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A gradual rise in Earth's surface temperature marks a transition from the late Paleocene to the early Eocene ca. 58-51 Ma. Paleocene/Eocene boundary (∼55.5 Ma) sediments deposited in the midst of this slow warming ubiquitously reveal evidence for a massive isotopically light carbon injection and an associated rapid but transient global warming event, or hyperthermal, that has been termed the Paleocene Eocene Thermal Maximum (PETM) and attributed to a carbon injection from multiple potential sources. The PETM has gained importance over the past two decades as a potential geologic analog to the modern anthropogenic carbon injection and climate change. However significant questions surrounding the nature of the carbon injection at the onset of the PETM remain. The Clarence River valley, located in the Marlborough region, South Island, New Zealand, contains a series of outcrops of lithified late Paleocene to early Eocene sediments originally deposited on a paleo-slope margin. Within these sections, the Lower Limestone Member of the Amuri Limestone Formation records the interval of interest. A Lower Limestone prominent recessed unit consisting of multiple marl-rich beds and recording a pronounced negative carbon isotopic excursion (CIE) marks the PETM at sections that have been bisected by tributaries to the Clarence River, including Mead Stream and Dee Stream. Here I detail and discuss Clarence valley Lower Limestone sections and relate these records to global trends with an emphasis on adding constraints to the PETM carbon injection. Specifically, I document the lithologic and carbon isotopic expression of the PETM and two younger paired sets of early Eocene events that, similar to the Mead Stream and Dee Stream PETM sections, reveal negative CIEs and expanded marl-rich units coincident to identical CIEs and condensed carbonate dissolution horizons in deep-sea sections. I further quantify the abundance of bioturbating macrofauna trace fossils through the PETM at both Mead Stream and Dee Stream and argue that New Zealand margin intermediate waters became hypoxic precisely coincident to the PETM carbon injection. In concert, these findings suggest a PETM carbon addition mechanism capable of both diminishing intermediate water dissolved oxygen and of repeated early Eocene injections. / U.S. National Science Foundation (NSF); Joint Oceanographic Institutions (JOI), Inc.

As mudanças climáticas influenciarão as médias de temperaturas ambientais e a frequência de eventos extremos com consequências ainda desconhecidas para a fauna. Conhecer os limites fisiológicos dos organismos ao aumento de temperatura pode ajudar a ampliar os marcos conceituais dos impactos regionais das mudanças climáticas sobre a fauna. Este trabalho abordou como a diversidade fisiológica representada pela tolerância termal da fauna de artrópodes terrestres estava relacionada entre os biomas do Brasil, em uma perspectiva macrofisiológica (ampla escala espacial). Especificamente, coletou-se a temperatura crítica máxima (TCMax) de espécimens de artrópodes das Classes Arachnida, Chilopoda, Dipoploda, Entognatha (Collembola), Insecta e Malacostraca (Oniscidea) nos biomas de Mata Atlântica (strictu sensu), Mata Atlântica de Altitude, Cerrado, Amazônia e Caatinga. Os artrópodes foram utilizados como modelo de estudo por permitirem uma associação mais clara com a teoria disponível sobre limites fisiológicos e o ambiente físico. Assim, foram investigados padrões de variação da TCMax entre e dentro dos biomas, considerando ou não a categoria sistemática. Igualmente, foi avaliada a relação da TCMax da fauna de artrópodes com variáveis bioclimáticas representantes do ambiente termal nos biomas. No aspecto de margem de segurança termal, avaliou-se a potencial tolerância ao aquecimento da fauna de artrópodes nos biomas. Os resultados mostraram que existe ampla diversidade fisiológica da fauna de artrópodes, com padrões atrelados aos biomas do Brasil. A relação do padrão de tolerância termal dos espécimens de artrópodes com o bioma é complexa, havendo nuances de variação dentro e entre os biomas. Houve grande proporção de fauna termotolerante no bioma da Caatinga e menor proporção de fauna termotolerante na Mata Atlântica. Quanto às margens de segurança termal, os dados de tolerância ao aquecimento sugerem que não há grande susceptibilidade ao aquecimento da fauna de artrópodes nos biomas do Brasil. Este trabalho contribui para ampliar a discussão dos possíveis impactos das mudanças climáticas em seus aspectos regionais, tendo em vista a diversidade fisiológica da fauna de artrópodes terrestres nos biomas brasileiros. Igualmente, os dados podem servir como uma importante base para a incorporação em avaliações globais da vulnerabilidade dos ectotérmicos frente às mudanças do clima / Climate change will affect the average environmental temperatures and the frequency of extreme events with still unknown consequences for wildlife. To understand the physiological limits of organisms in relation to the increase in environmental temperature can help extend the conceptual frameworks of climate change regional impacts on wildlife. This work discussed how the physiological diversity represented by the thermal tolerance of terrestrial arthropod fauna was related among biomes of Brazil in a macrophysiological perspective (large spatial scale). It was collected critical thermal maximum (CTMax) of specimens of the class Arachnida, Chilopoda, Dipoploda, Entognatha (Collembola), Insecta and Malacostraca (Oniscidea) in the biomes of the Atlantic Forest (strictu sensu), Atlantic Forest Highland, Cerrado (Brazilian Savanna), Amazonia and Caatinga. The arthropods were used as model to allow a better association with the available theory of physiological limits and the physical environment. Thus, it was investigated variation in patterns of CTMax between and within biomes considering or not the systematic category. It was also evaluated the relationship of CTMax of the arthropod fauna with bioclimatic variables as representative of the thermal environment in the biomes. In terms of thermal safety margin, it was evaluated potential warming tolerance of the arthropod fauna in the biomes. The results showed that there is a broad physiological diversity of arthropod fauna with patterns linked to brazilian biomes. The ratio between thermal tolerance patterns of arthropod specimens and the biome is complex, there were varying nuances within and between biomes. There is a large proportion of thermotolerant fauna in the Caatinga biome and a lesser proportion of thermotolerant fauna in the Atlantic Forest. The warming tolerance data suggest that the susceptibility to heat of the arthropod fauna in brazilian biomes is small. This work will help to expand discussions of potential impacts of climate change regional aspects considering the view of the physiological diversity of terrestrial arthropod fauna in the brazilian biomes. In addition, the data can be as an important basis for incorporation into global vulnerability assessments on terrestrial ectotherms in view of climate change

Lake sediments contain the remains of midge communities that may be used as biological proxies for inferring past environmental changes. Freshwater midges, including Chironomidae and Chaoboridae, from two alpine tarns (Pyramid Lake and Bullwinkle Lake) in the Cassiar Mountains of northern British Columbia were used to estimate Holocene palaeotemperature changes, and more specifically, to test for the presence of the Milankovitch thermal maximum, an early Holocene warm interval coinciding with peak Holocene summer solar insolation. Mean July air temperatures were reconstructed using midge-inference models developed via weighted averaging-partial least squares (WA-PLS) regression. Cold-tolerant midge taxa dominate the stratigraphies from both Pyramid and Bullwinkle Lakes; however, warm-adapted species are more common in Bullwinkle Lake. Early Holocene warming is apparent at both lakes, however it is unclear whether this is indicative of the Milankovitch thermal maximum. A decrease in temperature occurs from 8,700-7,900 cal. yr BP at Pyramid Lake, around the same time that the 8,200 cal. yr BP cooling event occurred in the northern hemisphere. During the middle Holocene, records from Pyramid Lake indicate an overall decrease in temperature, with a short period of warmer temperatures that peak at 5,100 cal. yr BP. Temperatures fluctuate little during this time at Bullwinkle Lake. A short warming phase is apparent at both lakes during the late Holocene. July temperatures are highest at 2,000 cal. yr BP (10.5°C) in Pyramid Lake and at 1,200 cal. yr BP (13°C) in Bullwinkle Lake. Thereafter, temperatures return to what they were before the warming occurred, and at Bullwinkle Lake, vary little throughout the remainder of the Holocene.

Lake sediments contain the remains of midge communities that may be used as biological proxies for inferring past environmental changes. Freshwater midges, including Chironomidae and Chaoboridae, from two alpine tarns (Pyramid Lake and Bullwinkle Lake) in the Cassiar Mountains of northern British Columbia were used to estimate Holocene palaeotemperature changes, and more specifically, to test for the presence of the Milankovitch thermal maximum, an early Holocene warm interval coinciding with peak Holocene summer solar insolation. Mean July air temperatures were reconstructed using midge-inference models developed via weighted averaging-partial least squares (WA-PLS) regression. Cold-tolerant midge taxa dominate the stratigraphies from both Pyramid and Bullwinkle Lakes; however, warm-adapted species are more common in Bullwinkle Lake. Early Holocene warming is apparent at both lakes, however it is unclear whether this is indicative of the Milankovitch thermal maximum. A decrease in temperature occurs from 8,700-7,900 cal. yr BP at Pyramid Lake, around the same time that the 8,200 cal. yr BP cooling event occurred in the northern hemisphere. During the middle Holocene, records from Pyramid Lake indicate an overall decrease in temperature, with a short period of warmer temperatures that peak at 5,100 cal. yr BP. Temperatures fluctuate little during this time at Bullwinkle Lake. A short warming phase is apparent at both lakes during the late Holocene. July temperatures are highest at 2,000 cal. yr BP (10.5°C) in Pyramid Lake and at 1,200 cal. yr BP (13°C) in Bullwinkle Lake. Thereafter, temperatures return to what they were before the warming occurred, and at Bullwinkle Lake, vary little throughout the remainder of the Holocene.

Lake sediments contain the remains of midge communities that may be used as biological proxies for inferring past environmental changes. Freshwater midges, including Chironomidae and Chaoboridae, from two alpine tarns (Pyramid Lake and Bullwinkle Lake) in the Cassiar Mountains of northern British Columbia were used to estimate Holocene palaeotemperature changes, and more specifically, to test for the presence of the Milankovitch thermal maximum, an early Holocene warm interval coinciding with peak Holocene summer solar insolation. Mean July air temperatures were reconstructed using midge-inference models developed via weighted averaging-partial least squares (WA-PLS) regression. Cold-tolerant midge taxa dominate the stratigraphies from both Pyramid and Bullwinkle Lakes; however, warm-adapted species are more common in Bullwinkle Lake. Early Holocene warming is apparent at both lakes, however it is unclear whether this is indicative of the Milankovitch thermal maximum. A decrease in temperature occurs from 8,700-7,900 cal. yr BP at Pyramid Lake, around the same time that the 8,200 cal. yr BP cooling event occurred in the northern hemisphere. During the middle Holocene, records from Pyramid Lake indicate an overall decrease in temperature, with a short period of warmer temperatures that peak at 5,100 cal. yr BP. Temperatures fluctuate little during this time at Bullwinkle Lake. A short warming phase is apparent at both lakes during the late Holocene. July temperatures are highest at 2,000 cal. yr BP (10.5°C) in Pyramid Lake and at 1,200 cal. yr BP (13°C) in Bullwinkle Lake. Thereafter, temperatures return to what they were before the warming occurred, and at Bullwinkle Lake, vary little throughout the remainder of the Holocene. / Irving K. Barber School of Arts and Sciences (Okanagan) / Earth and Environmental Sciences, Department of (Okanagan) / Graduate

Cities are rapidly expanding, and global warming is intensified in urban environments due to the urban heat island effect. Therefore, urban animals may be particularly susceptible to warming associated with ongoing climate change. Thus, I used a comparative and manipulative approach to test three related hypotheses about the determinants of heat tolerance or critical thermal maximum (CTmax) in urban ants—specifically, that (1) body size, (2) hydration status, and (3) preferred micro-environments influence CTmax. I further tested a fourth hypothesis that native species are particularly physiologically vulnerable in urban environments. I manipulated water access and determined CTmax for 11 species common to cities in California's Central Valley that exhibit nearly 300-fold variation in body mass. Inter- (but not intra-) specific variation in body size influenced CTmax where larger species had higher CTmax. The sensitivity of ants’ CTmax to water availability exhibited species-specific thresholds where short-term water limitation (8 h) reduced CTmax in some species while longer-term water limitation (32 h) was required to reduce CTmax in other species. However, CTmax was not influenced by the preferred foraging temperatures of ants. Further, I did not find support for my fourth hypothesis because native species did not exhibit reduced thermal safety margins, or exhibit CTmax values that were more sensitive to water limitation relative to non-native species. In sum, understanding the links between heat tolerance and water availability will become critically important in an increasingly warm, dry, and urbanized world that may be selecting for smaller (not larger) body size.

Pollen analysis of a sediment core from Lake SP02, Melville Peninsula, Nunavut, Canada provides a ~6300 year record of post-glacial vegetation and climate change. Dominant local and regional taxa identified include Cyperaceae, Ericaceae, Artemisia, Salix, and Oxyria. Fossil pollen assemblages, pollen accumulations rates, and variations in sediment organic matter, indicate a period of optimal Holocene warmth between 5300-3900 yr BP, followed by a prolonged period of Neoglacial cooling, as well as a period of relative warmth between 1300-1000 yr BP, interpreted as evidence for the Medieval Warm Period. Variations in pollen abundances and accumulations during the 20th century suggest a response to recent warming that is unprecedented since deglaciation of the Peninsula. Comparisons of the timing and rates of multi-scale climate variations for Melville Peninsula with adjacent sites reveal a potential late Holocene shift in the boundary separating continental and maritime climate regions in the eastern Canadian Arctic.

Pollen analysis of a sediment core from Lake SP02, Melville Peninsula, Nunavut, Canada provides a ~6300 year record of post-glacial vegetation and climate change. Dominant local and regional taxa identified include Cyperaceae, Ericaceae, Artemisia, Salix, and Oxyria. Fossil pollen assemblages, pollen accumulations rates, and variations in sediment organic matter, indicate a period of optimal Holocene warmth between 5300-3900 yr BP, followed by a prolonged period of Neoglacial cooling, as well as a period of relative warmth between 1300-1000 yr BP, interpreted as evidence for the Medieval Warm Period. Variations in pollen abundances and accumulations during the 20th century suggest a response to recent warming that is unprecedented since deglaciation of the Peninsula. Comparisons of the timing and rates of multi-scale climate variations for Melville Peninsula with adjacent sites reveal a potential late Holocene shift in the boundary separating continental and maritime climate regions in the eastern Canadian Arctic.

Freshwater mussels is one the most endangered groups of organisms worldwide and stand in front of several threats. Global warming along with anthropogenic influence affect the mussel’s natural habitat and stress leads to changes in their behaviour. The aim was to investigate if the behaviour of Unio tumidus exposed to thermal stress differs depending on fine particulate matter exposure. This study hypothesises that (1) the critical thermal maximum of mussels is lower in high turbidity than in clear water (2) mussels in highly turbid water extend their foot at a lower temperature than in clear water (3) mussels have a more frequent gaping behaviour in high turbidity than in clear water. Mussels were placed in each water filled beaker with sensors glued to their shells for monitoring gaping behaviour. Aquarium heaters increased the water temperature gradually until the mussels reached their CTM. One group were placed in clear river water and one group in water with high turbidity. There was no significant difference in the CTM between the highly turbid and clear water. The mussels in the river water extended their foot at a lower temperature compared to the mussels in high turbidity. One possible explanation is that the mussels remain shut to protect themselves due to higher stress levels. Valve gaping behaviour was visually investigated and displayed different patterns between mussels in clear and highly turbid water. This study contributes with information regarding mussel behaviour and response to thermal stress which can be of value for future studies. / Sötvattenmusslor är en av de mest hotade organismerna i världen och står inför flera hot. Global uppvärmning tillsammans med antropogen inverkan påverkar musslornas naturliga livsmiljö och stress leder till förändringar i deras beteende. Syftet var att undersöka om beteendet hos Unio tumidus som utsätts för termisk stress skiljer sig beroende på exponering av fina partiklar. Denna studie antar att (1) critical thermal maximum för musslor är lägre vid hög turbiditet än i åvatten (2) musslor i hög turbiditet sträcker ut sin fot vid en lägre temperatur än i åvatten (3) musslor har ett mer frekvent öppningsbeteende vid hög turbiditet än i åvatten. Musslor placerades i vattenfyllda bägare med sensorer limmade på sina skal för att övervaka öppningsbeteende. Akvarievärmare ökade vattentemperaturen gradvis tills musslorna nådde sitt critical thermal maximum. En grupp placerades i åvatten och en grupp i vatten med hög turbiditet. Det fanns ingen signifikant skillnad i CTM mellan hög turbiditet och åvattnet. Musslorna i åvattnet sträckte ut sin fot vid en lägre temperatur jämfört med musslorna i hög turbiditet. En möjlig förklaring är att musslorna förblir stängda för att skydda sig på grund av högre stress. Öppningsbeteende undersöktes visuellt och visade olika mönster mellan musslor i åvatten och vatten med hög turbiditet. Denna studie bidrar med information om musslornas beteende och respons på termisk stress som kan vara av värde för framtida studier.