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If you read my previous post on the interesting article about coccolithophore species-specific growth responses to environmental change, you may have been left wanting to know more about coccolithophores in general. I don’t blame you. Coccolithophores are pretty awesome. Continue reading Chalk talk: Coccolithophores
Dinoflagellates are large single-celled motile phytoplankton that are extremely widespread and abundant in the ocean. They are astonishing little creatures that – depending on the species – can produce potent neurotoxins, feast on organisms many times larger than themselves (whilst also photosynthesising), travel large distances in search of nutrients, hibernate for up to 100 years, and glow with terrific blue-coloured bioluminesence. So, without further ado, here are five reasons why dinoflagellates are friggin’ awesome: Continue reading 5 reasons why dinoflagellates are friggin’ awesome:
A reworked (some would say ‘improved’) version of Clement Clarke Moore’s classic Christmas poem:
‘Twas the night before Christmas, and all through the ‘photic zone,
Few creatures were stirring, most plankton were all alone;
The water was mixed, with nutrients galore,
Critters hoping come spring, temperatures would soar. Continue reading ‘Twas the night before Christmas (phytoplankton edition)
Most of you reading this will be very familiar with the story of how ocean acidification is likely to impact marine calcifying organisms: increased carbon dioxide in the atmosphere is decreasing the pH of the oceans and is proposed to eventually lead to the dissolution of the shells of organisms made from calcium carbonate. It is difficult to work out in the lab, however, exactly what the impact of ocean acidification will be on marine calcifiers, as time pressures favour experiments that only assess short-term acclimation responses of organisms to ocean acidification (rather than long-term potential adaptations). Even when long term experiments have been carried out, they have only looked at the impact of pH change alone (see here), ignoring other relevent variables such as temperature. Continue reading Calcifying plankton and climate change
It was revealed this week that Russ George, a controversial American Businessman (Deep-Sea News ran a good piece this week covering his chequered history), dumped around 100 tonnes of “iron-rich dirt-like material” off the west coast of Canada in July in order to “gather data targeting all the possible fears that have been raised” about ocean fertilization – an act that is in violation of two international moratoria designed to prevent material from being dumped in the ocean. Judging from the poor quality of news coverage on the issue, which tended to include the deceptive image shown above (Image 1), there are a lot of misconceptions about iron fertilisation of the ocean. Here is the official Words in mOcean idiot’s guide to make you instantly more knowledgeable on this subject. Continue reading A guide to iron fertilisation of the ocean
President Obama’s administration announced recently that as much as $14 million would be set aside to support the development of biofuels from algae. He was promptly mocked by some sections of the the US media and many of the Republican candidates. Serial ditcher of terminally ill wives, Newt Gingrich, proposed making T-shirts with the slogans, “You have Newt: Drill here, Drill Now, Pay Less. You have Obama: Have Algae, Pay More, Be Weird.” Continue reading Phytoplankton to the rescue: the promise offered by algal biofuels
This is the second of two articles written by Elizabeth Sargent on the marine nitrogen cycle; the first article covered some of the basics and can be found here
There are three main groups of nitrogen fixing organisms in the ocean: filamentous, heterocystous, and unicellular diazotrophs. The unicells are relatively new to the research scene (discovered in 1998), and are difficult to image due to their size, distribution, and our lack of knowledge about their lifestyle. I have some epifluorescent microscope images of unicellular diazotrophs, but you can get a good idea of what that looks like by picturing the night sky; it’s a whole lot of darkness and some tiny yellow dots. Continue reading Marine nitrogen fixation: the players
This is the first of two articles to be written by Elizabeth Sargent on the marine nitrogen cycle; the second article will go into more depth on nitrogen fixers (or, as Liz refers to them: ‘the diazotrophic organisms I hold near and dear’).
The marine nitrogen cycle is one of the most complicated biogeochemical cycles in the ocean. Nitrogen is a biologically limiting element and changes in its form, or concentration, can cause changes in the cycling of other elements, such as carbon and phosphorus. Marine nitrogen cycling has been and will continue to be an integral component of ocean biogeochemistry, so everyone should know at least the basics. Continue reading The marine nitrogen cycle
…I wish that what I did sounded a bit less interesting.
Let me explain: I really do love what I do, but what I dread more than anything else is telling ‘non marine biologists’ about it. You see, there are (generally) only two responses that you get when you tell someone that you are a marine biologist:
1) “So what the hell are you going to do with that?” often accompanied by a look of bemusement suggesting that you are currently in the process of throwing your life away
Or, and I think this is actually worse…
2) “Wow, so do you get to work with (swim with) sharks, dolphins, whales, turtles (etc.) then?”
Words in mOcean 