title: Sakurajima-Satsuma (Sz-S) and Noike-Yumugi (N-Ym) tephras: new tephrochronological marker beds for the last deglaciation, southern Kyushu, Japan

authors: Moriwaki, Hiroshi

subjects: marine core

abstract: Two prominent tephras, Sakurajima-Satsuma (Sz-S) erupted from Sakurajima volcano and Noike-Yumugi (N-Ym) erupted from Kuchierabujima Island, provide new key marker beds for dating and synchronizing palaeoenvironmental and archaeological records in the last deglaciation in southern Japan. These tephras were identified on the basis of glass major-element compositions in two distal areas, a marine core (IMAGES MD98-2195) in the northern part of the East China Sea and on the central part of Tanegashima Island, and related their stratigraphic positions to the marine oxygen isotope-based chronology. In MD98-2195, Sz-S, 0.8 cm in thickness at 9.12 m depth and N-Ym, 3 cm in thickness at 9.30 m depth, are both white, vitric, ash-grade tephras. On Tanegashima Island, Sz-S, 10 cm in thickness and N-Ym, 3 cm in thickness, are stratigraphically constrained by well-characterised marker tephras Kikai-Akahoya (7,300 cal BP) and Aira-Tn (29,000 cal BP). Sz-S is rhyolitic and homogeneous on the basis of glass major-element compositions assayed by electron microprobe. Pumiceous glass shards predominant in distal Sz-S tephra indicate that it derived from pumice fall units that correspond to pumiceous and phreatomagmatic fine ash units constituting proximal Sz-S tephra. N-Ym is rhyolitic and glass major-element analyses reveal compositional diversity between units, suggesting that the lower and middle tephra units dispersed to the east, whereas the upper unit was dispersed north to north-west from the vent.
Stratigraphically, Sz-S occurs at around the start of the late-glacial reversal (cooling) in oxygen isotope records of MD98-2195, corresponding to the end of GI-1 and the start of GS-1 in the ice-core events of NGRIP (GICC05), consistent with a terrestrial age of ˜12,800 cal BP. Based on the oxygen isotope stratigraphy, the tephra identified in the core as N-Ym at 9.30 m depth is close to the end of Greenland GI-1 and hence has an age of ˜13,000 cal BP, but on Kuchierabujima Island it has an age based on ¹⁴C assay of charcoal of c. 14,900 cal BP. Although this age discrepancy (14.9 vs 13.0 cal ka) needs resolution, the occurrence in core MD98-2195 of N-Ym shows that it is more widespread than hitherto demonstrated. The widespread distributions and key stratigraphic positions for the two marker tephras indicate that they are thus critical isochrons for precise correlation of palaeoenvironmental changes and prehistoric cultural events during the last deglaciation in southern Kyushu, and for relating such changes and events to the ice-core chronology via the marine oxygen isotope chronostratigraphy.

text: Sakurajima-Satsuma (Sz-S) and Noike-Yumugi (N-Ym) tephras: new tephrochronological marker beds for the last deglaciation, southern Kyushu, Japan Two prominent tephras, Sakurajima-Satsuma (Sz-S) erupted from Sakurajima volcano and Noike-Yumugi (N-Ym) erupted from Kuchierabujima Island, provide new key marker beds for dating and synchronizing palaeoenvironmental and archaeological records in the last deglaciation in southern Japan. These tephras were identified on the basis of glass major-element compositions in two distal areas, a marine core (IMAGES MD98-2195) in the northern part of the East China Sea and on the central part of Tanegashima Island, and related their stratigraphic positions to the marine oxygen isotope-based chronology. In MD98-2195, Sz-S, 0.8 cm in thickness at 9.12 m depth and N-Ym, 3 cm in thickness at 9.30 m depth, are both white, vitric, ash-grade tephras. On Tanegashima Island, Sz-S, 10 cm in thickness and N-Ym, 3 cm in thickness, are stratigraphically constrained by well-characterised marker tephras Kikai-Akahoya (7,300 cal BP) and Aira-Tn (29,000 cal BP). Sz-S is rhyolitic and homogeneous on the basis of glass major-element compositions assayed by electron microprobe. Pumiceous glass shards predominant in distal Sz-S tephra indicate that it derived from pumice fall units that correspond to pumiceous and phreatomagmatic fine ash units constituting proximal Sz-S tephra. N-Ym is rhyolitic and glass major-element analyses reveal compositional diversity between units, suggesting that the lower and middle tephra units dispersed to the east, whereas the upper unit was dispersed north to north-west from the vent.
Stratigraphically, Sz-S occurs at around the start of the late-glacial reversal (cooling) in oxygen isotope records of MD98-2195, corresponding to the end of GI-1 and the start of GS-1 in the ice-core events of NGRIP (GICC05), consistent with a terrestrial age of ˜12,800 cal BP. Based on the oxygen isotope stratigraphy, the tephra identified in the core as N-Ym at 9.30 m depth is close to the end of Greenland GI-1 and hence has an age of ˜13,000 cal BP, but on Kuchierabujima Island it has an age based on ¹⁴C assay of charcoal of c. 14,900 cal BP. Although this age discrepancy (14.9 vs 13.0 cal ka) needs resolution, the occurrence in core MD98-2195 of N-Ym shows that it is more widespread than hitherto demonstrated. The widespread distributions and key stratigraphic positions for the two marker tephras indicate that they are thus critical isochrons for precise correlation of palaeoenvironmental changes and prehistoric cultural events during the last deglaciation in southern Kyushu, and for relating such changes and events to the ice-core chronology via the marine oxygen isotope chronostratigraphy.

year: 2011

title: Foraging on café sugar packets by the house sparrow (Passer domesticus): Learning mechanisms, distribution, and human perception

authors: Davy, Michael Ambrose

subjects: urban ecology

abstract: People in cities interact with house sparrows (Passer domesticus) on a daily basis. Sparrows have previously been observed foraging on sugar packets at a single café in Hamilton City, New Zealand. The aim of this thesis was to explore aspects of this novel foraging innovation by sparrows and to investigate people’s perceptions of sparrows being present at cafés. 

Sparrows’ preferences for different grain sizes of raw sugar and artificial sweetener were assessed at a single café, which demonstrated that sparrows have a strong preference for raw sugar over artificial sweetener, but no clear preference between granulated raw sugar and powdered raw sugar. Sparrows’ responses to novel sugar packet colours were also investigated at the same café. The sparrows did not start foraging on the novel-coloured sugar packets within 10 experimental sessions, but did interact with the novel sugar packets, which demonstrated neophilia in the sparrows and is an important step in the process of learning.

The distribution of sugar packet foraging by sparrows across 174 cafés in Hamilton City was determined, and staff from 15 cafés had observed sparrows taking sugar packets. A short survey was also used to assess the attitudes of café staff members towards the presence of sparrows at their cafés, which showed that café staff had mixed views on the local sparrows. A different survey was used to investigate the attitudes of 249 members of the general public towards sparrows being at cafés. These participants tended to like sparrows being present as part of their café experience. 

This thesis demonstrates the value of sparrows being present in the urban environment, and is the first study to comprehensively describe sugar packet foraging in sparrows: a fascinating behavioural innovation.

text: Foraging on café sugar packets by the house sparrow (Passer domesticus): Learning mechanisms, distribution, and human perception People in cities interact with house sparrows (Passer domesticus) on a daily basis. Sparrows have previously been observed foraging on sugar packets at a single café in Hamilton City, New Zealand. The aim of this thesis was to explore aspects of this novel foraging innovation by sparrows and to investigate people’s perceptions of sparrows being present at cafés. 

Sparrows’ preferences for different grain sizes of raw sugar and artificial sweetener were assessed at a single café, which demonstrated that sparrows have a strong preference for raw sugar over artificial sweetener, but no clear preference between granulated raw sugar and powdered raw sugar. Sparrows’ responses to novel sugar packet colours were also investigated at the same café. The sparrows did not start foraging on the novel-coloured sugar packets within 10 experimental sessions, but did interact with the novel sugar packets, which demonstrated neophilia in the sparrows and is an important step in the process of learning.

The distribution of sugar packet foraging by sparrows across 174 cafés in Hamilton City was determined, and staff from 15 cafés had observed sparrows taking sugar packets. A short survey was also used to assess the attitudes of café staff members towards the presence of sparrows at their cafés, which showed that café staff had mixed views on the local sparrows. A different survey was used to investigate the attitudes of 249 members of the general public towards sparrows being at cafés. These participants tended to like sparrows being present as part of their café experience. 

This thesis demonstrates the value of sparrows being present in the urban environment, and is the first study to comprehensively describe sugar packet foraging in sparrows: a fascinating behavioural innovation.

year: 2019

title: "Thereness": Implications of Heidegger's "presence" for Māori

authors: Mika, Carl Te Hira

abstract: For Māori, the philosophical consequences of colonization are a hugely important issue, due to both the subtlety and the omnipresence of Western metaphysics. In this article I refer to the “meta-physics of presence” through one major Western thinker—Martin Heidegger—who identified “presence” as a problem for the West. He proposes that the metaphysics of presence underpins every perception in the West and that it is the fundamental mistake of philosophers since Plato but becoming ascendant with Aristotle. I identify the points of relevance within their claims and refer them to a Māori understanding of absence. I also consider the more affective nature of Western presence, which Heidegger refers to but which must be theorized by Māori. In the first instance I place particular emphasis on the ironies implicit in writing about metaphysics for the Māori writer in the academy and for the things being represented in that writing. Finally, the metaphysics of presence opens up possibilities for its own instability; this Heideggerean “saving power” is discussed in Māori terms.

text: "Thereness": Implications of Heidegger's "presence" for Māori For Māori, the philosophical consequences of colonization are a hugely important issue, due to both the subtlety and the omnipresence of Western metaphysics. In this article I refer to the “meta-physics of presence” through one major Western thinker—Martin Heidegger—who identified “presence” as a problem for the West. He proposes that the metaphysics of presence underpins every perception in the West and that it is the fundamental mistake of philosophers since Plato but becoming ascendant with Aristotle. I identify the points of relevance within their claims and refer them to a Māori understanding of absence. I also consider the more affective nature of Western presence, which Heidegger refers to but which must be theorized by Māori. In the first instance I place particular emphasis on the ironies implicit in writing about metaphysics for the Māori writer in the academy and for the things being represented in that writing. Finally, the metaphysics of presence opens up possibilities for its own instability; this Heideggerean “saving power” is discussed in Māori terms.

year: 2015