Stable isotope and Mg/Ca ratios of Paleogene benthic foraminifera in the western North Atlantic

Global cooling and the development of continental-scale Antarctic glaciation occurred in the late middle Eocene to early Oligocene (~38 to 28 million years ago), accompanied by deep-ocean reorganization attributed to gradual Antarctic Circumpolar Current (ACC) development. Our benthic foraminiferal stable isotope comparisons show that a large d13C offset developed between mid-depth (~600 meters) and deep (>1000 meters) western North Atlantic waters in the early Oligocene, indicating the development of intermediate-depth d13C and O2 minima closely linked in the modern ocean to northward incursion of Antarctic Intermediate Water. At the same time, the ocean's coldest waters became restricted to south of the ACC, probably forming a bottom-ocean layer, as in the modern ocean. We show that the modern four-layer ocean structure (surface, intermediate, deep, and bottom waters) developed during the early Oligocene as a consequence of the ACC.

Monthly Bonaire coral Sr/Ca and oxygen isotope data from 118 kyr ago (coral BON-5-D)

The end of the last interglacial period, ~118 kyr ago, was characterized by substantial ocean circulation and climate perturbations resulting from instabilities of polar ice sheets. These perturbations are crucial for a better understanding of future climate change. The seasonal temperature changes of the tropical ocean, however, which play an important role in seasonal climate extremes such as hurricanes, floods and droughts at the present day, are not well known for this period that led into the last glacial. Here we present a monthly resolved snapshot of reconstructed sea surface temperature in the tropical North Atlantic Ocean for 117.7±0.8 kyr ago, using coral Sr/Ca and d18O records. We find that temperature seasonality was similar to today, which is consistent with the orbital insolation forcing. Our coral and climate model results suggest that temperature seasonality of the tropical surface ocean is controlled mainly by orbital insolation changes during interglacials.

Ordenanças del Co[n]seio Real de su Magestad y los ara[n]zeles q[ue] han d[e] guardar los relatores, escriuanos d[e] camara, escriuanos d[e]l crime[n], escriuanos d[e] prouincia, alguaziles [et] alguaziles del ca[m]po, porteros y emplazadores ...

Imp. tomado del colofón

D. Jacobi Parez [sic] de Vale[n]tia ... ordinis diui Augustini ... expositiones in. CL. psal. Dauidicos ... Cantica ferialia in biblijs contenta. Cantica eua[n]gelica B[e]n[e]dictus Magnificat nu[n]c dimit. Gl[or]ia in excel. Ca[n]ticu[m] Amb. et Aug. Te Deum. Cantica canticor[um] Premissis Questio[n]ib[us] et earu[m] subtilissimis resolutionibus co[n]tra Judeos nostre fidei adversa [Texto impreso] : Cum tabula in totu[m] opus collecta

Marca tip. en port. y colofón en h. [27]

Ca(2+)-independent reduction of N-methyl-D-aspartate channel activity by protein tyrosine phosphatase.

Regulation of ion channel function by intracellular processes is fundamental for controlling synaptic signaling and integration in the nervous system. Currents mediated by N-methyl-D-aspartate (NMDA) receptors decline during whole-cell recordings and this may be prevented by ATP. We show here that phosphorylation is necessary to maintain NMDA currents and that the decline is not dependent upon Ca2+. A protein tyrosine phosphatase or a peptide inhibitor of protein tyrosine kinase applied intracellularly caused a decrease in NMDA currents even when ATP was included. On the other hand, pretreating the neurons with a membrane-permeant tyrosine kinase inhibitor occluded the decline in NMDA currents when ATP was omitted. In inside-out patches, applying a protein tyrosine phosphatase to the cytoplasmic face of the patch caused a decrease in probability of opening of NMDA channels. Conversely, open probability was increased by a protein tyrosine phosphatase inhibitor. These results indicate that NMDA channel activity is reduced by a protein tyrosine phosphatase associated with the channel complex.

Latent N-methyl-D-aspartate receptors in the recurrent excitatory pathway between hippocampal CA1 pyramidal neurons: Ca(2+)-dependent activation by blocking A1 adenosine receptors.

When performed at increased external [Ca2+]/[Mg2+] ratio (2.5 mM/0.5 mM), temporary block of A1 adenosine receptors in hippocampus [by 8-cyclopentyltheophylline (CPT)] leads to a dramatic and irreversible change in the excitatory postsynaptic current (EPSC) evoked by Schaffer collateral/commissural (SCC) stimulation and recorded by in situ patch clamp in CA1 pyramidal neurons. The duration of the EPSC becomes stimulus dependent, increasing with increase in stimulus strength. The later occurring component of the EPSC is carried through N-methyl-D-aspartate (NMDA) receptor-operated channels but disappears under either the NMDA antagonist 2-amino-5-phosphonovaleric acid (APV) or the non-NMDA antagonist 6-cyano-7-nitroquinoxaline-2,3-dione (CNQX). These findings indicate that the late component of the SCC-evoked EPSC is polysynaptic: predominantly non-NMDA receptor-mediated SCC inputs excite CA1 neurons that recurrently excite each other by predominantly NDMA receptor-mediated synapses. These recurrent connections are normally silent but become active after CPT treatment, leading to enhancement of the late component of the EPSC. The activity of these connections is maintained for at least 2 hr after CPT removal. When all functional NMDA receptors are blocked by dizocilpine maleate (MK-801), subsequent application of CPT leads to a partial reappearance of NMDA receptor-mediated EPSCs evoked by SCC stimulation, indicating that latent NMDA receptors are recruited. Altogether, these findings indicate the existence of a powerful system of NMDA receptor-mediated synaptic contacts in SCC input to hippocampal CA1 pyramidal neurons and probably also in reciprocal connections between these neurons, which in the usual preparation are kept latent by activity of A1 receptors.

"A list of the books belonging to the late Library of Harvard College that were in the hands of the Overseers, Governors, & Students of the College & escap'd the flames," ca. 1764

This list appears to be the most comprehensive in this series. Although its contents are very similar to those of the list in Folder 2, there are some discrepancies. Entries are arranged by format (folio, quarto, octavo) and include the date the book was "delivered" (loaned), the name of the individual who borrowed it, and its author, title, and volume number. Many of the books had been out of the library for decades prior to the fire, with some loaned out since as early as 1742.

Kitāb Mufarriḥ al-nafs / taṣnīf al-Imām al-ʻālim al-fāḍil Sharaf al-D��n Abī Naṣr Muḥammad ibn ʻUmar ibn Abī al-Futūḥ al-Baghd��d�� thumma al-Mārid��nī al-maʻrūf bi-Ibn al-Marah : manuscript, [ca. 1530]

The author's name appears as ابن المره in title page (f. 1r) and ابن المراه at the beginning of the book (f. 1v).

Thabat al-ʻAllāmah al-Shaykh ʻAlī ibn Aḥmad ibn Mukarram Allāh al-Ṣaʻīd�� : manuscript, [ca. 1850]

Unbound.

Kashf al-ghayn ʻammā bi-wād�� al-Shardad min dhurrīyat al-sibṭayn : manuscript, [ca. 1918]

Title not mentioned in Brockelmann, S, II, 548.