Intro to aDNA and paleoecology Flashcards

(45 cards)

1
Q

What is aDNA?

A

Ancient DNA (aDNA) is DNA isolated from ancient specimens. Also, aDNA can also be referred to as DNA samples recovered from biological samples not intended for DNA use, including historical and archeological samples.

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2
Q

The Arrhenius equation describes the parameters that affect DNA breakdown/preservation. Which are the two main factors in the equation that affects DNA decay?

A

The main takeaways from the Arrhenius equation is that DNA decay is dependent on temperature and time (humidity and light are also factors in the case of DNA but not implied in the Arr. Eq.)

So:
- The hotter things are, the faster the reaction
- The colder things are, the slower the reaction
–> Therefore, cold storage is good for DNA
- Also the longer the time, the more decay –> younger samples = better for DNA preservation.

Think of DNA as an ice cream - Keep it cold or use it quick, heating it up or leaving it out for a long time will make a mess.

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3
Q

What is the optimal conditions for aDNA preservation?

A

Cold, dry, dark environment and dense specimens are the most optimal for aDNA preservation.

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4
Q

What are the main characteristics of aDNA?

A
  • Its heavily fragmented (between 50-100 bp length)
  • post mortem damage (e.g. C -> T modifications)
  • usually very little endogenous DNA can be recovered (<1%) - a lot of contaminants.
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5
Q

What is the difference between endogenous and exogenous DNA?

A

Endogenous DNA is DNA that was present in the living organism at the time of death. Exogenous DNA is everything else, can be ancient contaminants or modern.

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6
Q

How can you tell the difference between modern and ancient contaminants?

A

Ancient contaminants have degraded and have similar patterns of post mortem damage ad the endogenous aDNA.

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7
Q

Name at least three different sources of aDNA.

A

Some sources of aDNA includes:
- Bone/teeth found through excavations
- Ancient sediments
- Museum collections
- Permafrost findings: e.g. bones, soft tissue etc.

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8
Q

What was the first aDNA to be sequenced?

A

The first aDNA sequence was from the Quagga (an extinct member of the horse family, study published in Nature 1984).

At the beginning of the whole field, the process was very complicated. For example, first one needed to use bacterial cloning of the fragments to get a lot and then PCR extremely time consuming before NGS.

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9
Q

Pretty early on in the field, there were extraordinary claims of aDNA sequences from VERY far back being sequenced, what and what happened to these claims?

A

During the early 90s there were several publications regarding aDNA sequences from dinosaurs, these papers were under a lot of scrutiny and later it was found to be modern contaminants that had been sequenced. This did however not stop Jurassic park hehe.

A lot of careers were flushed down the toiloets from this, “extraordinary claims require extraordinary evidence“ but from this stricted regulations and better practices came so that was good at least.

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10
Q

What are the two key aspects when working with aDNA?

A

Precautions and authentications are key for aDNA work. The precautions are there to minimize modern contamination and authentication is needed to show that the DNA is indeed ancient, for example showing that the DNA is fragmented, that there is post mortem damage and having blanks for every step to show that there hasn’t been any contamination in the handling process.

Also making phylogenetic sense is a good way to approach data, for example, if you extract DNA from a big bone, it makes little sense that you have extracted DNA from it if it comes back being more closely related to a fungi than a big animal.

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11
Q

Give three examples of measures taken to avoid contamination in an aDNA study.

A
  • Sterile equipment: UV treating everything that is brought into the lab to avoid modern contamination.
  • positive air pressure: To make sure nothing from the outside can come in.
  • Polishing the area of extraction to avoid surface contaminants.
  • Separate extraction from PCR facilities: Since PCR produces huge amounts of DNA, this practice is entirely separate from handling of the samples to avoid contamination.
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12
Q

What is the oldest aDNA ever sequenced?

A

The currently oldest aDNA that has been sequenced is for animals an about 1.1-1.2 million year old mammoth (krestovska) and for sedaDNA/eDNA an about 2 million year old ecosystem in greenland!

https://pmc.ncbi.nlm.nih.gov/articles/PMC10586222/

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13
Q

What is palaeoecology?

A

The study of past ecosystem functioning
(the interactions between species and their environment in the past)

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14
Q

What is the goal of palaeoecology?

A

To use the past to inform the present and predict the future.

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15
Q

Explain the term “shifting baseline syndrome”.

A

Shifting baseline syndrome is a phenomenon that occurs as ecosystems change over time, and new generations only remember the recent/current state as the baseline, even though an older generation might remember an entirely different situation. So the baseline is shifting, and changes might not appear as severe as they are due to the newer baselines.

Paleoecology offers a solution to this problem, as it allows us to study past ecosystems - which can inform about “true” baselines (assumes uniformitarianism) It also allows for answering different questions, for example “How much diversity have we actually lost” or how population size of different species can be affected by changes in the environment.

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16
Q

What is Uniformitarianism?

A

Uniformitarianism he belief that ‘the present is the key to the past’.

For example, erosion as a process works the same way today as it did in the past, or the fact that spruce trees today grow in cold climates, so if we find evidence of spruce growing in the past, it was probably cold in the region at the time.

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17
Q

Palaeoecology links two disciplines together, which?

A

Palaeoecology links palaeoenvironmental research (study of past abiotic systems) with palaeontology (the study of past biotic systems).

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18
Q

There are three types of palaeoecology, which?

A

The three types of palaeoecology are:

  • Classical: single-species interactions which environment
  • Evolutionary: The cycle of evolutionary innovation and generation of novel ecological niches, rise and fall of species (palaeontological deep-time palaeoecology)
  • Community: Interactions between multiple taxonomic groups and their environment (Quaternary palaeoecology) - Focus on the last 2,6 million years.
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19
Q

How old is the earth?

A

The earth is approximately 4,5 billion years old.

20
Q

When did the great oxygenation event occur? What is the evidence of this? What was the consequences of this event?

A

The great oxygenation event occurred about 2,4 billion years ago. It was a period in which the earth first experiences an increase in free oxygen in the atmosphere due to photosynthesizing microbes, leading to the death of many anaerobic species and paved the way for more complex life (multicellular life).

The evidence of this is that we can see banded iron formation (caused by oxidation) in layers dating back to this time. When atmospheric oxygen was low, iron was soluble but when the oxygen levels rose, the iron was oxidized and precipitated - forming the bands. Before this, there is no evidence of oxidation - Paleosols (fossil soils) older than 2.4 billion years old have low iron concentrations that suggest anoxic weathering (reducing environment).

21
Q

During which time/period do we find the evidence of the first multicellular organisms?

A

The first evidence of multicellular life are from the the Ediacaran, ~610–540 million years ago. This “fauna” was soft bodied so we only have trace fossils, e.g. impressions in stone, no physical fossils.

22
Q

At which time did the Cambrian explosion start? What is so special about it?

A

The Cambrian explosion started ~540 million years ago and lasted somewhere between 13-25 million years. This was a time of weirdness, also called “the time where life tried to figure out what life was supposed to look like”. During this time, there was a major increase in taxonomic diversity and all practically all major animal phyla started appearing in the fossil record. A lot of new behaviors seem to have evolved (e.g. burrowing), leading to new niches available and thus high speciation.

This period was followed by the Ordovician and Silurian periods, which a lot of geographic changes and further increase in diversity of life. The first plants are from about 470 million years ago during mid-Ordovician and the first terrestrial fungi appear in early Silurian records.

23
Q

When was the Devonian? What is the Devonian fauna known for?

A

Devonian ~420–360 million years ago was a time of terror, with the first appearance of jaws - large predators which led to armored fish for protection. During this time we also find terrestrial vascular plants and arthropods. Two major mass extinctions during this period.

24
Q

When was the Carboniferous period and what is it known for?

A

The Carboniferous period, ~350–290 million years ago, is known as being “the time of giant bugs”. During this time, oxygen levels were very high and could thus support large bugs. There were very limited fungi and other detritus/lignin consumers, so we have a lot of coal deposited from this period from falling into vast swamps and stagnant water.

25
Which periods are included in the Mesozoic era and what is it known for?
The Mesozoic era includes the Triassic, Jurassic and Cretaceous periods. Dinosaurs first appeared in the mid-triassic and dominated during the Cretaceous ~250–65 million years ago - The time of the large reptiles. During this time flowing plants took hold there was a big diversity in other animals. The Cretaceous ended with the mass extinction that took all the non-avian dinosaurs, and this opened up a lot of new niches to mammals that started to thrive.
26
Explain the interplay between evolutionary innovation and ecosystem changes.
Evolutionary innovations lead to major ecosystem changes, opening up new ecological niches and resulting in further innovation.
27
There are two major themes that are recurring through the different geological eras in regards to life, which?
- Changes in feeding --> defense against predation - Responses to major abiotic changes in the environment
28
Community palaeoecology focuses on one specific period, which and when is it?
Community palaeoecology focuses on the Quaternary period, which includes Pleistocene and Holocene (2,6 million years ago until today).
29
What characterizes the Quaternary?
The Quaternary was a time of cycling glacial and interglacial periods, with more severe and longer glacial periods closer to the present and bigger swings in ice volume.
30
How do we measure temperature in the far past?
To estimate the temperature of the past we use isotopes of oxygen, specifically the O16 and O18 isotopes. The O16 isotope is generally more abundant, and O18 is heavier so it precipitates more easily. When cold spreads towards thew equator, a lot of water evaporates --> O18 precipitates fast around the equator while O16 evaporates at higher latitudes --> glaciers are enriched in O16 (and much of the O16 is therefor bound in glaciers during glacials, and O18 is high elsewhere. The opposite occurs during interglacials.
31
Explain briefly what happens to an area that have been glaciated and then thaws.
Directly after thawing, the area is just bare rock. First, during the pioneer stages, lichens, then small annual plants and last perennial grasses and herbs colonize the land. Then as they live and die in the area they will build up substrate for bigger organisms over time. During the intermediate stages shrubs and shade-intolerant trees colonize and after some time Shade tolerant trees and other flora move in --> Climax community. This whole series of events is also referred to as succession - both in space and time.
32
Name five types of archives of past ecosystems.
- Caves: Layers can be dated - Lakes: Eg glacial lakes that carves out a basin in which surrounding material is deposited in layers over time. - Sea floor: very understudied but upcoming. - Permafrost: often contain tephra layers from previous volcanic eruptions that help form a timescale. - Archaeological sites: also a place to study what organisms coexisted with habitants. But as these are also influenced by people we need to be careful with proxies. - Rodent middens: contains anything the rodents collected - Stalactites and Stalagmites also. Those of these that are layered form a natural archive that allows for better dating estimates.
33
Explain the differences with sampling lakes vs permafrost briefly, why are they different?
Since permafrost is exposed from the side often, one can easily simple layer by layer vertically which are all visible. When sampling lakes, only the top layer is visible, so they are cored and then the undisturbed middle of the core is sampled horizontally. Lake sediments are generally undisturbed but permafrost is melting so things can fall out. Usually when sampling, one part is saved as an archive and the other half is destructively sampled.
34
What is a proxy in palaeoecology?
A palaeoecological proxy is something "else" in the natural archive/sample that can be used to inform further, for example for dating purposes. Although these can be very useful, one need to keep in mind that the proxies are only indirect evidence of the presence of an organism, so they should be complemented with other strategies for a more solid date --> Multiproxy studies are the best (and the norm today).
35
Give four examples of palaeoecological proxies and how and why they are useful, also provide pros and cons.
There are many proxies that can be used in palaeoecology: - Pollen/Spores: pollen - produced by seed plants and useful to reconstruct vegetation through microscopic observation. Abundant! Really hard to distinguish on species level, so only useful for genus level. Also since airborne, not useful for local reconstruction. - Non-pollen Palynomorphs (NPP): e.g. fungi, amoebas, sponges, algae (microscopic organisms that are not pollen in a sample). Often only identified to genus-level or higher, but can be useful in reconstructing mammalian herbivore abundance or water conditions. - Macrofossils: Plant seeds or fragments of leaves, stems, wood or roots and can represent local vegetation. Often allows for species level identification (great!) and can be used for radiocarbon dating. Although great its often much less abundant than for example pollen. Also preserves shorter and haven't been around as long as some other proxies. - Foraminifera: Amoeboid protists that are abundant in marine sediments that go all the way back to the Cambrian period, but specific species live in a limited period, so they are useful in dating and in old samples. These protists are highly sensitive to the environment, so they can be useful in determining the conditions in the environment back in time. They are also a source of carbon and oxygen isotopes that can be useful in dating. - Diatoms: photosynthesizing microalgae that also have been around a long time (originated in Triassic or Jurassic). They are abundant in moth marine and lake sediments and are highly sensitive to climate and source of carbon, oxygen, & silicon isotopes. - Beetles (remains): Parts of beetles that are preserved, e.g. wing cases or exoskeleton. Often allows for species level identification and are abundant in terrestrial archives. Highly sensitive to local climate and habitat specialists (salinity, temperature), so useful in constructing local ecosystems. - Chironomids: larvae of non-biting midges whose head capsules preserve well in lake sediments. Can usually only be identified to the genus-level, also sensitive to environment. - Biomolecules: E.g. Sedimentary ancient DNA (sedaDNA) or lipid biomarkers. SedaDNA is very useful, it allows for species identification of many different organisms at the same time and with high temporal resolution.
36
Why do we use a multiproxy approach?
We use a multiproxy approach because all proxies have their biases, and so does the different types of natural archives. For example, a bone or tooth could have been physically brought into a cave or been transported long distances after death.
37
What is "taphonomy"? Why is it important?
Taphonomy is the study of everything that happens to an organism after death until it's fossilized and deposited, e.g. the breakdown, transport and deposition of fossils. It is important to take taphonomy into consideration as the origin of an organism might be far away from the fossil record, it might have changed the material over time and since some organisms are better preserved than others, he taphonomy can lead to preservation biases as most taxa leave no trace.
38
Explain the terms "Autochthonous vs. allochthonous"
Autochthonous means that the proxy material was produced in the archive itself, e.g. aquatic plants or algae in a lake sediment. Allochthonous means that the proxy originated elsewhere and have been transported into the archive, sometimes over very long distances, e.g. pollen.
39
What are the two main biases when using microscopy for palaeoecological proxies?
The two main biases when using microscopy for palaeoecological proxies are: - The counting can be biased, if dome by hand, is everything counted correctly, sixe of the things that are counted etc. Also do we count all or just a part, that part might be biased in abundance. - Chemical used can be harsh and destroy specimens/proxies.
40
Name and explain briefly one example method used to establish chronology.
Age depth models are used to establish sample ages and are a vital aspect of palaeoecology. The thickness of each layer and the sedimentation rate allows for modelling the stratigraphy. The samples that are dated are then entered which allows for fitting the curve and extrapolate the rest of the ages. This is a great method to model the whole sample with only limited samples sent for radiocarbon dating.
41
There are many methods that can be used to support palaeoecological data, name and explain two.
- X-ray fluorescence (XRF): Measures relative ratio of sediment elemental composition - Magnetic susceptibility: Measures amount of magnetic minerals Both useful in informing on erosion. - Loss-on-ignition: Measures proportion of organic matter present - Charcoal presence: Evidence of burning (can be natural or anthropogenic)
42
Two common ways of exploring palaeoecological data are presence/absence plots and abundance plots. Explain briefly what they show and how they can be useful.
Presence/absence plots: Show which species are present/absent through time, this can be useful to get an overview of the composition of an ecosystem at a given time. Abundance plots often plots time on the X-axis and abundance in % on the Y-axis, with key species plotted. This gives you a nice overview of how abundance and composition of an ecosystem changes over time.
43
What are the benefits/pitfalls of using stratigraphic plots?
Stratigraphic plots show the percentage of different things over time, it's very useful because you can plot many different parameters next to each other for a good overview, for example species abundance, chemical composition ratios, temperature etc.
44
Give two examples of Palaeoecological data analysis methods and explain them briefly.
- Richness and turnover: richness over time, allows you to see how parameters change. - Principal Co-ordinates Analysis (PCoA): Taking large amounts of data and boiling it down to the biggest differences and comparing those, very useful to explore a dataset. - Redundancy analysis (RDA): Allows you to compare multiple types of data and multiple samples at the same time. - Mixed models: allows measurements to be explicitly modeled in a wider variety of correlation and variance-covariance avoiding biased estimations. - Mutual Climatic Range (MCR): allows for mapping overlapping data, useful to find the most likely conditions of the environment based on species composition.
45
Case studies: Relict permafrost preserves megafauna, insects, pollen, soils and pore-ice isotopes of the mammoth steppe and its collapse in central Yukon https://www-sciencedirect-com.ezp.sub.su.se/science/article/pii/S0277379122005091?via%3Dihub Anthropogenic and environmental drivers of vegetation change in southeastern Norway during the Holocene https://www-sciencedirect-com.ezp.sub.su.se/science/article/pii/S0277379121003826?via%3Dihub High resolution ancient sedimentary DNA shows that alpine plant diversity is associated with human land use and climate change https://pmc.ncbi.nlm.nih.gov/articles/PMC9636257/ Arctic shrub colonization lagged peak postglacial warmth: Molecular evidence in lake sediment from Arctic Canada https://onlinelibrary-wiley-com.ezp.sub.su.se/doi/full/10.1111/gcb.14836 Global acceleration in rates of vegetation change over the past 18,000 years https://www-science-org.ezp.sub.su.se/doi/10.1126/science.abg1685
Sedimentary ancient DNA as a tool in paleoecology https://www-nature-com.ezp.sub.su.se/articles/s43017-021-00158-8