many would call “lake scum”, and up to my eyes in diatoms in Iowa. And it was excellent.

Life at a biological field station is an experience completely its own, and as such it’ll get its own blog post! But suffice it to say, here, that it facilitates connections that are hard-pressed to forge elsewhere – connections to the research, to faculty, to peers, to the community, to nature. And it is my good fortune that Gene Stoermer established a “Diatom Clinic” at Lakeside in 1963 and that this course has persisted for 52 years, taught by Gene, Charlie Reimer, Gene again, and now Mark Edlund and Sarah Spaulding – all rock stars in diatom science committed to grooming new generations of diatomists. And the intrigue and utility of diatoms (boy, what a boring book title – we’ll have to think of something better) is such that students from all over the world – literally – come to this Great Lakes region of Iowa each summer to gain a proper education and exposure to the wonderful world of diatoms (getting there. But, really, “Great Lakes region of Iowa”?! Whoever heard of such a thing? Sounded like science fiction to me.). The class is capped at ten students per summer (one four-week session), and this year we came from Miami, Delaware, Colorado, Utah, MinnesOta, Montana, Ontario, and Colombia – with some old class T.A.s who can’t get enough from Arkansas and Macedonia. In short, students and professionals come from all over for a very focused class on a very focused group of algae that many people probably don’t know exist.

But, why? Why diatoms? If you can’t even see these microalgae, why even care? Why not care more about the cursed algae causing that green scum layer on my mom’s supposed-to-be-blue pool? Or those algae being used to solve our fossil fuel dependency? Well, we do care about those – I think cf. Thomas jeffersonii is keyed out as having “all algae are created equal” in its striae pattern (who wants to erect that genus?!) – but some pay particular attention to diatoms for a variety of reasons. And you can see diatoms – but few with the unaided eye. But when a bunch of 10 µm cells (1/1000thof a millimeter) hold a party they can be seen collectively (but only if you want to be seen as a party crasher). If you’ve ever fallen ungracefully into a lake because you slipped on those muddy rocks, don’t curse the mud but the diatoms and the mucilage they produce. Actually, I wouldn’t curse them – maybe reprimand them for their slippery inconvenience – but get to know them (especially now that you’re intimately acquainted, having fallen face first into a nice community [biofilm] of them). When you get to know them you realize that diatoms. are. awesome.

              E Pleurosira Unum? Creepy.

Diatoms are generically and specifically diverse (see what I did there?), widespread, productive, and tasty; they throw great house parties (just don’t throw rocks – their cell walls are glass after all); and they keep on giving after they’ve stopped living. They’re the algae you want to get to know at a party, the ones that always have your back and will give you good guidance in times of trouble (just like Mother Mary). They’re your best friends in the algae world.

Want to know why? Why choose diatoms over beautiful kelp forests or tasty nori (Porphyra, a red alga ‘seaweed’) or nutritious Spirulina (cyanobacteria)? Will Nick be held accountable for such a preposterous claim (after all, who 
doesn’t love sea otters?!)? Will we ever get to the “wonder” in the Wonderful World of Diatoms? Tune in next week for even more humorless asides and frustrating skirting around the facts (we are in a bit of a political lull, though!). Tune in next week for these answers and more!

(In all seriousness, thanks for reading this far, and I really do hope you’ll continue with this series!)




Tuesday, January 7, 2014

Exploring the Outer Reaches of the Everglades

January 07, 2014 0

 This post was written by guest blogger Emily Nodine, a PhD candidate in FIU's Periphyton Lab (http://algae.fiu.edu/research/).

When people think about today’s Everglades or the “River of Grass,” they generally think of Lake Okeechobee, Everglades National Park, and the canals and water control structures in between.  But the watershed is actually much larger than that.  Lake Okeechobee does serve as the headwaters of the Everglades; prior to human alteration, Lake Okeechobee would slowly overflow southward during very wet periods, forming the shallow, slow-flowing sheet of water that earned it the title “River of Grass.”  Today, the Hoover Dike prevents this and the water flow is strictly controlled, mostly released to the east and west coasts via the St. Lucie and Caloosahatchee Rivers, but also southward to the Everglades through an extensive system of canals and water control structures.  But the water in Lake Okeechobee came from somewhere else, too.

Lake Okeechobee sits at the mouth of the Kissimmee River and several smaller creeks that drain much of highlands central Florida as far north as Orlando.  Much like Lake Okeechobee and the Everglades, the Kissimmee River has also been through dramatic hydrological alteration and subsequent restoration efforts.  Once a meandering 103-mile waterway with a floodplain 1 to 3 miles across, the Kissimmee River was transformed during the 1960s to a 56-mile canal 300 feet wide and 30 feet deep.  Within the next couple of years, the South Florida Water Management District and U.S. Army Corps of Engineers plan to complete backfilling of a large section of the canal and removing water control structures in order to restore ecological integrity to 40 square miles of the river-floodplain system and 12,000 acres of wetlands.  Already, flora and fauna that disappeared following the canalization have begun to return.  Additional details about the restoration project can be found at http://my.sfwmd.gov/portal/page/portal/xweb%20protecting%20and%20restoring/kissimmee%20river.


Little of the Everglades watershed has been left untouched by hydrological alterations.  While restoration efforts such as the one-mile bridge on Tamiami Trail aim to deliver more water southward to the Everglades, estuaries at the outflows of the St. Lucie and Caloosahatchee Rivers  suffer from the effects of too much freshwater.  Historically, the Caloosahatchee River’s headwater was a small wetland pond west of Lake Okeechobee called Lake Hicpochee.  During early efforts to drain the Everglades for farmland in the late 1800s, a canal was dug connecting Lake Hicpochee to Lake Okeechobee, allowing the Caloosahatchee to become a major outflow for the larger lake.  Through subsequent canalization and installation of water control structures, the Caloosahatchee, like the Kissimmee River, was transformed.  Today, freshwater is released through a series of lock and dam structures down the Caloosahatchee to relieve pressure on the aging Hoover Dike that surrounds Lake Okeechobee, causing an influx of eutrophic water to the Charlotte Harbor estuary that results in adverse effects on seagrasses, oyster beds, and water quality.
My research is focused on the Charlotte Harbor watershed, which sometimes feels peripheral to the work of FCE LTER scientists in the Everglades, but I remind myself how important this region is as part of the Greater Everglades Ecosystem.  There are three major inflows into Charlotte Harbor, and they couldn’t be more different.  The Caloosahatchee, which is near my home, is highly managed and cut off from marine influence by water control structures (except during severe storms, when these are occasionally breached); the Peace River, which is naturally enriched in phosphorus and has been extensively mined for fertilizer; and the Myakka River, which is relatively pristine, with much of its watershed set aside as conservation lands and parks.
My goal is to understand the differences among these systems and how they influence inputs to Charlotte Harbor over time.  I am studying the diatom communities across this watershed in order to interpret long term changes from sediment cores taken from the estuary.  Diatoms are single-celled algae that provide clues about past environments because they are indicators of specific environmental conditions and they preserve in sediments, allowing us to determine what past conditions were based on which diatoms are present.  Specifically, I am interested in how they are distributed along environmental gradients, and how this changes in response to a disturbance such as a tropical storm or hurricane.  By studying what diatoms occur in these waterways before and after storms, I hope to identify a signal of hurricane activity that can be detected in sediment cores and help us to understand how these types of storms have affected south Florida ecosystems on large time scales.
Tropical Storm Debby, in June 2012, provided an excellent opportunity to investigate changes across the watershed.  During the dry season, diatom assemblages are strongly related to a salinity gradient across the watershed.   But following the storm, diatom communities changed in different ways across the various regions of the watershed.   Next, I hope to identify patterns in these differences to help us understand drivers of the type or direction of changes, such as whether anthropogenic alteration causes a different response to disturbance compared to more pristine areas.

Wednesday, October 17, 2012

Everglades Science: By land, by sea, and by air.

October 17, 2012 0

The Everglades is our backyard, and that backyard is HUGE!  Fourteen cities of Miami fit in the Everglades. But in exchange for the high-rises, freeways, and spanish-tiled roofs there are tree islands, sloughways, water, pines, mangroves, birds, alligators, fish, spiders, mosquitoes, and plenty of beautiful scenery. The vastness of the Everglades provides prodigious niches of scientific interest to pursue. Some of us study the impacts of the drainage and canal system that line the perimeter or pierce through the Everglades. Other scientists scrutinize the causes of vegetation community structure changes. Some research predator/ prey relationships and others, the animal movement between biomes. Some study the water cycle and the physical and chemical interactions between surface water and groundwater*.  But before we can crunch all the numbers, write all the papers, graduate and go off to save the world, we need to take the measurements, collect the samples, and download the data. Truthfully, it might just be the best part!
*In no way am I limiting the tons of amazing research going on in the Everglades with FCE to this list. You can check out more great glades research here.

As I mentioned earlier, the Everglades is huge and extremely remote. Different forms of transportation are needed to gain access your sites. Depending on your area of scientific interest, you have a few options on how to get there. My study is primarily focused in the coastal mangroves, but I also collect data, maintain autonomous data loggers and help other researchers in other portions of the Everglades. So I am fortunate enough to see many of the different environments. The Everglades has been coined as the "River of Grass" by Marjory Stoneman Douglas, giving you a hint up front that you are going to need at least a boat.
Fig. 1
 
There are days when I need to collect surface water and ground water samples in the southern and southwestern mangroves. For field days up Taylor River, we ride in a 16’ flat-bottom to the FCE sites TS/Ph 6 & 7.  In the early morning we grab the truck, hitch up the boat and drive down to the Key Largo Ranger Station to launch the boat. From there we drive north-northwest across Florida Bay to the mouth of Taylor River. A lovely 30 minute drive on the open water followed by a 25 minute sinuous maze through the tidal creeks. The mangroves at Taylor tend to be very short, growing a little larger around the tidal creeks which are just large enough to drive a skiff through (Fig 1).  Packed away in the boat are water pumps, bottles, sippers, field computers, field probes and the usual set of tools and electrical supplies (Fig. 2). All the necessary items plus a little more, because it is not like you can head to the store real quick to get something you forgot. The samples will later be analyzed for there chemical composition; major ions, nutrients, and isotopes. These analyses help us to understand the how different water sources interact with other water bodies or with the environment around it. More on that topic at a later date. 
Fig. 2

On other days, I need to collect samples up Shark River. The day pretty much starts the same way. Meet early in the morning. Hitch the boat up and head south. But instead of continuing to the Keys, we turn west toward the main Everglades National Park Entrance on our way to Flamingo. This is a long and lonesome 50 minute drive from the entrance to Flamingo, but the bright side is that you get to drive through many of the unique environments in the park; pine rocklands, marl prairies, cypress stands,  ponds and mangroves.  On really good days you can spot some really cool birds (especially in the coming months). 
Fig. 3

Once at Flamingo, we launch the boat and head northwest across Whitewater Bay and the turn northeast up Shark River to sites SRS 4, 5 & 6.  On lucky days you can run into other FCE researchers from FIU, the USGS, or the ENP (Fig. 3). Most days I am the captain of the vessel (requires MOCC training), on other days I get to put my feet up and enjoy the ride (Fig. 4). During the wet season (May-Nov) it is inevitable that you will encounter a thunderstorm or two (Fig. 5). Usually this happens in the early afternoon, once the convection clouds start to form. In the rainy season, you can almost set your clocks to it.

Fig. 4

Fig. 5

Both the Taylor River and Shark River sites are located in brackish water. In the freshwater portion of the Everglades we can use an airboat to get around, even when there is just a few inches water above the surface. We start with another early morning, but this time we hook up the airboat and head west on Tamiami Trail to Frog City. At Frog City (authorized access only) we launch the airboat on a beat up boat ramp (Fig, 6). Thank goodness for 4-wheel drive.  
Fig. 6

After putting on lifejackets and ear muffs, we crank the boat up with a thunderous roar from the small aviation engine and head south along the airboat trails (Fig. 7). Once we get to our site, it is time to get wet and muddy (Fig. 8). At our freshwater sites, we download data and maintain our Sontek velocimeters. This instrument uses an acoustic pulse to measure small changes in water flow and helps us to understand how fast and how much water is moving through the Everglades.

Fig. 7
 
Fig. 8
 

The best view of the Everglades comes from the air (Fig. 9).
Fig. 9

In the dry season, the water levels in the glades can drop very low and prevent us from using the airboat. Therefore, we have to take the helicopter. No complaints here. The ride to our sites takes only 15 minutes instead of 60. The perspective from the helicopter helps you to really see the great expanse of the Everglades (Fig. 10).

Fig. 10

The cost of the helicopter is pricey so we take measures to help be as cost-effective as possible. We usually share the ride with another researcher and split up to take care of different tasks simultaneously (Fig. 11). Depending on the water levels we might fly over some fellow researchers (Fig. 12) or depending on our heading we might catch an old plane wreck (Fig. 13).

 
Fig. 11
Fig. 12
 
Fig. 13
 
The "River of Grass" is really an amazing place to see and it is always a journey to get to our far-away sites. Ultimately, seeking out the scientific mysteries of the swamp.  
 


Tuesday, August 14, 2012

Grad Student Life Beyond Fieldwork: Part 4 (Our Labs)

August 14, 2012 0

Today’s post is the last installment of my series “Grad Student Life Beyond Fieldwork.” Take a look at Part 1 (Classes), Part 2 (Teaching) and Part 3 (Our Offices) to read about other facets of grad student life. Part 4, the post you are reading now, is about the labs where we produce and analyze data.


Some measurements we use for our research, like water temperature and salinity, can be measured directly in the field. Other more complicated things like “cyanobacteria community structure” involve taking field samples back to a lab (or multiple labs) for extensive analysis. Below I have posted a “virtual tour” of the lab I work in, the Microbial Ecology Lab at FIU, to give readers an idea of what grad students and scientists do other than walk around wearing lab coats. 


Above is the door to the lab. It basically says, “Welcome! You are about to encounter biological materials, carcinogens, flammable materials and high voltage equipment! You should probably turn around.” All of these dangers are necessary to understand what microscopic organisms live in water samples from the Everglades and Florida Bay. Although this sign implies that you might die upon opening the door, our lab is generally safe as long as you use common sense and have a little bit of lab safety training. 


Next we enter the lab. Note that just like my office, it has no windows. All scientists are allergic to sunlight.

One line of research conducted in this lab is determining cyanobacteria community structure. While one could look under a microscope at a water drop and take a guess at what kinds of cyanobacteria are in it, genetic techniques have been developed to give a much more accurate picture of what species are in a water sample. Understanding cyanobacteria community structure and factors that impact it is important for Florida Bay water samples because Florida Bay often experiences cyanobacterial blooms. Below is some of the equipment and tools we use to determine community structure.


This is the PCR (polymerase chain reaction) thermocycler, which amplifies segments of cyanobacteria DNA. An extremely small drop of a water sample and several reagents are added to tiny vials then placed in this machine. The machine then repeatedly heats and cools the vials so copies of the desired DNA segment can be made.

How small of a scale are we talking about? Above are the pipets that we use. Notice that they are set in microliters.

Not all laboratory equipment is highly advanced and specialized. While the DNA is synthesized, agarose gels are prepared using the microwave shown above. Since ethidium bromide, a probable carcinogen, is used in the gels, this is not the best place to heat up your lunch. 

After the gel is prepared and solidified, we pipet 5-10 microliters of the amplified DNA into tiny wells in the gel (I am probably really good at the board game “Operation” after doing this hundreds of times). An electric charge is then run across the gel in the gel electrophoresis machine shown above, which moves the DNA down the gel. The distance the DNA travels tells us how long the segment of DNA is. With a few more lab procedures and hours of analysis on Excel, we can determine what species of cyanobacteria were in the original sample.

FCE Grad Students: How much time to you spend in your lab? What are some things you like or don’t like about your lab work?

Other Readers: Do you have any questions or comments about our lab work?  Do you have any questions remaining about grad student life (classes, teaching responsibilities, etc.)?