Biodiversity in the cryosphere

As one of Earth's major biomes, the Cryosphere (taken from the Greek 'krios' meaning cold, frost or ice) is extremely important to consider when trying to understand global biodiversity. The Cryosphere encompasses those parts of the world which are frozen including, ice sheets, glaciers, frozen rivers, lakes, sea ice, permafrost and ice shelves. Today, I am focusing on the importance of sea ice to Arctic biodiversity after being fascinated by the paper published from Post et al (2013) introduced to me by my global environmental change lecture on the 6th December. With it being published only a few months ago, I decided to read the full paper and became instantly intrigued by polar biodiversity.

Sea ice compromises unique ecosystems in, on and under the ice. This habitat is critical for many species including vertebrates, diatoms, also terrestrial productivity and aquatic diversity. With 80% of the tundra in the Arctic lying within 100km of an sea ice covered ocean, Arctic ice loss driven from amplification Arctic warming is vital for ecological dynamics in this area (Post et al. 2013). Arctic amplification is the melting of ice due to a positive feedback albedo system. Ice has a high albedo therefore reflecting sunlight keeping the poles cool. However through ice melt, more of the Arctic ocean becomes exposed and due to oceans being darker they have a much lower albedo. This means they absorb heat warming the oceans and the atmosphere. As the oceans absorb heat, they also have to release this increased heat to enable the sea ice to form for the next year. Due to this feedback, the more ice loss the longer it takes for oceans to release the heat it has absorbed and therefore sea ice formation gets delayed. This can have affects for semi-aquatic species such as polar bears which use the sea ice for reproduction ground and for resting during long migration routes.

With anthropogenic warming Arctic sea ice extent has slowly been declining.

Source. A) Graph showing the declining annual minimum Arctic sea ice extent from 1979 to 2012. Although,  there is seasonal variability the overarching trend is a decline. B/C) Two maps showing the percentage concentration loss of sea ice with the scale bar showing -5% to 5% change. B is from 1979-1999 and C from 2000 -2011. 


The trend seen in the maps is showing percentage loss, especially around the edges of the sea ice, due to warming oceans.

The direct effects of Arctic sea ice loss

1. Primary producers depend on the sea ice habitat, underpinning the whole Arctic marine food web.

- With the loss of sea ice, this is a loss of habitat for algae and phytoplankton.  The timing of the algae bloom which is ultimately driven by light penetrating the ice when it is thin enough, is vital for the reproduction of zooplankton grazers. Disruption of this timing due to accelerated ice melt has created mismatches for zooplankton production timing and the consumers up the food chain.
- Earlier phytoplankton blooms can shorten the length for primary productivity consequently affecting the zooplankton production and the Arctic cod species that feed on them (Post et al. 2013).

2. With ice melt comes increasing freshness of the Arctic ocean.
- This reduces the nutrient availability for phytoplankton which limits their productivity despite increased solar penetration through ice thinning.

3. As previously touched upon, vertebrate species such as polar bears require sea ice for reproduction and resting and therefore they are directly implicated by sea ice thinning. One species also effected is the ringed seal (Gohring, 2012). More than two thirds of the Arctic has been estimated to have insufficient snow cover for ringed seals to reproduce challenging their whole survival. A ringed seal is currently under consideration for the threatened species list due to the way it builds caves to rear its offspring in snow drifts on sea ice (NOAA, 2013).  (Hezel et al. 2012) estimated that snow drifts must be at least 20cm deep to support the caves. As sea ice disappears, there is no where for the snow to pile up, ultimately declining the area where the seals can reproduce. What is also worrying is that with earlier snow melt year on year, the caves will melt also much earlier, leaving the young vulnerable to the outside conditions and predators.

Next week, I will be continuing the polar theme by exploring the indirect impacts of sea ice loss in the Arctic so keep those eyes peeled. Only two weeks till christmas!!

Score Board Update: Anthropocene 4 - 2 Biodiversity. 

Discovery of new species everyday: Is biodiversity increasing?

Moving away from the ocean focus from the past two weeks, todays post explores a recent article by the BBC about the identification of a new wild cat in Brazil by Coles (2013).

Everyday I look on Nature and there is an article about a new species being discovered. These new species are found in a range of locations from Burma to closer to home in the United Kingdom. With new species being discovered everyday, is it possible to make the judgement that biodiversity is possibly increasing on local scales around the world?

Check out the Coles (2013) article and make up your own judgements. It is important to note that we do not know everything about the natural world and therefore to make all encompassing conclusions about global biodiversity, is extremely difficult.  These conclusions are strictly based on the knowledge we do have while accepting the unknown.

Articles to check out:

New species of Hammerhead shark discovered off Carolina coast (Kenniff, 2013)

Spectacular New Species Found in the Lost World (Dell'Amore, 2013).

New Species of 'Skeleton Shrimp' discovered (Vincent, 2013).

Score Board Update: Anthropocene 3 - 2 Biodiversity 

Coral Catastrophe?

Being an ecology enthusiast with a particular fondness for corals, todays post is one of my favourites so far. We all acknowledge that coral reef ecosystems are extremely important to the health of the oceans. While they cover only 1% of the oceans, it is estimated that one quarter of all marine biodiversity spends, at least part of their life on a coral reef. When corals are mentioned most people think of tropical waters and an instant picture of the Great Barrier Reef pops into mind. To me the term 'coral' automatically conjures up brightly coloured images present in the Pixar film, Finding Nemo.

However, as the NOAA state shallow water corals are only one type. There are cold water corals and deep sea corals that have limited light producing soft corals. 

What are corals?

The Oxford English Dictionary defines corals as ' hard stony substance secreted by certain marine coelenterates as an external skeleton, typically forming large reefs in warm seas'. 

Corals are invertebrate animals belonging to a group called the Cnidaria. They can exhibit a wide range of colours, shapes and come in all sizes. Each coral is made up of hermatypic polyps and most live in colonies. A coral colony can grow to be very large indeed. The hermatypic polyps produce calcium carbonate to form calyx (NOAA, 2011). The calcium carbonate adds to the coral skeleton forming the beginnings of the coral structure. Corals develop slowly over millions of years, today the corals you see have been growing for around 50 million years. To date there are around 800 known species of hard coral and more being discovered, just as new species of marine animals are being found in the most remote ocean locations every day. 

Source. Coral forming diagram.

Where are corals found?

Coral reefs are found throughout the oceans, from deep, cold waters to the shallow tropical waters of the Indian Ocean. Tropical reefs extend from 30 degrees North and South of the equator. However, cold corals can also be found in places closer to home such as off the West coast of Scotland and Ireland. Cold water reefs have also been found in the Mediterranean. 

There are various factors that cause the pattern of coral reefs throughout the world. 

These include:

The role of ocean temperature

The effects of emersion

Bathymetry

Levels of sedimentation



Types of Coral Reef

• Fringing Reef: most common type of coral reef located close to land. 

• Barrier Reef: looks like a fringing reef, however, it is located further away from the shore. They are separated from the shore by a band of water.

• Atoll: large ring shaped reef, which create a lagoon in the middle. 

Anthropogenic threats to coral reefs
Corals are ecosystems that have been developing for years, and in this time have been subjected to natural change. The worry now is that with increasing human stresses, corals may not be able to cope.   WWF (2010) states that already 'one quarter of coral reefs are subjected to damage beyond repair, with another two thirds under threat'. With reef building corals representing a critical component for marine biodiversity, it becomes important to conserve these ecosystems in order to conserve the species that use coral environments (Huang and Roy, 2013). 



Destructive fishing practices: Blast, dynamic fishing and bottom trawling are types of fishing practices that cause devastation to sensitive coral reefs. Bottom trawling has been widespreadsince the 1980s. The large rubber tires on the nets can damage the coral structures. Dynamic fishing is  where explosives are set off underwater destroying coral. This has been particularly a problem in South East Asia (Cadwell and Fox, 2006). 



Pollution: Urban and industrial waste being released into the oceans which are poisoning the reefs.  Pollutants increase the amount of nitrogen in the waters causing an overgrowth of algae, which can smother the reefs, concealing them from sunlight which the polyps need to survive (McManus, 2000).



Sedimentation: Anthropogenic coastal construction, mining, logging and tourism developments can cause erosion. This erosion causes increased levels of sediment being produced. Sediment covers coral, almost suffocating it and causing the corals to produce a protective mucus (MES, 2002). This process takes incredible amounts of energy and if corals are overworked they can die. 



Ocean acidification: As mentioned in my previous post, marine environments are particularly threatened by climate change and the increasing pH of ocean waters. Since the beginning of the industrial revolution, the oceans have been absorbing increasing amounts of excess carbon dioxide. With ocean acidification, corals cannot absorb the calcium carbonate needed to maintain their structures and therefore the reef will dissolve (SCOR, 2009). 



        
Ocean acidification effects on coral reefs. 


Global warming and coral bleaching: In the Anthropocene, global warming is a known threat to many ecosystems. It occurs because carbon dioxide and other greenhouse gases cause a blanket, preventing heat from the sun to escape, warming the atmosphere. Ocean warming is extremely devastating to coral biodiversity, which is sensitive to changes in temperature. If oceans stay warm for several weeks, zooplankton leave the corals, turning them white in the process, because it is the zooplankton that gives corals their unique colours. NOAA (2013) discussed how in 2005, the USA lost half of its coral reefs in the Caribbean in only one year due to a huge coral bleaching disaster. 



       
Coral Bleaching: showing the distinctive white coral. 



However, a recent study showed it is not all bad news. Elevated nitrogen and phosphorous at a study site in Florida Keys from 2009-2012, showed coral bleaching. What this study also noted was that once the injection of pollutants ceased, the corals became able to recover and in a surprisingly short period of time (PhysOrg, 2013). 


There are other threats to corals, however I have rambled on too much already. I hope you enjoy this post and it provides a insight into the marine biome and the anthropogenic impacts of coral ecosystems. Being a corals fanatic, I find it extremely worrying that humans can be having such disastrous effects to one of the world's most beautiful environments. I, for one, want to be able to dive  and explore these unique ecosystems, enjoy their bright colours and extraordinary patterns and it would be devastating if these environments were not there for people to enjoy. 

Score board update: Anthropocene 3 - 1 Biodiversity 

Oceans- What will the future hold?

In previous posts I have concentrated on mainly terrestrial biodiversity (however not on purpose). Today I take a swim with the fishes to investigate one of Earth's most interesting biomes- the ocean.

'The ocean covers nearly three quarters of the Earth's surface, provides about half of the oxygen we breathe and feeds billions of people every year' (Le Roux, 2013). 

The oceans have been protecting the Earth from the worst effects of human induced climate change for years by absorbing excess carbon dioxide (Bijma et al. 2013). This absorption, however, is having a negative effect driving the oceans into an acidic state. Along side this acidification, ocean warming is having grave impacts on the structure of many marine ecosystems. Bijma et al.(2013) coined ocean warming, acidification and deoxygenation the 'deadly trio' of anthropogenic impacts that are causing  accelerated loss of marine populations (Worm et al. 2006). Since the industrial revolution the world's oceans have become 26% more acidic and will continue to force oceans into a acidified state at an unprecedented rate.

Ocean acidification is the reduction in the pH of the ocean waters by the uptake of carbon dioxide from the Earth's atmosphere. It can also be caused by chemical pollution into the oceans. The carbon dioxide dissolves in the seawater generating changes in seawater chemistry. The addition of carbon dioxide increases the concentration of bicarbonate ions and carbonate ions which, consequently lowers the pH making oceans more acidic. For a beginners insight into ocean acidification take a look at the below flow chart, showing the changes in chemistry from slight alkaline to acidified seawater. 

Beginners guide to ocean acidification.

Many recent reports, have discussed how ocean change may be faster than any time in the last 300 million years, predicting that by 2100 there will have been a 170% increase in ocean acidity. But is it all doom and gloom for oceans? There has in fact,  been scientists that have discussed how marine species could survive and even thrive (seagrass) under ocean acidification and warming (McGrath, 2013). 

What environmental scientists are most worried about is the effect of the 'deadly trio' on corals. In the Great Barrier Reef half of the coral cover has been lost over the past 27 years. There have also been dramatic coral bleaching events in 1998 and 2002 due to anthropogenic ocean warming. In the Southern Ocean, we can unfortunately already see corrosion of pteropods (sea snails) shells. In my next post, I aim to expand on corals in more detail, focusing on the threats posed by the anthropocene to these highly sensitive environments. 

Coral Disaster: Great Barrier Reef coral bleaching. Source. 

With a carbon release of around 30 gigatonnes of carbon dioxide a year, it is no surprise that academics are worried about a major ocean extinction. As I touched upon in my previous post a sixth mass extinction' is a upcoming worry. However, speculative this theory may be, oceans are one of the biomes which are most vulnerable to a huge biodiversity decline. With changing ocean conditions, many species could possibly find themselves in unsuitable environments, especially in oxygen poor "dead zones"(Le Roux, 2013). 

What will the future hold for the oceans? Will there be a biodiversity loss in one of the worlds most diverse environments? Keep your eyes peeled for my next post which will look at the threats posed to corals.

Score Board Update. 

Anthropocene 2- 1 Biodiversity.

Sixth mass extinction just around the corner?

Following on from the videos I posted last week, my post today is going to focus on a recent paper by Barnosky et al. (2011).  Barnosky provides a detailed background to previous mass extinctions and also  focuses on arguments surrounding the possibility of a sixth mass extinction.

What is a mass extinction?

The answer lies in the past. Palaeontologists characterise a mass extinction as a short geological period in Earth's history where more than 75% of estimated species become extinct (Jablonski, 1994).  This type of extinction has only happened 5 times in the past 540 million years (Barnosky et al. 2011). The 5 mass extinctions occurred at the end of the Ordovician, Devonian, Permian, Triassic and Cretaceous periods. Will the anthropocene hold the next mass extinction?

Biodiversity of the planet over time, showing the five mass extinctions in history.
Graph adapted from Wilson (1992)

Why do we care about past extinctions?

Scientists are interested in past extinctions because they provide a key to the future. The most famous species extinction was the Cretaceous- Tertiary which occurred 65 million years ago. This is the extinction that is famed for the death of the dinosaurs. One hypothesis for this decline was climatic cooling causing a reduction in hospitable habitats (this is the worry for current global warming). The Permian extinction (248 million years ago) also causes scientists to quake in their boots due to being caused mainly by global environmental change, including methane release from the sea floor, increased sea level and a shift in ocean circulation (Eldredge, 2011). The main concern is that history will repeat itself? Increasingly, academics are recognising contemporary species extinctions as part of an overarching 'sixth mass extinction'. Anthropogenic influences such as habitat fragmentation, disruption by invasive species and changing global climate all directly contribute to the decline of biodiversity. Scientists are now worried that the Earth will, in a few centuries, be under threat from major species decline.

Before we can come to any sort of conclusions, it remains vital to establish the current situation within the context of  previous mass extinctions. There have been many landmark studies that have told of modern extinction rates an order of magnitude higher than than previous extinction rates (Doubleday, 1992; May et al. 1995). The below chart explores the extinction magnitudes of IUCN assessed taxa in comparison to the 75% benchmark (International Union of Conservation Red List, 2010).  The black icons add the species that are currently 'threatened' species to those that have been extinct for over the past 500 years. Therefore, we can see that all species are threatened in the age of the anthropocene. Groupings such as mammals, birds and amphibians, which have had historically the lowest percentages of species extinctions, nowadays have the highest numbers of endangered and threatened species. Could these species be susceptible to catastrophic extinctions? The current numbers show the sixth mass extinction is looming quite far away, however anthropogenic activities are causing more and more species to become increasingly threatened. Barnosky et al. (2011) suggests that if all 'threatened' species disappeared we would be half way towards a possible anthropocene mass extinction.

Extinction magnitudes of IUCN assessed taxa (2010)

It is not just terrestrial species that are vulnerable, marine species are particularly susceptible to mass extinction. At least 830 marine species have been classified as critically endangered, endangered or vulnerable. Assessments for marine species are lagging behind those for terrestrial species. However, the IUCN aimed to have 20,000 marine species assessed by 2012. It is important to understand that the past drivers of extinction in the oceans are the same as the current threats  (as can be seen in the chart below).  Marine scientists that released the State of the Ocean 2013 report on 3rd October 2013, gave a warning stating 'we are entering an unknown territory of marine ecosystem change, and exposing organisms to intolerable evolutionary pressure. The next mass extinction event may have already begun'. The report explains how the ocean is the world's largest carbon sink and the increasing carbon dioxide levels are creating a 'deadly trio of impacts' including ocean acidification, ocean warming and deoxygenation all of which are threatening marine biodiversity. If you want to know more about this , check out The AnthropoSea, a blog dedicated to investigating the 'deadly trio' and its threat to marine biodiversity. 

What is the situation today? 

Today, the rapidly changing atmospheric conditions and warming of above average interglacial temperatures cause species to become vulnerable. With rising carbon dioxide levels, habitat destruction, pollution, overfishing, over hunting and invasive species, the world now has more ecological stressors than many species have ever experienced before. 

Species extinctions rising with increasing human populations.

The worrying question is how will this affect the already threatened species? It seems quite plausible that if humanity carries on living in the same way, it will not be long before the 'sixth mass extinction' is just around the corner.  It is encouraging that there is still much of Earth's biodiversity that can be saved. However, it is daunting that in order to save such species there must be rapid reversal of escalating threats. How realistic is this? 

While I was researching for this blog post I came across a very interesting short film that had just been released called the 'Last Hours'. The film had been produced for presentation at COP21 (the 21st session of the Conference of the parties to the UNFCCC expected to take place in 2015). The film maker was Thom Hardmann, an American radio talk show host and best selling novelist. I watched the film and I have to say although highly dramatised, with a soundtrack that could rival 'the day after tomorrow', it provides an insight into the possibility of another mass extinction.  The film has caused a media outpour, with the likes of Leonardo DiCaprio tweeting his affection for the film (thats the reason we know it is worth a watch!). 

However, the film has also received criticism for its methane hydrates hypothesis. In the recent IPCC 2013 report, many of the catastrophic changes being forecast were described as likely, unlikely or exceptionally unlikely. The melting of permafrost and the subsequent release of huge reservoirs of methane is deemed exceptionally unlikely, therefore the film has to be taken with a pinch of salt. Why not have a look and make your own judgements. 

Do you think we are in a sixth mass extinction, or are we very close to entering one? 

To end this post here is just a snapshot of some news articles that have documented species extinctions and the catastrophic possibility of another mass extinction.

Ananthaswamy, A (2004) 'Earth faces sixth mass extinction', New Scientist. 

Harvey, F (2013) 'Rate of ocean acidification due to carbon emissions is highest for 300 million years', UK Guardian.

IUNC (2009) 'Wildlife crisis worse than economic crisis', IUNC. 

Mccarthy, M (2011) 'Marine life facing mass extinction within one human generation', Independent. 

Pappas, S (2012) ' Earth's ecosystems nearing catastrophic "tipping point" warn scientists', The  Christian Science Monitor. 

Score board update. 

                                    Anthropocene 1- 0 Biodiversity 

Invader Intolerance: A presumptuous viewpoint?

As my introductory post touched upon, there are many anthropogenic impacts effecting biodiversity (see below for a comprehensive list!). 

- Habitat destruction and fragmentation

- Agricultural intensification and changes in land use

- Changes in forest management practices

- Overfishing

- Atmospheric pollution

- Water pollution

- Climate change

- Human disturbance

- Invasive species

- Harvesting and collection of species (hunting)

- Ocean acidification

(Natural England, 2011) 

The focus for today is invasive species. Before I start chattering on about zebra mussels and the red squirrel, I believe it is crucial to understand just how scientists define and quantify biodiversity. The term 'biodiversity' originates from conservation biology and was coined by Walter Rosen in 1985. A formal definition was published by the Convention of Biological Diversity (1992) which stated:

'Biodiversity is the variability among living organisms including terrestrial, marine and other aquatic ecosystems and the ecological complexes of which they are part; this includes diversity within species, between species and of ecosystems'. 

Biodiversity measures have, however, also taken a battering over the years.  Wilson (1992) discussed the ambiguity surrounding measures of diversity and explored the possibility that biodiversity was in fact restricted by measuring species numbers alone. This has also been reiterated more recently by (McCann, 2007).  Nowadays there is still uncertainty when quantifying biodiversity (scientists can never make up their minds) and therefore this will be considered in much greater detail in a few weeks. 

So now back to the purpose of this post- 'INVASIVE SPECIES'. Although known worldwide as threatening and disruptive, non-native species and their impacts to biodiversity continue to be greatly debated throughout scientific literature. So why do invasive species have such a bad reputation? Invasive, known also as 'alien' and 'non- native' species can have significant effects on the existence of some species and their habitats. An example is the native red squirrel (Sciurus vulgaris) which has become threatened and outcompeted in the UK by the non-native 'grey' squirrel (Sciurus carolinensis). The first evidence of the red squirrel dates back to the end of the last ice age, 10,000 years ago. 

Save our native: The Red Squirrel

However, since the grey squirrel became introduced to the UK in the 19th Century it has replaced the red squirrel throughout most of England, Wales and parts of Scotland and Ireland (Bryce, 1997). The traditional explanation for this reduction in the red squirrel, is the overwhelming competition with the grey squirrel for food resources (Kenward and Holm, 1993). This was not the only reason for their gradual decline, another proposal is the introduction of devastation parapoxvirus (a fatal strand of squirrel "pox") that was brought from North America to the UK by the grey squirrel. The disease spread into the red squirrel population hence the rate of infection was extremely high. This induced a population crash, reducing the crowding pressures on non-native grey squirrels which subsequently increased in numbers (Gurnell et al. 2004). 

Squirrel distribution maps from 1945- 2010 showing the interaction between the red and grey squirrels (RSST, n/d). 

From the above maps, the red squirrel population can be seen to be rapidly declining especially in Northern England and Wales, with the grey squirrel taking over the South of England and the Eastern Coast of Wales. Wales and the the midlands, surprisingly, have habitats which are occupied by both species. From the maps above it is highlighted that urgent steps are needed to address the issue of invasive species in order to save native species. 

It is not just terrestrial ecosystems that can become jeopardised by non-native species, freshwater habitats are also extremely vulnerable. The ICAIS (International conference on aquatic invasive species) 2013 report stated that 'the introduction and spread of invasive species in freshwater and marine environments is a worldwide problem that is increasing in frequency'. A recent example is the invasion of the Asian Carp throughout the river systems of Illinois, USA. They were introduced, from China, into water treatment ponds to remove algae in 1970s. The carp escaped and migrated northwards through the Mississippi and Illinois rivers. Although the carp did not cause any extinctions of native species, there was a decline of certain commercial fish such as the big mouth buffalo (Ictiobus cyprinellus). 

Bigmouth buffalo threatened...

Invasive species (in some cases) are considered such a colossal threat because they have the upper hand when resources become scarce.  CSIRO, Australia's national science agency calls invasive species 'one of the greatest threats to biodiversity and to the ecological and economic well being of society and the planet'.

However... not every scientist shares the same assertive view on invasive species. In fact, only a week ago Professor Phil Roberts from the University of York published a paper which throws all opinions up in the air. This is why I love science, its contestable nature. Roberts (2013) discusses how the Anthropocene could raise biological diversity through the introduction of non-native species causing evolutionary hybridisation. He acknowledges that some invasive species damage ecosystems and can eradicate resident species (as I have already explored). However, his discussion remains focused on how people fail to acknowledge that invasive species can also be positive for biodiversity. On average, less than one native species dies out for each introduced species that becomes established. Roberts (2013) neglects cases of invasive species disruption and instead highlights that, despite the fact that we are losing irreplaceable populations, in some (some being the key word here) regions biodiversity is actually increasing.

I will leave you with Roberts (2013) departing words: 

'we have to rethink our "irrational" dislike of invading species'.

I, on the other hand, do not believe that the negative reputation of invasive species is 'irrational', due to the destruction they can and have previously caused. However, it is vital to understand both arguments in order to judge whether there is still hope for biodiversity, in particular at a regional level, despite the doom and gloom of inevitable global species decline.

Anthropocene 0-0 Biodiversity 

What do you think is in the lead? Suggestions welcome!

 

Biodiversity vs 'The Anthropocene': Let the battle commence

Despite my initial inhibitions, I have finally joined the blogging world (enter applause here). Since this is my first post, I am going to explain the focus of my blog and why I believe it warrants such discussion. As my title, 'Is the grass greener on the other side?' suggests, I will be investigating debates surrounding the Anthropocene and its effect on global biodiversity. Are we entering a 6th mass extinction or is there still hope for the species that roam our planet? Roberts (2013) discusses how the Anthropocene has brought an age of 'ecological transformations' and my blog will explore the impacts of these 'transformations' for global biodiversity. My reasoning for choosing this focus, is probably due to my slight obsession with ecology (I love plants, what can I say). 

So what is the Anthropocene I hear you say? A simple definition can be found in the Oxford English Dictionary:

'relating to or denoting the current geological age, viewed as the period during which human activity has been been the dominant influence on climate and the environment'.

As is suggested, the Anthropocene is unlike any geological period before. The dangerous levels of industrialisation, land use change, ocean acidification, freshwater eutrophication, carbon dioxide and methane emissions are what distinguish this 'Age of the Humans'. Humanity has taken on the role of God and is now pushing the Earth over planetary boundaries. The exact time when the Anthropocene emerged still remains a highly contentious debate. For a VERY basic explanation of the Anthropocene and its implications, feel free to watch the following short video.

Over the course of my blog I aim to cover a wide range of topics including (but not limiting myself to) invasive species, ecosystem resilience, migration of species with climate change, ocean acidification, freshwater eutrophication and the 6th mass extinction. Rather than having a strict agenda, I want my blog to be an engagement with current literary debates and allow my opinions freedom to develop over the next 3 months. 

I hope you enjoy following the battle between biodiversity and the Anthropocene. What will come out on top? Will the grass for biodiversity be greener on the other side? 

Let the battle commence.