UCLA After the Ice Age Summary Presentation

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Post-ice age recolonization and differentiation of Fucus Northern Europe ABSTRACT REWRITE Fucus serratus, a seaweed, is assumed to have evolved in the North Atlantic, and current populations represent recolonization from a southern refugium since the last glacial maximum 18 000–20 000 years ago. By analyzing seven microsatellite loci in populations taken from 21 locations across the species' range, we were able to evaluate genetic structure at many spatial scales. Despite restricted gamete dispersal in F. serratus of less than 2 m from parental individuals, spatial auto-correlation analysis of seven microsatellite loci found no evidence for spatial clustering of alleles on a scale of 100 m. The minimal panmictic unit for F. serratus, according to pairwise analysis, was 0.5 to 2 kilometers. Along some adjacent beaches, isolation by distance was significant. Despite a brief history of 7500 years, population differentiation was substantial within the Skagerrak–Kattegat–Baltic Seas (SKB) (global = 0.17) A neighbor-joining tree based on Reynold's distances computed from microsatellite data revealed a central assemblage of populations on the Brittany Peninsula, which was surrounded by four wellsupported clusters: the SKB, the North Sea (Ireland, Helgoland), and two populations from the northern Spanish coast. Icelandic and Nova Scotian samples were most closely related to samples from northwest Sweden and Brittany, respectively. Allelic diversity was twofold higher in Brittany groups than in populations to the north and threefold higher in southern populations when sample sizes were standardized (N = 41). The Brittany region could represent a refugium or a recolonized area, but the Spanish populations are most likely present-day edge populations that have gone through several bottlenecks as a result of thermally induced recolonization and extinction cycles. Abstract The goal of this research is to look into the impact of post-LIA Neoglacial retreat on the slope instability in 19 alpine reservoirs in British Columbia's upper Lillooet River Valley. The study investigates the effects of scouring and glacial retreat on the shape and stability of hillslopes. The research is designed through the creation of a flow chart that compares the landslide hazards associated with glacier melting. The analysis employed field mapping, GIS analysis, landslide statistic comparison, landscape characteristics, and a comparison of landscapes with and without a history of landslides. The extent of landslide response to glacial retreat is primarily determined by rock characteristics, and the variation of glacial scour below the LIA trim line. There is intense terrain activity, aggressive rock and landslides in hillsides engraved in frail rock formations. Post-LIA retreat, on the other hand, rarely causes increased bedrock instability in stronger granitic rock, except in cases of shallow-seated rock slides and unstable slopes. Landslides caused by post-LIA retreat begin as debris slides or debris avalanches from unstable deposits and cluster in bedrock components along directional glacial ice or glaciation trim lines. The findings of the study revealed a highly significant relationship between the landslide hazard, gravitational slope displacement, and over-steeped hillsides caused by glacial erosion. The results indicated that 8/10 dangerous rock slope failures occurred just above deep valley terrains and in areas associated with deep landslides, implying that this type of instability was the starting point for dangerous landslides. Your presentation (Week 7, 8, or 10) should be about 7 minutes long, and have three main components: 1. a summary of your book 2. a brief summary of your abstracts and a discussion of how they relate/contribute to your book’s message 3. your thoughts on the book (such as: Is it worth reading? What made you choose it?) These components do not have to be in this order, and you can blend them together if you like. As a presenter, you will be graded on the content, organization, clarity, design, and delivery of your presentation. Book: After the Ice Age: The Return of Life to Glaciated North America by E.C. Pielou
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AFTER THE ICE AGE: THE RETURN OF
LIFE TO GLACIATED NORTH AMERICA

by E.C. Pielou

After the Ice Age: The Return of Life to
Glaciated North America by E.C. Pielou
Introduction
◦ “After the Ice Age: the Return of Life to Glaciated North America” is a book that demonstrates the evolution of
life in North America after the melting of glaciers. The author, E. C. Pielou, is a Canadian biologist and writer
who has written extensively about science and nature. Her writing style is engaging, and she presents complex
scientific information in an easy-to-understand way.

◦ This book chronicles the restoration of life to areas that were once covered in ice. It’s also a great lesson in
evolution, as it explains how species from elsewhere migrated to North America as the glaciers receded and
recolonized the land.
◦ It is not just a general overview of the effects that glaciers have on landscapes, but a very detailed look at
specific areas and what happened to them after being exposed to the elements.
◦ It shows how vegetation grows back, animals recolonize the area, and ecological succession occurs after
◦ It follows the story of the fossil record from near extinction at the end of the last ice age to the thriving
ecosystems that exist at present.

Summary: “After the Ice Age: the Return of
Life to Glaciated North America”
◦ The book “After the Ice Age: The Return of Life to Glaciated North America” wrote by Pielou described
the events happened on Earth after the glacial advances after 20,000 years. It provided information through
samples from both extinct as well as extant inconsequential species. These samples served as geological
evidence in understanding the cycles affecting the different condition of the environment such as the
Malankovich Cycle.
◦ Malankovich Cycle describes the rotation of the Earth around the sun, the warming of the climate for the past
10,000 years, as well as the Ice Age during 1600 A.D.
◦ The Agassiz and the McConnell lakes which is demarcated on the map and its influences on the present pattern
of landforms as well as vegetations are clearly described by the author.

Continuation of the Summary of the
Book…
◦ It is explained in the book how the species were distributed across North America due to their capability to
migrate especially when the lakes flowed and drained in different major drainages.
◦ The author narrated articulately the observations of insignificant organisms like the floating single-celled
species, the foraminifera that were fossilized and mixed to the sediments of the lake. The changes in these
forams in the water sediments signifies climate change.
◦ The evolution of the Glacial lakes such as the Lake Missoula, the changes in terrains in eastern part of
Washingto...


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